* 1^.v^. If *4'^. -■'* — ^ :&.<' t^i^ .• \r *-i*^. .J:^ ^M ",«^."', i^ W^- U«»*' ■J^ i^'JlS THE UNIVERSITY . OF ILLINOIS ^;lig.3^r Library i3L;^'3t^'iv^=i;e ■^.'^ .r'Jj O /^>" :*/?*■ Yt^ * v<^ .;rtv t^;-t '*.rv >: ^ . . -^* 'V . ^- , •^:v^.!g^-.;: -^••>'^' ■■'■?-. t ^ LIBRARY OF THE UNIVERSITY of ILLINOIS OF THE ^ f lliiliililllliilliilllillililllllliMllililillllliillliiiliiiiliiiiiliiiiilJitliili^^^^^^^ THE EARTH AND ITS INHABITANTS lyo THE UNIVERSAL GEOGRAPHY By ELISEE RECLUS EDITED By E. G. RAVENSTEIN, F.R.G.S., F.S.S., Etc. VOL. II. FRANCE AND SWITZERLAND ILLUSTRATED BY NUMEROUS ENGRAVINGS AND MARS y^ LONDON J. S. VIRTUE & CO., Limited, 294, CITY ROAD LONHON : IMtD BV J. S. V.KU'B AND CO., UMnH'. CONTENTS. FRANCE. CHAP. I. II. III. PAGE 1 iv VI VII 23 74 Gexehai Aspects. The Country and its Inhabitants Geographical Position; Geology, p. 1. Climate; Rivers, p. 7. The Prehistoric Age of France, p. 13. The Inhahitants of France, p. 16. The Pyrexeks, the Landes, and the B.isin of the Garonne The P)Tenees, p. 23. The Landes, p. 39 The Adour, p. 45. The Garonne, p. 48. Topography. — Pj-renees-Orientales, p. 53. Ariege, p. 55. Haute-Garonne, p. 57. Hautea.- Pvrenees, p. 59. Basses-PjTenees, p. 62. Gers, p. 64. Tarn-et-Garonne, p. 65. Lot-et- Garonne, p. 67. Landes, p. 67. Gironde, p. 69. The Alps, the Rhose, and the Co.iST of the M' diterr.inean General Aspects : Mountains, p. 74. Provence, p. 75. Maritime Alps, 78. Cottian Alps, p. 78. The Alps of Dauphine, p. 80. The Alps of Savoy, p. 8t. The Rhon"- and other Livers, p. 89. Coast-line and Lagoons, p. 108. Climate, p. 114. Top,r/,-aph!/.—Auie, T^. 115. Herault, p. 117. Gard, p. 119. Ardeche, p. 122. Bouches- du-Rhone, p. 124. Var, p. 130. Alpes-Maritimes, p. 134. Vaucluse, p. 136. Hautes- Alpes, p. 139. Basses-Alpes, p. 140. Drome, p. 141. Isfere, p. 142. Savoie.p. 144. Haute- Savoie, p. 146. The Jlra and the B,vsin of the Saone (Franche-Comte and Blrgvndv) General Aspects ; Mountains, p. 148. Lakes and Rivers, p. 150. Inhabitants, p. 156. Topogniphy.—Ma., p. 157. Jura, p. 158. Doubs, p. 159. Belfort, p. 162. Haute-Saone, p. 163. Cote-d'Or, p. 164. Saone-et-Loire, p. 167. Rhone, p. 171. The PLATE.iu OF Central Fr.\nce (Gevavdan, Velav, Auvergne, Rouergue, Limousin, Perigord, Marche, Bovrbonnais) The Cevennes, p. 174. Mezenc and Vivarais, p. '177. Velay, p. 179. The Volcanoes of Auvergne, p. 181. Limousin, p. 186. Forez, Beaujolais, and CharoUais, p. 188. Inha- bitants, p. 188. Topography.— Lozere, p. 189. Ilaute-Loire, p. 189. Aveyron, p. 190. Tarn, p. 191. p. 193. Cantal, p. 194. Puy-de-Dome, p. 195. Correze, p. 197. Dordogne, p. Haute- Vienne, p. 199. Creuse, p. 200. Allier, p. 201. Loire, p. 204. Chaeente and Vendee (Anqoumois, Saintonge, Aunis, Poitov) General Aspects ; Hills, p. 206. Rivers, p. 207. The Coast, p. 208. Topography.— Q^HTenie, p. 212. Charente-Inferieurc, p. 214. Vienne, p. 218. Sevres, p. 219. Vendee, p. 220. The Bisin of the Loire -^-^ General Aspects, p. 222. The Loir.', p. 223. Topography.— Jsievre, p. 230. Cher, p. 232. Indre, p. 232. Loiret, p. 233. p 234. Euro et-Loir, p. 236. Indrc-ot-Lou'e, p. 236. Maine-et-Loii-e, p p S39. Mayennc, p. 242. Loiiolnfericuie, p. 242. 14S 174 Lot, 198. Deux- 2'M. Loir-ct-Clier, 238. Sarthe, A-'A^'^^ iy CONTENTS. on\p. ^ PAOB Viii. Bkittanv (Buetaone) '^i6 Genenil Aspects, p. 246. The Coast, p. 248. Inhabitants, p. 253. Topography. — Morbihan, p. 2o6. Finistere, p. 258. COtes-du-Nord, p. 2G1. Ille-et- VUaiuo," p. 264. IX. The Channel Islands 266 Jersey, p. 266. Serk, p. 268. Guernsey, p. 268. Aldemey, p. 269. X. Lower Nohmanuv and Coje.stin 270 General Aspects, p. 270. Topograph ij. —La Manehc, p. 272. Orne, p 275. Calvados, p. 276. XI. The Valley of the Seine 280 The River Seine, p. 280. Upper Normandy, p. 287. The Coast, p. 289. Topography. — Yonne, p. 290. Auhe, p. 291. llaute-Marue, p. 291. Maruc, p 292. Scine- et-Mamo, p. 297. Paris, p. 299. Seinc-et-Oiso, p. 307. Aisne, p. 310. Oise, p. 314. Euro, p. 314. Scine-Inferieurc, p. 316. XII. Northern Fkance (Basins of the Sonlme and the Scheldt; Picardy, ^Vrtois, and Flanders) 322 General Aspects, p. 322. Topography.— ^maic, p. 331. Pas-de-Calais, p. 334. Nord, p. 337. XIII. The Vosoes (Basins of the MtusE and the Moselle) 345 General Aspects, p. 345. Topography. — Mcuso, p. 350. Ardennes, p. 350. Vosges, p. 352. lleurthc-ot-Mosello, p. 354. XIV. Statistics op France 356 Population, p. 356. Agrieulturo, \>. 359. Slining, p. 304. Mauul'actiir.s, p. 365. Com- merce, p. 366. Social Statistics, p. 371. XV. Government and Administuaiion 374 Local and Central Government, p. 374. JudiciiU Authorities, p. 376. Ecclesiastical Authorities, p. 376. Education, p. 377. .iVmiy and Navy, p. 377. Finance, p. 378. tVilouics, p. 380. Tabular Statement of Area and Population, p. 382. France ; its Departments, Natural KcgionB, and Principal Communes, p. 381. SWHTZERLAND. I. General Aspects. — The Ali-s 391 II. The Jlra 409 III. Glacial Period 414 IV. UivEHS AND Lakes 419 V. Climate, Fauna, and Fi.oka 434 VI. The 1'eoi-le 442 VII. Topography 452 Ticino, p. 453. Valais, Vaud, p. 454. Geneva, p. 456. Fribourg, Ncuchatel, p. 459. Bern. p. •leO. Solothum, p. 464. Basel, p. 465 A.irgau, p. 467. Luzern, p. 471. Schwy;:, Uri, Unterwalden, p. 469. Zug, Ziirich, p. 470. Glarus, Orisons, p. 471. St. Gallen, p. 472. Appenzell, Thurgau, p. 473. SchaflFhausen, 474. Vin. Agriculture, Industry, ami Commerce 475 IX. Government and Administration 490 INDEX 497 LIST OF ILLUSTBATIOJSrS. MAPS PRINTED IN COLOUES. PAGE 1 . France, Geological ..... 4 2. France, Political 53 3. Mont Blanc ^ 86 4. The Volcanoes of Central France • . 177 5. Geological Map of the Paris Basin C. Switzerland ..... 7. Mount St. Gotthard PACK 301 3i)l 4b4 PLATES. The PjTences, as seen from the Terrace of the j Castle at Pau .... To face pnyc '2S \ The Maladetta, seen from the Summit of the j Posets 31 Panorama of Cier and the Valley of Luchon . 56 Toulouse 58 I Peasants from the Valley of Ossau . . ' . 62 Bayonne 63 Bordeaux 69 La Perte du Rhone at BeUegarde ... 89 Carcassonne 116 Marseilles 124 Grenohle and the Alps of BeUedonne . . 142 Mont Auxois and the Statue of Vercingetorix . 167 Lyons 171 Peasants of Auvergnr 1*<6 Le Puy-en-Velay . . . • . . .189 Valley of Mont Dore-les-Bains . . .197 Limoges To face page 200 Source of the Loiret 233 Chambord Castle 235 Nantes 242 Mont St. Michel 252 Paris 299 Prospect from the Terrace of St. Germain . 308 Rouen 317 Lakes of Retoumemcr and Longemer . . 348 Nancy 354 Railway Viaduct of Morlaix .... 367 Le Havre 370 Mont Cer\an, or the Matterhom . . . 398 The Jungfrau 401 The Lake of Thun 427 Geneva 4')6 The WeUhom and the Rosenlaui Glacier . . 464 The Lake of the Four Cantons (Axenstraase) . 470 LIST OF ILLUSTRATIONS. ILLUSTRATIONS IN TEXT. FRANCE. no. 1. The Contour of Franco ... 2. The Iliatorical High-roads of Franco 3. Lithologic.-il Map of tlie British Channel 4. Isothermal Lines of France 5. Lines of Equal Winter and Summer Tern pcrature for Paris 6. Comparative Area of the River B.tsins and average Surface Drainage 7. Comparative Discharge of the Great Rivers of Franco . 8. DoL - ER - Vekchant ok "Merchants' Table," near Locmauiakeh 9 Dispersion of the Aryans . 10. The Stature of Frenchmen 11. Profile of the Pyrenees 12. Slont Canigou . 13. Puy de Carlittc 14. Defiles of the Audo . 15. The Isthmus between the CorbiC^rcs and the Ccvennes 16. The Little Pyrenees . 17. The Maladetta. 18. Mont Perdu . 19. Roland's B ieach . 20. The Amimiitheatiik of Gavahnie 21. Section of the Ancient Glacier of Argelfcs 22. Ancient Glacier of Argoliss 23. The Basques on the French Slope of the Pyrenees 24. View in the Lanhes 25. The Dunes and Landes in the Pays Bom 26 The Basin of Arcachon . 27. TTie Slope of the Landes . 28. TTie .iVncient Coast of the Landes 29. Successive Changes of the Bed of the Gave of Pau 30. The Mouth of the Adour 31. The Suhterranean Course of the Garonne 32. Radiating River Courses of Gers 33. Valleys of Gers .... 34. The Plain of Riviere 3.5. The Estuary of the Gironde 36. The " Passes " of the Gironde . 37. Section of the Passes of the Gironde 38. Port-Vendres 39. Bagneres-de-Luchon 40. The Convergent Valleys of the Garonne, the Ariege, and the Hers . 41. Toulouse 42. Canal of the Neste .... 43. Bagneres-de-Bigorre 4 I. Tumuli of Ossun .... 4.5. Bayonne and the Mouth of the Adour 46. Roadstead of St. Jean-de-Luz . 47. The Alluvial Plain of the Garonne, the Tain, and the Aveyron 2 5 G 8 12 13 1.5 17 19 24 2.; 26 27 29 30 31 32 3 J 34 35 36 38 40 41 42 43 44 46 47 48 49 50 60 51 62 62 64 66 57 58 59 60 61 63 61 60 75 FIO. 48. Cap-Breton .... 49. Bordoau.\ 60. The Wine Districts of the Gironde 81. The Invasion of PhyUoxera, 1»73 62. Zones of Orvnges and Olives . 53. The Mountains of the Moors . 64. The Valli-y of the Arc 65. The Veudon at (U'inson 66. The Gorge, or " Clus," of the Verdon 67. The Glacieus of Oisans 68. AlOlILLE OF THE MeDJE 69. The Glacieu of La Grave 60. The "Forest" of Saou 61. Le s Mouur£ . 62. Mont Blanc as seen from Chamoni.x 63. Ancient Lake Beds in Savoy 64. Perte du Rhone and BuUegarde 65. The Lake of Annecy 66. The Lake of Bourgot 07. Ancient Glaciers of tho Rhone and the Isero . . . • 68. Plain of La Valloiro 69. The Sorgucs of Vaucluso 70. Pontd'.Vrc (\rdecho) 71. I'oNT d'Arc 72. The Roman Aqveduct over the Gard 73. Tho Crau and the Canal of Crapponno 74. The Canal of tho Verdon . 76. The Delta of the Rhone . 76. The Canal of St. Louis 77. The Lagoons of Aigucs-Mortes 78. The Delta of the Aude . 79. Rigoles of tho Canal du Midi . 80. The Mouth of the Herault and Cap d'Agde 81. Leucate and the Roadstead of Fniuqui 82. The Lagoon of Thau 83. Bionomical Condition of the Littoial Region of Herault 84. Etang de Berre • . . . 85. The Canal of Caronte 86. The Prevailing AN'inds at Aigues-Mortus 87. The Port of La Nouvelle . 88. Tho H.arhour of Cette 89. The Protestant Congreg.ations in the South of France .... 90. Beaucaire and Tarascon . 91. The Invasion of the Phylloxera 92. M.arscilles .... 93. The Roadstead of Marseilles . 94. The Mai-solevm at St. Rcmy 95. King Rene's Castle at Tarascon 96. Toulon 97. Hyeres 98. The Gulf of St. Tropez . 99. Nice 100. VUlcfranche .... 101. The Caverns of BAOis.-i-Eov.'-SE 0!S 7 J 71 72 75 76 77 78 79 80 81 82 84 85 86 8S 89 90 91 93 91 9.5 90 97 98 99 100 101 103 104 105 107 108 109 110 111 112 113 114 116 lis 120 122 123 125 126 128 129 130 131 132 1.33 1.15 136 LIST OV ILLUSTRATIONS. VII FIG. PAOt no. 102. Baousse-Rousse .... . 137 163. 103. Cannes and the Isles of Lerins . 138 164. 104. AVIGNO.N 139 165. 105. Col de Larche . 140 166. 106. SiSTERO.N . . 141 167. 107. Valence . . 143 168. 108. Grenoble . . 144 169. 109. Passes over the Alps 145 170. 110. Thonon . . 146 171. HI. The Jura 149 172. 112. The Forest of Chaux 150 173. 113. The Lake of St. Point 151 174. m. The Lake of Chalin . 152 175. 115. The Lakes of the Cluse of Xautua . 152 176. 116. The Lower Valley of the Ain . 153 177. 117. The Great Defile of the Doubs 154 178. 118. The Falls of the DoUjS 155 179. 119. The Combos in 1834 156 180. 120. The Mountains of Jlorez and St. Claude 158 181. 121. The First Terrace of the Jura, between 182. Lons-le-Saunier and Salins 160 183. 122. Besan(;on 161 1S4. 123. BES.is<;oM 162 18.5. 124. Belfort 163 186. 125. Belfort 164 187. 126. Vesoul 165 1S8. 127. The "Wine District of Cote-d'Or 166 189. 128. Le Creusot 168 190. 129. Le Ckecsot 169 191. 130. Lvons 170 192. 131. The Enviions of Lvons . 172 193. 132. The Mountains of Espinouze . 175 194. 133. The Causse of Mi jean 176 195. 134. The Defile of the AkdIche, xe.\ii 196. EUOMS 178 197. 135. The Hills of Coiron .... 179 198. 136. LePuv ISO 199. 137. The Ply de l'Aiguillier, Moxt Doue 1S2 200. 138. The Puy of Sancy and the Lake District 183 201. 139. The Chain of the Puy de Dome 184 202. 140. Volvic 185 203. 141. The Meanderings of the Lot 186 204. 142. The Rapids of Lalinde . 187 205. 143. Roquefort 191 206. 144. DecazevDle 192 207. 145. Clermont and Montferrand 195 208. 146. Thiers 196 209. 147. Section of the Carboniferous Strata oi 210. St. filov 197 211. 148. Tayac and Lcs Eyzies, on the Vezere 198 1 212. 149. 201 213. 150. Vichy 202 214. 151 203 215. 152. The Head- Waters of the Tou^Te 207 153. 2.8 2! 6. 154. Xoirmoutier ..... 209 217. 155. 210 218. 15-. The Ancient Gulf of Poitou . 211 219. 157. 212 220. 158. The Brandy Districts of Ch.arente . 213 221. 159. Rochefort and the Lower Charente . 214 160. La Rochelle . . ... 215 222. 161. La Rochelle 216 223. 162. AhS-E.v-R^ 217 224. PAOl , The Gulf of Aiguillon . . . .218 , Les Sables-d'Olonne .... 220 The Bill of the -Ulier .... 223 The Authion 224 La Sologne 225 , The Erdre 226 The L^ke of Grand Lieu . . .227 La Grande Briere 228 Paimboeuf 229 The Mouth of the Loire . . . .230 Le Croisic and Batz 231 Cleans 233 Chartres 235 Tours 237 Angers 238 The t-LATE QC.VRRIES XF.AR A.NGERS . 240 Le Mans 241 Nantes 243 St. Xazaire 244 The Landes of Lanvaux .... 247 Morbihan 248 The Peninsula of Quiberon . . . 249 The Headland of Comouaille . . .250 The Bay of St. Michel . . . .252 Bketox Peasants 253 Approximate E.\tent of the Breton Tongue 254 WoMEX OF Cakcale .... 255 Lorient and Port- Louis .... 257 Concameau 259 Brest 260 Morlaix 262 St. Malo and St. Servan . . .263 View op St. SIalo 264 The Channel Islands . . . .267 The Forest of Andaine . . . .271 Meadows of Normandy . . . .272 The Sinks of the Aui-e . . . .273 Cherbourg ...... 271 The Beach at Grasville . . . 275 Caen and the Mouth of the Ome . .277 TrourUle 278 The Ra%-uied Plateau of Upper Burgundy 281 The Lake Reservoir of Settons . . 282 The Source of the Seine . . . .283 The Basin of Vitry-le-Francois . . 284 Section of the Paris Basin . . . 285 The Estuarj- of the Seine . . .286 The District of Bray .... 287 Da'.es on the Coast 288 Cape de la HkvE 289 The En%'irons of Langrcs . . . 292 Chalons and its Camp .... 293 The Bifurcation of the Grand Morin at Sezanne 294 Reims and Epemay .... 295 The Cathedral of Reims . . . 296 Fontainebleau 297 Paris and the Great Highways of France 298 The Growth of Paris .... 299 The Comparative Growth of London and Paris in Popluation .... 300 The Areas occupied by London and Paris 301 Notre-Dame 302 The Louvre 303 LIST OF ILLUSTEATIONS. no. PAoi: 225. The New Opera Hov.'se, P.\k IS 304 Fin. 226. Paris aud its Aqueducts . 305 280. 227. Paris and its Forts . 300 281. 228. St. Germain-cn-Laye 308 229. Laon .... 310 282. 230. St. Qucntin 311 231. Compicgne 312 283. 232. ChantiUy 313 284. 233. Les Andelys 315 285. 234. Rouen and its Environs . 316 286. 235. Le Ha\Te . . . 317 287. 236. The Cliffs of Etketat 318 288. 237. Fecamp .... 319 289. 238. Dieppe .... 320 290. 239. The HiUs of Boulogne . 323 291. 240. The Estuary of the 8ommo 324 292. 241. The Ancient Gulf of Flanders 325 293. 242. The Moercs of Dunkirk . 326 294. 243. Section of the Strait of Dover 327 295. 244. Strait of Dover and the Proposed Tunnel 328 296. 245. Section of the Proposed Tunnel 328 297. 246. Extent of the French and Flemish 298. Languages .... . 329 299. 247. The Coal Basin of Northern France 330 300. 248. PfeHONNE-SUR-SOMME , 331 301. 249. Amiens . 332 30i. 250. Amiens Cathedral . 333 303 251. Boulogne .... . 335 304. 252. Calais 336 305. 253. Valenciennes .... 338 306. 254. Lille 339 307. 255. Koubaix and Turcoing . 340 308. 256. The Belfry op Beroues . 341 309. 257. Gravelines .... 342 310. 258. Dunkirk 343 311. 259. Glaciers of the Vosges 346 312. 260. The Lakes of Gerardmer and Longe- 313. mer . 347 314. 261. Meanderings of the Meuse 349 315. 202. Charle\-ille and Slezidres . 351 316. 263. Epinal 352 317. 204. Nancy 355 318 205. Increase of Population in the Principal 319 Countries .... 357 320 260. Density of the Population in France 358 321 267. Wheat Harvests 359 322 268. Produce of the Vineyards 360 323 269. Pastures and Meadows . 362 270. Average Value of Agricultural Produce, 324 with the Exception of Wine 363 325 271. The Increase of Steam Engines 365 326 272. The Railroads of France . 367 327 273. Canals and Navigable Rivers . . 868 328 274. The Commercial Marines of the World . 369 329 275. The Navigation of French Ports 370 276. Map exhibiting the Educational Condition 330 of France .... 372 331 277. View of Moxaco . 370 332 278. Comparative .\reas of France and of her Colonies .... . 380 333 279. The Languages of France . 381 334 SWITZERLAND. PAOE Val Piora and the Lukmanior . . . 394 Diagram showing the Slope of the Valleys South and North of the St. Gotthard . 395 Sources of the Rhone, the Ticino, aud the Toce 396 The lUgraben 397 The Matterhom (Mont Cer\-in) . . 398 Glaciers of the Bernese Alps . . . 400 Blv.mlisali' Glacier .... 401 The Diablerets 402 The Windgalle 405 Piz Bernina 406 The Glaciers of Tschiorva and Morteratsch 407 The Valley of Tra vers . . . .410 The Cluse of Undervelier . . .411 Meanderings of the Doubs at St. Ursanne 412 The I^ake of Joux . . . . .413 TheCatogne 416 Ancient Glaciers of Eastern Switzerland . 417 The Lake of Locarno (Lago Maggioro) . 420 The Lakes of Lugano and Como .421 The Aletsch Glacier 422 The Lak(! of Geneva . . . .424 Section of the Lake of Geneva . . 425 The Lakes of Neuc hutel, Bienne, and Morat 426 The Lakes of Brienz and Thun . . 427 The Grindehvald Gl.icier . . . .428 The Swamps of the Linth . .430 The Sources of the Rhine . . .431 Rain Map of Switzerland . . . 435 An Ali'Ine Club Cabin .... 437 Pfaffikon Lake 443 The Pile Dwellings of Switzerland . . 444 Ethnographical Jlap of Switzerland . 447 C0STf.ME8 IN Uki 449 Costumes in Frihouho .... 450 Eastern Extremity of the Lake of Geneva 455 Geneva 456 The Lake of Morat 459 Bern 461 View op Bekn 462 Interlaken 463 Bienne and the New Bed of the Aar . 464 Basel 466 Porrentruy ...... 466 Confluence of the Rhine, Aar, Eeuss, and Limmat ...... 467 The Lake of the Four Cantons . . 468 The Simmenthal ..... 476 Industrial Map of Switzerland . . . 480 The Ebexe Fluh 481 Passes across the Alps .... 482 The Devil's BkidijE and the Road of THE St. Gotthard .... 483 , Railways of S^vitzerland .... 484 The Tunnel of the St. Gotthard . 4,S5 Diagram of the Tunnels of the Simplon and the St. Gotthard . . . .480 The Pass of Maloggia . . . .487 , The Mo.vch 488 A UNIVERSAL GEOGRAPHY, FRANCE. CHAPTER I. GEXEKAL ASPECTS.— THE COTIsTEY AXD ITS DOIAniTAXTS. Geogkaphical Positiox. — Geology.* EAXCE occupies a medium extent amongst those countries of the ■(vorld which have played a distinct part in politics and in the history of civilisation. Smaller in area than either China, Russia, the Brazils, or the United States, it is nevertheless for more con- siderable than that of either Greece, Portugal, Switzerland, Holland, or even of England, all of which have left their mark upon the march of human history. Scarcely covering the 225th part of the habitable portion of the globe, its dense population has nevertheless enabled it to plaj' a part quite out of propor- tion to its area. It would be presumptuous if we claimed on behalf of France a sort of moral hegemony amongst the nations of the world. Still, within the comparatively small territory bounded by the iVlps and Britany, by the Pyrenees and Yosges, there have taken place events whose influence has made itself felt to the farthest corners of the world. In arts and science France has found worthy rivals since the beginning of this century, and there are other nations which claim to march at the head of civilisation. But this merely proves that the area of the civilised world has been enlarged — that there are other nations capable of giving birth to initiatory movements. But France has at all times performed her share of this work of human progress, and looking to the influence which her ideas have exercised throughout the world, it would be difficult to conceive a future history of nations with France blotted from the map of Europe. To a very large extent Dufrenoy et Elio de Beaumont, "Mumoires pour scrvir a ime Description gcologique do la France' VOL. ir. 2 FRANCE. the inhabitants of France arc indebted for the eminent position they hold to Iho climate, the soil, and the geographical features of the country which they inhabit, and a faithful description of these will be our task in the following pages. It has often been said that Franco enjoys oxceptiomil advantages from its position between the Mediterranean and the open ocean. This position has made it the intermediary between the old coxmtries of the ^loditerranean and Northern Fig:. 1.— The Contovr ov FiiAxrn. 5| tl J] a| /| o\or/t.n.yi i j \3 1» \5 . \s' ,,^ftt AclatU iaundaty. ...... .^isrA diagonals cFJi-aat». Europe. Nowhere else in Europe is communication between the coasts of the Mediterranean and the Atlantic equally facile. The plains of Poland and Russia may offer fewer obstacles to intercommunication, but the Baltic and the Black Sea, which they unite, are remote inland seas. In Central Europe the Alps are an obstacle to the exchange of ideas and merchandise between the North Sea and the Adriatic, but in France great natural highways join the Atlantic and ]\Iedilcr- ranean ports and river basins. Mountainous Europe may be said to terminate at GEOGEArillCAL POSITION.- GEOLOGY. 8 the foot of the Ceveimes, and the great diagonals of the ■western portion of that continent, yiz. that drawn from Germany to the Iberian peninsuhi, and that connecting Italy with England, intersect each other ■within the boundaries of France, ■which is thus marked out bj' nature as the great centre in ■which European thought may be elaborated, where North and South may exchange their ideas. The contour of France is distinguished by compactness no less than by a certain elegance. A meridian passing through the capital connects the two extreme points of the territory, dividing it into two symmetrical portions in such a manner as to form an octagon. Oceanic alternate ■with land boundaries, and these latter for the most part consist of mountain chains, ■n^hicli separate France very distinctly from neighbouring countries. The principal- of these natural, frontier ranges are the Pyrenees, the Alps, the Jura, the Yosges, and the Ardennes.* We may even include amongst these bastions the granitic heights of the xi.rmorican peninsida, which overlook the fields of Normandy and Anjou to the west. To these sterile hills France is probabh- indebted for not having been conquered by England, for if Britany had been capable of attracting hardy Anglo-Saxon settlers, it ■would have formed a link between Guyenne and Normandy, and these provinces might then have remained for ever in the jiosses- sion of the foreigner. Curiously enough, it is the highest amongst these frontier ranges which separate the French from nations of kindi'ed origin, ■whilst the less elevated ranges consti- tute the boundaries towards the Germanic countries. The Pyrenees, a most formidable barrier, hardly to be passed in winter, divide France from Spain ; the Alps, an obstacle almost equally formidable, separate it from Italj-. But farther north, the Jura and the Vosges, which are of comparatively small height, separate the French from the German-speaking populations, whilst in the north-east, in the direction of the ravined plateau of the Ardennes, the boundary in certain parts is completely open and quite conventional. The frontier there has varied much in accordance with, the fortunes of war, but the two conterminous races did not assimilate. In the south, however, had there not been the Pyrenees and the Alps, it is to be assumed that instead of three Latin nations — French, Spaniards, and Italians — each possessed of some special genius, there would now be but one. France is thus doubly privileged. Its southern mountain barriers have pre- served it from a premature fusion with other Latin nations, whilst in the north, where the frontier is open, it was preserved by the natural antagonism of race, and yet, owing to the facilities of communication, it rendered possible an extensive commerce and an exchange of ideas. Paris, placed close to this open frontier, was thus marked out by nature as the capital of the country : valleys and hills con- verge upon it ; it is the principal seat of commerce and industrj*, and whether in peace or war has always held the foremost place. The physical features of the interior of France arc harmonious in their very • Development of coast-line, not including imlentations of less than three miles, 1,030 miles (Channel C9fl, Atlantic S61, llediterranean 382 miles). Development of land frontiers, 1,319 miles (Belgium 286, Luxemburg 9, Germany 199, Switzerland 2-lG, Italy 255, Spain 351 miles). Tutal circumference, 3,288 miles. B 2 4 FllANCE. contrasts. A grauitic plateau of a triaiigulav coiilouv occupies the centre of the countrj'. In the east it is bounded by tlie deep valley througb which flow the Saone and the Rhone ; on the south-west it is bounded by the valley of the Garonne, whilst its north-eastern boundary runs parallel with the Loire. The granitic mountain of Roucrguo and the heights of Morvan are attached to this plateau-like peninsula. Porphyries and lavas have been erupted through the granites forming the nucleus of this plateau, and on all sides it is enveloped by rocks of more recent age, as the bones of a human body are by flesh. This comparison may be carried even further, and we may liken the granites and other ancient rocks of the Alps and I'yrenecs, of Poitou, Britany, and Cotcutin, of the Vosges and Ardennes, to the skeleton, whilst the sedimentary rocks depo- sited in the valleys separating them represent the flesh. A zone of Jurassic limestones surrounds almost completely the granitic moun- tain mass of Central France, spreading out in the north-east along the foot of the Vosges and Ardennes, and bounding in the north-west the peninsula of Britany. A corresponding zone of cretaceous rocks extends along the northern foot of the Pyrenees, from sea to sea, whilst the crystalline rock niasses of the Alps rise above the strata of Jurassic formation. The s^Jacc occupied by rocks of more recent origin than the chalk and Jurassic limestones is of small extent. Geological formations and the relief of the soil divide France into a number of historical and geographical regions. The elevated granitic plateau of the interior, as well as the mountain barriers on the frontiers, must at all times have exercised a deterrent influence upon the surrounding populations, whilst the rich and fertile plains extending between them proved a powerful attraction. The rugged plateaux, however, offered a secure shelter, whilst the plains were open at all times to the incursions of enemies. Down in the valleys man struggled for the posses- sion of the land ; in the mountains he held it securely. The historical contrast between this barren central plateau and the surrounding lowlands is very evident. The valley of the Rhone in the east, the basins of the Garonne and the Charente in the west and south-west, and the huge bend of the Seine in the north, pulsate with life, and the number of mountaineers who descended into these inviting plains has been greater by far than that of the lowlanders who sought a home in the moun- tains, for men, like water, always travel downhill. The direction of the great historical highways of France has necessarily been influenced by the configuration of the soil thus indicated. From Paris i-outes radiate in all directions towards the north, the east, and the west, for there they encounter no obstacles, but to the south of the Seine and the Loire these routes had to accommodate themselves to the relief of the soil, and there are in reality but two of them, viz. the great Roman road which leads across the lowest part of the plateau of the Cote d'Or into the valley of the Rhone, and which Cscsar followed when he invaded Gaul ; and the great Iberian road, which passes to the west of the central plateau. A third natural highway joins the extremities of these two roads in the south. This latter skirts the southern slopes of the Cevennes, end joins the Mediterranean to the basin of the Garonne. Nearly all the towns LIBRARY OF THE UNiVERSirr of ILLINOIS. GEOGRAPHICAL POSITION.— GEOLOGY. 5 which have phiycd a great part in historj' are situated along cither of these roads. "We need only instance Orleans, Blois, Tours, Poitiers, Bordeaux, Toulouse, Car- cassonne, Narbonne, IMontpellior, Nimes, Aries, Avignon, Lj-ons, Chalons-sur- Saone, and Dijon. It has been noticed that the larger towns along these roads are generally two stages apart, the intermediate stages being marked by places of less consequence. In fact, these towns were originally merely military stages, the distances being accommodated to the marching powers of infantry and cavalry. Fi'j. 2.— TiiF. IIisTonicAi. TIigii-ho.\ps of Fkance. 7i <=: >' . >^ -^J .^-^ ME^t^^" v^ \i- yi V "Where exceptions occur, thc\- are due to special features of the soil or to the neces- sities of commerce. In our own days railways have almost annihilated space, and towns no longer grow up at such regular intervals. It would be interesting to ascertain the great routes of the migration of man and animals in prehistoric times. But this is a matter of no inconsiderable diffi- culty. Constant Prevost, Delessc, and others have attempted to construct maps exhibiting France during various geological epochs, but their value is merely 6 FEANCE. conjectural, for, irrespective!}' of tlie uncertainty still existing with regard to the age of certain rocks, it is almost impossible to tell to what extent the more ancient formations have disappeared, owing to subsidence or denudation. In the Silurian age it would ajipcar Gaul consisted merely of an elongated peninsula extending from where the Aljis are now to modern Britany. Subse- quently a wide strait separated this peninsula from a few Alpine masses, then recently upheaved above the ocean, whilst newly formed land joined it to the Fig. 3. — LiTHOLOGICAL MaI" Ul' THE BllITISII ClIANNEL, SllOWINO THE AxClENI CONNECTION UETWEEN BlUTAXY AND ExOLAXD. According- to Dclesse. A" Ivo'E.orCr- vifo" ^' yn' ■i-Un- l°|t»0' 1 i i":',f.|'::ri Mi li'l'tj" ■' m^-r" ^«t ■>' '''O'' M "if p :m' ^ . ,1 1,1 ■ i ' \ - '\^A ■"IWofPons O" ."1 ■ ' '---.r ... Land. Sea Bottom JfocAy. mil Sojid^- A Pj'renees and to England. The rocky bottom of the channel, as laid down on M. Delesse's lithological map, shows where the union between the two Britunics existed. When the liassic strata were being deposited in the gulfs of the sea, the contours of the great plateau of Limousin and its outer fringe, consisting of the Cevennes, the Forez, and the IMorvan, were pretty much as they are now, excepting that a deep strait intersected the southern portion. Four wide arms of the sea separated this plateau from the Ardennes and Vosges, the Alps, the Pyrenees, and Britany. The framework of modern France had thus become CLIMATE. -]RI\'ERS. 7 apparent, and cacli subsequent formation helped to fill it up. Daring tlio cretaceous age the central plateau was finally united on the one hand to Britany, and on the other to the Vosgcs and the Ardennes : Uoulonnais rose like an island in the centre of the sea to the north. At the eonimcnccmcnt of the tertiary age this sea had become a gulf, the estuaries of the Garonne and the Adour had much diminished in size, lakes were drained or filled up by alluvial deposits, and at the time of the last glacial epoch, the date of which cannot be fixed even approximately, the contour and relief of France were nearly what they are now. The innumerable agencies, however, which change the surface of the land arc still at work : mountains are being washed away, lakes silted up, rivers change (heir courses, extend their deltas, or enlarge their estuaries, while secular oscillations of the land effect changes along the coast. As regards these latter an upheaval during historic times has been distincth' traced along the Mediterranean coasts. On the Atlantic seaboard the coast of the Landcs has subsided ; to the north of the Gironde we meet with incontestable proofs of an upheaval ; and along the British Channel there are again indications of a subsidence, which extends through the Netherlands as far as Denmark and the southern shores of the Baltic. These slow movements have resulted in changes which have exercised an appreciable influence upon the march of history. Climate.^Eivers.* There can be no doubt that the climate of Franco has undergone changes since the beginning of the historical period, although it would be difficult precisely to deter- mine their extent. The destruction of forests, the draining of swamps, and the embankment of rivers must necessarily have affected local climates. There exist no precise data in that respect, for exact meteorological observations are only of recent growth, but a few general considerations prove it inconfcstably. Certain plants can no longer be cultivated at the same altitude as during the Jliddle Ages: olive, fig, and orange trees have retired farther south; tlie vine no longer grows in Picardy and along the Channel. This retreat of certain plants, however, may be due to our improved means of communication with countries where their cultivation yields a richer harvest than under the inclement northern skies, and we cannot therefore conclude from it that the climate of France has detoriorated since the Middle Ages. But that changes in the climate have nevertheless taken place is amply proved by an examination of our fossiliferous strata, from which we learn that a sub-tropical and an arctic climate succeeded each other at intervals. France at the present moment is divided into two climatic zones by the gra- nitic masses of the great central plateau. The mean temperature to the north of that barrier varies between 50^ and 54^ F., whilst to the south of it it gradually rises to 50'^. The contrasts are still greater if we take into account the moistun^ of the air, rainfall, winds, and all those other meteorological phenomena which constitute climate. ^^'e (hen find that the northern Atlantic slopes of Finance • Bouilot, '■ Vuiialions de Liititude ct dc C'linmt." 8 FBAXCE. form a p^rrlon c f Western Europe, Trhilst tte soutliem M^ediferranean slopes are almost Airic-iii iz. their aspect. Eastern and Western France contrast likewise, though not in so marked a manner. The Atlantic coasts are exposed to the influence of the gulf-stream and of warm south-westerlv winds, and their temperature is more elevated than might be condoded from their latimdes. As we proceed inland the warm Atlantic Fig. 4. — IsoiHEKaAi. Leces of Fbxsce. BT5LP.«aoa. Erhard,. current giadnallr loses its power, westerly winds blow less frequentlr, and the mean temperature of Cherbourg is thtis nearly 3" higher than that of Terdun, in spite of its lower latitude. But this decrease in mean temperature is not the only contrast between the extreme west of France and the inland districts, for the seasons in these latter present greater differences. The climate along the Atlantic coast is essentially a maritime one, and the differences between the extremes of temperature are not CLIMATE.— EIVEES. vciy great. In tlic cast, where llic equalising influence of tlic ocean is less felt, the summers are warmer, the winters more severe tluin on the coast. The farther wo iirocccd inland tlic more will lines of equal winter and summer temperature be found to differ. Localities in Eastern France, whose mean annual temperature is inferior to that of localities on the coast, nevertheless enjoy a higher tempera- ture than the latter during summer. The influence which these varying con- Fig. 6. — Lines of Euial 'Winter and Simmeu TEMrEii.VTiRE roii Pauis. 'I » " January 36 "n F. w V It July OS "i^ F. ditions of temperature exercise upon vegetation is apparent, for some plants require a comiJaratively high mean annual temperature, whilst others, like the vine, do not suffer from frost, but require a high summer temperature. The mean direction of the winds in France has been computed by Kacmtz and Martens at S. 88'^ W. ; that is to saj', they blow up the lower valley of the Loire. The proportions between easterly and westerly winds is as 100 to 102, that 10 FEANCE. between nortlicrly and southerly winds as 100 to 103. The prejwnderanco of westerly and southerly winds w'ould be still more marked, did not the Pyrenees oppose an obstacle to their progress. Along the Atlantic seaboard north-westerly winds prevail, on the Channel south-westerly winds. Their direction, as a matter of course, is modified by local causes and the configuration of the land ; but thus much may be assumed as certain, that the atmosphere of France is being continually renewed from the west. In the valley of the Lower Rhone, which forms almost a world of its own as regai'ds climate, the direction of the winds is quite different : they blow up and down this narrow valley, either from the Mediterranean or from the north. Between the Spanish frontier and the Rhone, as well as to the east of that river as far as the Hyeres, north-westerly winds predominate, whilst along the valley of the Rhone itself the prevailing wind blows from the north, in the direction of the Mediterranean. Thus, whilst the Atlantic slopes of France are exposed to a preponderance of sea breezes, it is the land winds which prove victorious on the Mediterranean slopes. The configuration of the soil exercises as great an influence upon the distribu- tion of the rain as it does upon the direction of the winds. The country, in that respect, may be divided into three zones. Summer rains prevail in the north and in the centre, as also in Germany and nearly the whole of continental Europe ; autumn rains prevail in the west ; and on the Mediterranean slopes two rainy seasons can be distinguished, viz. one in the beginning of the year, the other in autumn : summer rains are rare there. The amount of rain varies exceedingl}^ in different localities. Along the sea it is gcnerall}' abundant ; the quantity decreases as we proceed inland, but the mountains in the interior of the country form a second region where the pre- cipitation is considerable, and on a map of France showing the distribution of rainfiill these mountain ranges stand out very distinctly. As a general rule the quantity of rain increases from west to east, and from north to south ; that is, in the direction in which the land rises. In the south, where the air owing to higher temperature is capable of holding a greater amount of moisture in suspen- sion, the rain after storms sometimes descends in torrents. Upon the whole, however, the rainfall near the Mediterranean is less than near the Atlantic, and the air there is drier, a feature sufficiently explained by the prevalence of land winds. There are onlj'- three stations in France at which the annual rainfall approaches eighty inches. These are the Pyrenees of Gavarnie, which inter- cept the moist winds blowing from the Bay of Biscay ; the mountains of the Tanargue, between the sources of the Ardeche and Loire ; and the Alps to the north of Gap. On the western slopes of the mountains and on the plateau of Limousin the rainfall exceeds forty inches. It is least in a district embracing Meaux, Troyes, Epernaj', and Compiegne, which is remote from the sea as well as from the mountain region, is badly wooded, and consists for the most part of chalk. At Dunkirk, likewise, it rains but little, for the winds prevailing there part with CLIMATE.-EIVERS. H their moisture whilst passing across Enghaud. From a careful computation made I'V 31. Delesso it appears that the rainfall throughout France averages 30-3 inches. The number of rainy days varies quite as much as the amount of rain. At Abbeville rain falls on 175 days in the year, at Lille on 1G9 days, whilst Marseilles has only 55 and Hyeres 40 rainy days. As a rule the number of rainy days decreases as we travel towards the south-east, and where this is the case the rains are proportionately heavj'. Storms, which occur generally during summer, afflict as a rule the centre and the east of the country, and M. Becquerel has shown that they blow ordinarily along the great valleys. Speaking broadly. Franco may be divided into seven climatic regions, of which that of the great granitic plateau occupies the centre. Britany, in the north-west, is remarkable for its equable temperature ; the northern region, named after its principal river the Seine, is distinguished by a paucity of rain ; while in the region of the Meuse and the Yosges the extremes between cold and heat are greatest. The three southern regions are distributed in an analogous manner. The climate of the Gironde and of the Rhone is mild and humid ; that of the Mediterranean is changeable ; heavy rains alternate with periods of drought, and the winds are high.* The climate of a country is reflected to a great extent in its rivers. Unless these are fed oy glaciers or flow for considerable distances underground, they reflect the succession of seasons verj-^ faii'lj*. Great is the contrast between the torrents of the Mediterranean and the rivers and rivulets of hilly BritanJ^ On the southern slopes of the Cevennes, scorched in turn by the sun or lashed by showers of rain, the torrent beds, dry during the greater part of the year, are converted after rains into mighty rivers, sweeping before them vast masses of debris. These icadis of Languedoc differ most essentially from the quiet rivulets of Xormandy and Britany, which flow steadily throughout the year, and scarcely ever overflow their banks. The rivers of France flow in opposite directions towards the Atlantic and the Mediterranean. The Ehonc, rising In a glacier like the Rhine, and flowing through a large lake, takes Its course to the south. Where It traverses the plain which formerly was merely a gulf of the sea, it receives numerous tributaries descending from the Alps and the Cevennes, and when the alluvium brought down by it shall have filled up the Lion Gulf, It will number amongst Its affluents Climatic Regions. ^ Mean Temperature (F). ...^uv i>co.u.»= Year. Summer. Winter. • Limousin (Limoges) .... .51-8 — — Britany (Brest) 5!1 62-2 41-8 ITie Seine (Paris) 500 040 3"-9 Vosges (Nancy) 500 65-1 35-2 Gironde (Bordeaux) . . . .■ 5C-3 "M 430 Rhone (Lyons) 53-2 70 371 Mediterranean (Jlontpellier) . 58-3 71-6 42-4 Average for France . . . . 51-8 G80 410 Mean Direction of Winds. Rainfall, in. Days with Seasons Rain, of heaviest No. Raius. — 3G — Autumn AV. 23 208 do. ■\v. 20 154 Aut. and Sum. S.W., X.E, . 31 120 Summer "W. 32 150 Autumn X. 31 110 do. x.w. 20 — • Spring i- Aut. AV. 30 HO Autumn 12 FEANOE. the Herault, Orb, Au'de, and other rivers of Roussillon, for all these, as well as tho rivers rising in Provence, converge upon that gulf. On tho other hand, the rivers flowing down the Atlantic slope take a divergent course, and a line drawn through their sources is much shorter than one con- necting tlieir estuaries. As to Britany, it constitutes a hydrographieal region apart ; and neither its commanding position nor its excellent harbours have countervailed the disadvantage of its lying outside the great river systems of France. Fig. 6. — CoMrARATivE Area op Riveu Basins an-d Aveuaoe Surface Drainage. Horizont,il Scale 1 : 20,000,000. Verticil Roale 1 : 50. ; 2 : 20.000.000 J8^o ii'--' So^o ;. % Average/ Raifu Foil in/ Franxx^. A vera/^e^ XurFcu^^ ir^ France/' .■ i-:d Jifion£' Seine/ Glroiide/ Loire/ Formerly it was supposed that the waters discharged by large rivers like the Loire or Seine far exceeded in amount what could be derived from the rains, and their sources were consequently supposed to communicate with reservoirs fed by the ocean. Bernard Palissy and Denys Papin (1669 — 72) first demonstrated the erroneousness of this view, and careful observations have revealed the fact that only one-third or at most one-half the rain that falls throughout France finds its way back to tho sea by means of the rivers, the remainder being absorbed by the vegetation or evaporating.* Hirer. Length of Course. Miles. * Biver systems of Franco according to Delesse, Cli. Martins, Thoni^ de Gamond &c. Surface Drainage in Millions of cub. ft. 6.3,500 (?) 772,100 223,600 (?) 1,096,700 106,000 1,312,000 247,200 (?) 71,000 (?) Somme 133 Seine 482 Vileine 143 Loire 009 Charente 224 Gironde 016 Adour 187 139 Aude Ehone (with Saone 'J and Doubs) 3 Moselle (in France) . Meuse do. Scheldt (Escaut, do.) France . . . , 637 194 318 75 Area of Catchment Basin. Sq. m. 2,144 30,927 3,707 44,459 3,860 35,962 6,564 2,510 38,096 2,606 2,898 2,548 200,315 Average Kaiufoll. In. 25-2 24-8 27-6 27-2 33-4 32-5 39-4 27-0 37-4 29-.5 28-3 23-6 30-3 EainfaU in Millions of cub. ft. 12.5,443 1,646,380 237,327 2,089,356 300,190 2,022,290 000,386 160,690 3,310,340 178,770 190,710 140,858 14,109,000 1,915,430 55,660 (.?) 88,290 63,500 0,710,000 Discharge per Second. Cub. ft. 2.013 (?) 24,510 3,880 (?) 34,786 3,354 (?) 41,600 7,840 (?) 2,225 (?) 63,850 (?) 1,770 (?) 2,800 (?) 2.014 (?) 212 000 (?) THE PEEHISTOEIC AGE OF FEANCE. 13 The rain which finds its way through rivers to the sea is one of the most powerful geological agents. The ravines and vallej-s of the Pyrenees, the C^vennes, the Alps, and the Jura exhibit its power of erosion : the la3-ers of sand and mud deposited along the banks of the Loire after floods testify to its giving birth to new land, and at the mouths of the Rhone we may see how a river causes the land to encroach upon the sea. The fecund soil of the Limagne, Touraine, Agenais, and Bigorre, those gardens of France, is entirely a gift of the rivers. The rivers, owing to the fertility of their banks, have proved the most power- ful agents of civilisation in France, as everywhere else. In former times they alone were available for the transport of merchandise and travellers on a large scale, and most of the great towns grew up on their banks. Towns not situated on navigable rivers, such as Nimes, Montpellier, Dijon, and Reims, were mere stages on the roads connecting these river highways. Roads and railways have to some extent deprived the rivers of the importance they enjoyed in former times, and considerable towns have sprung up far away from them, near mines, mineral springs, or line scenery. St. Etienne, Le Creuzot, and Bagneres-de- Kg. 7. — Comparative Discharqb op the Great Rite&s op Feanck, Horizoatal Scale 1 : 4,000. Shone Seinir Girondc' Xofre/ J%^mA/)l£,^/' Frana/. Luchon are of this class. The rivers, on the other hand, are being rendered more useful to man from day to day. Canals are dug to connect them or to irrigate the fields in their vicinity, embankments are thrown up to regulate them, and their water is rendered available as a motive power. Still most of their water is allowed to run to waste, and the day is yet apparently very distant when they will be exhaustively utilised in the service of man. The Prehistoric Age of France.* France had its inhabitants long before the events of history were placed on record. Human bones mixed with those of animals, rude imj)lements of peace and war, and rudimentary works of art amply prove this. "With Belgium and the basins of the Rhine it is probably richer in these prehistoric remains than any other country, and many caves and heaps of debris have become famous on account of them. Anthropologists are generally agreed that the most ancient examples of human • Hamy, " Paleontologie humaine;" Gabriel de Mortillet, "Tableau arcbeologique de la Gaule;" Lartet et Christy, " Reliquiie Aquitanicse ; " Broca, " Compte-rendu du Congrea intern, de Paris, 1867." VOL. II. C 14 FRANCE. workmanship are the flint implements discovered by M. Bourgoing near Thenay, in the valley of the Cher. In the tertiary age, when the contemporaries of acero- therium and mastodon fashioned these rude implements, the aspect of France was very difEerent from what it is now, and there existed neither the same plants nor the same animals. Centuries passed away, and the men who dwelt in the plains bordering upon the Somme and the Seine, on the plateaux of Central France, and along the foot of the Pyrenees had learnt to fashion tlint implements of a superior kind, and with these they pursued the elephants, hippopotami, i-hinoceroses, and other animals which at that time roamed over the lands of the Gauls. At a subsequent period, when the rhinoceros had been exterminated, when man had expelled the bears from the caverns to dwell therein himself, and when the horse, with the mammoth, was one of the commonest animals, these stone implements began to be fashioned in greater variety, to serve the needs of hunters, fishing, and domestic labour. Later still, the bones and horns of animals were made use of, and frequently the figures of animals and even of men were engraved upon them. Artists must have lived at that time, though their names are for ever lost to us. Ornaments and figures which they engraved upon their stag-horns are the same in style as those met with subsequently on the vases dating back to the age of dolmens, on the arms of the ancient Gauls, and even on some GuUo- Roman monuments. Once launched upon the path of invention, man never turns back. Some sort of relapse appears to have taken place after the reindeer age, but this applies only to the ornamentation, and may be accounted for bj' an inflow of immigrants inferior in civilisation to the older inhabitants of the country. At the same time new weapons came into use ; man had acquired the art of polishing stones, and of making durable earthenware. Later still he learnt to cultivate the soil, and to train domestic animals. The old cave dwellings no longer sufficed for his wants, houses arose in the plains, and solid structures of stone were erected by the men of the neolithic age, wherein to deposit their dead. They threw up entrenchments as a defence against enemies, and those who lived along the margins of rivers or lakes erected their dwellings upon piles, thus securing themselves against unex- pected attacks. In France itself the^e lake dwellings are scarce, but they abound in Switzerland. No written record or tradition reaches back to that neolithic age, but we know from the objects discovered in tombs and dwellings that bronze had come into use. Imported from abroad, we find it applied to the most varied uses, either cast or wrought. A new era began with the introduction of iron, which was fashioned not only into weapons, but also into tools of every description. Thenceforth human art and industry took a rapid development. The numerous grave-hills scattered over the country abound in curious objects deposited there by the relations of the defunct. History begins to dawn, and we find ourselves in the presence of those tribes of various races formerly known as Gauls. There can be no doubt that the most populous districts of modern France were also the centres of civilisation of the Celtic, Iberian, and Ligurian ancestors of the THE PREHISTORIC AGE OF FRANCE. 15 modern French, although no traces of them have been discovered there. Their towns have vanished, ruins have succeeded ruins, until all remains of the ancient occupiers of the land have been reduced to dust. If we would find traces of them we must penetrate into the woods, and into those remote parts of the country where the population has at all times been thinly sown. The heaths of Britany and the plateaux of Poitou still abound in dolmens and menhirs ; in the woods of Franche-Comte grave-hills are met with in thousands ; on the granitic soil of Central France we may still trace the pits which formed the underground story of the Gallic houses ; whilst the pine woods of the Laudes abound in vast trenches {dotes), which mayhap sheltered the population of a village until it was driven forth b}' invading Celts or Basques. But these dwellings, remote as thev were from the centres of civilisation, can hardly convey an idea of the con- Fig. 8. — Dol-er-Veechaxt, oa Merchants' Table, at LocMABiAKEKr dition of the population of ancient France, any more than an idea of our present century could be obtained from the half-obliterated ruins of oui" out-of-the-way hamlets. Ever since the tertiary age the surface of France has been changing slowly through geological agencies, and without catastrophes. We may assume, there- fore, that the population of modern France has in its veins some of the blood of these ancient tribes. The invading conquerors of France have become amalga- mated with the tribes whom they found living there, and thus arose a race resembling a trunk with thousands of roots, and known as the French " nation." We cannot otherwise explain the astonishing variety of types met with in the difierent provinces of France. As M. Andr^ Sanson savs, " We are the intel- lectual sons of the Aryans, but not their carnal sons." c 2 10 FEANCE. The most ancient human remains hitherto discovered in France date back to the quaternary epoch, for miocene man, who wrought the tools discovered at Thenay, has left no trace. To judge from the skulls discovered under the lava of Denise, near the Puy-en-Velay, in Auvergne, the men of that period were long-skulled, but towards the close of the age of the mammoth and the bear, short skulls are first met with. Archaeologists are agreed that the men who dwelt in the caverns of the Pyrenees, on the Vezere and the Aveyron, were kinsmen of the Laps, Samoj'cds, and Eskimos. Their mode of life, their weapons and imple- ments, and even their style of ornamentation, all appear to support that conclusion. An invasion of barbarians destroyed the civilisation then attained, but gave birth in the end to a new era of civilisation much superior in many respects. The IxiiABiTAXTS OF France.* The Iberians are the most ancient inhabitants of Gaul known to history. They were kinsmen of those of Spain, who traded with Pha-nicians and Greeks, and whom the latter looked upon as aborigines. These Iberians occupied the country between the Atlantic Ocean and the Garonne, as well as the valleys of the eastern Pyrenees. In the west they were associated with the Ligurians of the Mediter- ranean, and elsewhere they came into contact with Celtic or Kymric tribes. Though Latinised, they have in a large extent their race characteristics ; they have even retained their ancient appellation of Gascons and Basques, and near the Pyrenees they retain their old language. Basques, Bearnais, and Gascons can easily be distinguished from other Frenchmen ; they are full of natural grace, supple of limb and mind, gay when at work, brave, though boastful, talkative, and imaginative to the extent of sometimes allowing themselves to be carried beyond the bounds of truth. The Celts, a race quite distinct from the Iberians, occupied the country to the north of the Garonne. Most modern Frenchmen look upon these as their veri- table ancestors, though very little is known about them. Ancient authors can hardly assist us in elucidating this point, for they wrote about the regions beyond the Alps much as our ancestors wrote about Central Africa. Modern historians, led away by false patriotism or by a rage for classification, have still further obscured this question, which is only in recent times being cleared up by the discovery of arms, weapons, dwellings, and human remains hidden for ages beneath the soil. Williams, Edwards, and Broca have shown satisfactorily, from a comparison of skulls and bones thus discovered, that ancient Gaul was inhabited by two distinct types of man, in addition to Iberians. The first type is met with between the Garonne and the Seine. These Gauls, or Celts, as they were formerly called, were small of stature, of a brown complexion, and short- skulled, whilst the tribes in the north-east, whether we call them Belgse or Kymri, were tall, fair, and long-skulled. • A. Hovelaeque, "La Linguistique ;" Fustel de Coulanges, "Histoire des Institutions politiquee de I'Ancienne France;" Lagneau, "Bull, de la Soc. d'Anthropologie," Feb. 1868, Nov. 1874; "Re^oie d'Anthropologie," tome ii. 1873 ; Saint-Eene Taillandier, " Revue des Beux-Mondes," Dec. 1875. THE INHABITANTS OF FRANCE. 17 Ancient authors onlj' describe these latter, probably because they were the most warlike. The men described bj' Ammianus Marcellinus, like the Gauls repre- sented by Roman and Greek sculptors, rather resemble Scandinavians, and they were certainly not the direct ancestors of the present inhabitants of Central France. Subjected tribes of a diflFerent tj'pe may possibly have lived amongst these Gauls of ancient authors, and been numerically superior to them. At present the physical type of the populations of Southern Eurojie prevails almost throughout France. We can hardlj- assume that a slight change in the climate, brought about by time and cultivation, should have exercised an influence sufficient to account for this southern type. Taken as a body, the French are in reality a brown-complexioned people, with heads round rather than oval, with eyes varying between black and Fig. 9. — Presumld Dispersion of the Aryan ILices according to Ancient Authors. pale brown ; with a stature and muscular development rather below the average, but of strong constitutions and capable of resisting fatigue and privations. Of these ancient Gauls there now exist only geographical names and a few short inscriptions. To judge from these their language appears to have differed very much from the dialects spoken in Great Britain, and to have had more affinity with Latin. Still the Aryan nature of the language does not prove that the people who spoke it were of Asiatic origin. Omalius d'Halloy altogether denies that an exodus of Gauls took place from Western Asia, and the map of Aryan migrations prepared by Pictet, though of scientific value, cannot prove it. All we know is that the Gauls dwelt for some time in the valley of the Danube. There can be no doubt that we must trace the existing character of the popula- 18 FRANCE. tion of France back to the tribes who inhabited the country anterior to the historic epoch. Still we must not lose sight of the influence exercised by immigrants of foreign races. The Phoenicians confined themselves to a few factories along the shore of the Mediterranean, and were succeeded hj the Greeks, whose colonies — Marseilles, Nice, Agde, and others — were of sufficient importance to enable them to exercise an appreciable influence upon the surrounding populations. Many Greek expressions have survived to our day, and the Marseillais have no doubt reason on their side when the}' boast of their Hellenic ancestors. The Romans, however, those merciless conquerors of the Gauls, exercised a far greater influence upon the formation of the French nation than did the Greeks. Italian colonists, many of them old soldiers, settled in the country, and this immi- gration, going on for six centuries, led to so considerable an infusion of Roman blood that several towns in the south could fairly be described as daughters of Rome, and the entire population as Gallo-Roman. These physical influences, however, were far surpassed by moral ones. It was the Romans who introduced the ideas and civilisation of the East, and more than all, they made Latin the tongue of the entire country. Language is the mould of thought, and must influence most powerfully the mind of a nation. The French, speaking a Latin tongue, must therefore bo ranged amongst the Latin races, in spite of their most diverse origin. Though belonging geographically to the Atlantic countries rather than to the Mediterranean ones, historically France forms a member of these latter, more especially since Algeria has become a French colony. Nevertheless, the barbarians, who after the fall of the Roman empire repeatedly invaded France, whether Franks from the Rhine, Northmen, or Huns from the plateaux of Asia, always came from the North. Scandinavian Visigoths established themselves in the south of France, and more especially in the Narbonnaise, and soon adapted themselves to their Gallo-Roman surroundings. The Germanic Burgundians, who occupied Eastern France, are described by their contemporaries as tall and strong, but at the same time good-natured. The Franks were far more harsh towards the tribes they conquered. In the end they gave a new name to transalpine France, and more particularly to that province of it which is known as He de France. M. Fustel de Coulanges does not think that those early German and Gothic invasions sensibly affected the character of the Gallo-Roman populations. The language and religion, social usages and political institutions, remained the same. But though the Germans never arrived iii bodies sufficiently large to change the character of the people, their immigration continued for centuries, and in the end their influence upon its phj-sique became very apparent. M. Broca, in his researches on the stature of Frenchmen, has shown this very clearly (see Fig. 10). The Normans, who settled in that portion of France now known as Normandy, likewise influenced the type of the inhabitants of Neustria. In the south of France " sea-kings " of quite a diflPerent kind put in an appearance. These were the Saracens, who maintained themselves for a considerable time on the coasts of THE INHABITANTS OF FRANCE. 19 Provence. In tke eighth century, when the Berbers invaded Europe in such overpowering numbers, these Saracens penetrated as far as the valley of the Loire, and perhaps even to Luxeuil and Jletz, and the inhabitants of Yerdun are said to have carried on a lucrative trade in slaves with them. Colonies of Saracens were established in many parts of France, and there can be no doubt that numbers of the Frenchmen now living in the basins of the Garonne and the Rhone are the remote descendants of Mussulmans. Fig. 10. — The Stature of Fhenchmen. By Broca. -r^ LU N°l - 26 N? 27. bZ N?iJ. 86 The departments are nvunbered according to the stature of their military conscripts. The small figures indicate the exemptions granted per thousand on account of small stature. Since those invasions of Normans and Moors, the ethnical character of the popu- lation of France has undergone no wholesale change, for the influence of English settlers in Guyenne, of German lansquenets and reitres who remained in the country at the close of the religious wars, and of the Spaniards in Flanders and Franche- Comte, has been quite of a local nature. On the other hand, the vast peaceable immigration which has been going on for some time past is certainly bringing about changes, and in the presence of the cosmopolitan population of some of the 20 FEA2JCB. large cities, a stranger may well be puzzled to tell whether it is a Frenchman he has before him or not. It almost appears as if a European type were gradually coming into existence. In the meantime the population of France has been welded into a nation, and in certain respects this nation exhibits greater unity than any other. This cohesion is due not so much to the existence of a centralized government, but rather to historical events, community of interests and of language, and to the existence of a capital which is universally acknowledged as the common national centre. Ancient rivalries between the provinces of France have not, however, alto- gether disappeared. The Bretons, Basques, and Flemish have even retained their distinct language, and the peasants of some of the more remote districts can hardly be said to have been assimilated with the rest of the population. Throughout France, however, these local diversities are of a very subordinate nature, the influence of the great towns is increasing from day to day, and the landmarks between the old pro'V'inces have almost disappeared. Of all the inhabitants of France, those lining respectively in the north and the south differ most strikingly. This difference is accounted for by the nature of the country, diversity of historical traditions, and the memories of struggles carried on in a past age. In a great portion of Southern France the Provenfal and other dialects are still the dominant tongue, and about twenty years ago French was hardly known by the bulk of the population. But as a literary language these southern dialects have no future, and those even who speak them often hold them in contempt. On looking at the map it wiU be found that the dialects of Southern France, including the "langue d'oc" properly so called, Proven9al, Dauphinois, Lyonnais, Auvergnat, Limousin, Gascon, and Bearnais, occupy very nearly one-half the area of the country. Nearly the whole basin of the Rhone, that of the Garonne, and the upper tributaries of the Loire belong to this half, and in the direction of Switzerland it extends even beyond the French frontier and comes into contact with German dialects. The wide range of these southern dialects proves the former preponderance of Southern France in the work of civilisation, but the " langue d'o'il " is at present steadily gaining ground. Language constitutes the strongest tie between man and man. We may fairly say that the French language, the origin of which dates back a thousand years, gave birth to the French nation. Common woes may have engendered a sort of fellow-feeling amongst the diverse populations of ancient Gaul ; they nearly all combined in the time of Vercingetorix against their Roman oppressors. But Gaul was merely a geographical expression then, and modern France only dates from the time of the epic poems of the Middle Age. In the course of centuries this language, as well as the men who speak it, has undergone many changes. T7e can hardly conceive such a thing as an average Frenchman. Those who maintain that the national character has under- gone no changes ever since the Gauls appeared upon the stage of history are THE INHABITANTS OF FRANCE. 21 decidedly in the wrong. There may still exist features which recall the Gauls of Caesar and Strabo, but can it be fairly said of modern French peasants what has been said of the Gauls, that " the}' are a people of war and uproar, running through the world with swords in their hands, less, it appears, from avidity than from a vague desire of seeing, knowing, and acting ? " If we would meet a typical Frenchman, we must search for him in a place offering every facility for his development. Such places are the large towns, and more especially Paris, to which original minds fly from the stifling atmo- sphere of small towns and villages. There the natives from every province come into contact and amalgamate : the babbling Gascons, ever in motion ; the men from the plateau, inured to hard work, and slow to make friends ; the people from the Loire, with their quick eyes, lucid intellect, and wcU-balanced tempera- ment ; the melancholic Breton, always living as in a dream, but full of tenacity in all concerns of real life ; the Norman, slow-speaking, circumspect, and prudent ; and the men from Lorraine, the Vosges, and Franche-Comte, who are quick- tempered and enterprising. All these Frenchmen mutually influence each other, and evolve what may be called the general character of the French people. It is no easy task to sit in judgment over a nation. Since the days of the illustrious Grimm, who denied " every truly moral sentiment " to Frenchmen, manv foreigners, from envy or ignorance, have painted them in odious colours. On the other hand, there have been writers who have sought to elevate France above all other nations. As to French writers, they have been charged either with being prejudiced in favour of the nation to which they belong, or with unfairly under-estimating its merits ; and, indeed, psychology is one of the most difficult subjects of discussion. Speaking broadly, the character of the French exhibits a combination of northern and southern qualities. The country itself is intermediate between the Mediterranean and the Atlantic, and its inhabitants form a link between the Roman civilisation of the South, and modern times. The most diverse tj'pes are met with amongst the French, but, as a whole, they present a new type, in which classical features are replaced by mobility of expression, one-sided energj' by varied aptitudes. As a rule Frenchmen, and more especially Frenchwomen, are most impressionable, and they are capable of fully reflecting the ideas conceived by other nations. It is thus that all the great movements of Europe have found a powerful echo in France, if they did not originate there. This explains too the universal character of the French revolutions. It was France which pro- claimed the "Rights of Man," and posterity no doubt will praise her for it; it is France which does not allow its progress to be stopped by matters of detail, but always seeks for principles. It is only natural that a nation holding the position of an intermediary of ideas should be eminently sociable. A feeling of iaborn goodwill attracts the Frenchman towards his fellow-men, a spirit of equity dictates his conduct ; he obliges by forethought and captivates by amiability. He is discreet in all things, pleasing in dress and manners, without outraging good taste, and excels in the 22 FRANCE. art of conversation. The Frenchwoman is in these respects even a better repre- sentative of the national character. She is not only an excellent mother and housewife, but possesses social qualities of the highest order. She delights by her conversation, and constitutes the chief attraction of French society. It seldom happens that foreigners do not enjoy themselves in France, but a French- man scarcely ever feels perfectly happy in a foreign land, and no one feels more cruelly than he the bitterness of exile. The sons of Gaul are distinguished not only by quickness of comprehension and superior reasoning powers, but they are remarkable amongst all civilised nations for their tact and taste. For a long time they were looked up to as the arbiters in literature, and in certain departments of art they still stand unrivalled. Several of the neighbouring nations are indebted to them for a development of their art industries, and Paris still remains the high school of good taste. France is a busy beehive, as is shown by the immense quantities of French produce exported to other countries. In spite of the excessive subdivision of the soil, the peasant landowners have converted France into one of the most productive countries of Europe. Activity such as this not only testifies to the strength of family ties, but also to the personal worth of the workers. Moreover, the revivals which have succeeded each national disaster prove that the nation is still full of vigour, and fully capable of taking its part in the great works of humanity. But if Frenchmen have their virtues, they also have their faults. Their sociability often degenerates into undue familiarity ; clever talkers on every possible subject, they run the risk of becoming superficial ; men of taste and refinement, they are apt to sacrifice vigour and originalitj' ; too observant of social propriety, they sometimes stifle the voice of their conscience ; members of society or of " parties," they have not always the courage to assert their manly independence. But in these respects how many true men do we meet with in any nation ? But, in spite of all, France has exercised a most powerful influence upon the civilised world. Numerically the influence of Frenchmen grows smaller in proportion as the area held by civili.sed nations extends ; but moral and intellec- tual influences are not measured by numbers. The national life of France is as intense as that of any of her sister nations, and her past experiences will enable her to play an important part in the political and social evolution now impending. But even if France were to disappear from the world's stage, there would still remain the influence of the French language and literature. The vigour, grace, precision, and suppleness of that language have made it one of the most perfect vehicles of human thought. It has been propagated far be}'ond the territorial limits of the nation, and millions speak it, not only in the Latin countries, but in all other parts of the world. LIBRARY OF THE UNIVERSITY of ILLINOIS, ll I I 'I l'lllllllll W H W w ?^ O CHAPTER II. THE PYREKEES, THE LAKDES, AXD THE BASIN OF THE GARONNE. The Pyrenees.* r^^ HE region of the Pyrenees constitutes a distinct and separate portion of France, whether ve look upon its geology or the history of its inhabitants. From the very first they differed from those inhabit- ing the remainder of Gaul, and even now the Catalans of Roussillon and the Basques resemble in language and manners their neigh- bours of the Iberian peninsula. But it is principal!}' because the Pyrenees form the northern edge of the Iberian plateau, ■which is geologically bounded by the lowland of the Garonne, that they form a region apart. The lowland referred to extends from sea to sea, and up to the tertiary epoch was occupied by a strait connecting the Mediterranean with the Atlantic Ocean. This ancient sea-bed has gradually been upheaved, and is traversed now bj- the Aude, the Garonne, and their numerous tributary rivers, joined more than two centuries ago by a navigable canal, affording communications between the two seas. This Canal dii JJidi may be said to form the southern limit of continental Europe, for the Pyrenees which rise bej'ond already belong to a world half African in its nature. The vast depression which separates the Pyrenees from the Cevennes is one of the great natural high-roads of France, which, however, is far less important than the great northern roads, which place Slarseilles and Bordeaux in communication with Paris. Still a region which can boast of towns like Bordeaux and Toulouse, which enjoys a mild climate, and possesses a fecund soil, must exercise considerable local influence. The Pyrenees and the Alberes, which bound this southern region of France, extend like a wall from sea to sea. As compared with the Alps, the geological • H. MagTian, " Jfateriaux pour unc Etude stratigraphique des Pyrenees ; " Companyo, " Ilistoire naturelle des Pj-renees-Orientales," 1861; De Chausenque, "Les Pj-renees," 1854; Kussell-Killough, "Grandcs Ascensions des Pj-renees;" "Bulletin de la Society Ramond," 1867, 1868, 1870, 1875; " Annuaire du Club Alpin fran<;ai8," 1876 ; Calvet, " Progrds rural dans lea P>'renee8 ; " P. Raymond, " Diet, des Basses Pyrenees." 24 FRANCE. structure of these mountains is of the simplest, and one might fancy that they had been suddenly ejected from a fissure in the earth's crust. Its mountain masses are not separated by low passes, as in the Alps, and there is no difficulty in tracing the direction of the main range, which runs almost in a straight line from Cape Creus to the lower mountains of the Basque countries. The geological features are equally simple. Granites, apparently not of erup- tive origin, occupy the centre of the chain, and form many of the summits of the main range. Schists and other ancient rocks connect these crystalline masses, whilst sedimentary strata succeed each other in regular order on both slopes, from triassic sandstones down to the alluvial soil deposited by the rivers. In spite of this general regularity, the chain of the Pyrenees presents a great amount of diversity if studied in detail. About its centre, where the head-waters of the Garonne take their rise, the main range consists of two parallel ridges joined together by a transversal chain. The northern ridge extends to the east, and forms the Mediterranean Pyrenees, whilst the southern stretches west towards the Fig. 11. — Profile of the Ptsenees. Horizontal Scale 1 : 4,000,000. Vertical Scale 1 : 400,000. — PYRE WEES — AiOBGC.- EI"CWBJKTiE .irvFTHCTEKS '- — .B^'PIHBffieS- Bay of Biscay, and constitutes the Atlantic Pyrenees. Of these two chains the eastern is the least elevated, and the granite there is nearly always exposed ; whilst the more elevated summits of the western Pyrenees consist of schists and lime- stones. This shows that denudation has been going on more actively in the former, and in a large measure accounts for the striking contrasts in the aspect of the two extremities of the chain, and for the great variety of landscape met with when travelling along their northern foot from the Mediterranean to the Atlantic* The Pyrenees rise steeply from the Mediterranean, which, at a distance of only twenty-five miles from Cape Creus, has a depth of over 500 fathoms. Close to that cape rises the group of San Pedro de Roda, resembling a detached outwork con- nected with the frontier range of Alberes by a rugged ridge. The frontier range named gradually increases in height from 660 to 5,000 feet, as we proceed from Cape Cerbere to the mountains of Prats de Mollo and Campredon, and is indebted • Length of PjTenee9 from Cape Creus to Cape Sainte-Anne, near Hendayc, 266 miles : average breadth, exclusive of Spanish foot-hills, 51 miles; area occupied, 13,563 sq. miles; average height, 3,940 feet (?) ; volume, 1,650 cubic miles. THE PYEENEES. 26 for its name to the whiteness of its barren rocks. It rises steeply on the French side, but slopes down gently towards the south. Many roads lead across it, and have been used from the most ancient times. Near Amelie-lcs-Baius a wall most erroneously ascribed to Hannibal is pointed out; at the Col de Pertus (951 feet) Pompey erected a trophy in commemoration of his victories, and Visigoths, Franks, and Moors crossed there after him. Numerous fortifications bear witness to the strategical importance of these passes of the Alberes. Collioure in France, and Fig. 12. — Mont CAXioon. Scale 1 : 240,000. rhdrd 5 Miles. Bosas in Spain, defend the road along the coast. Perpignan and Figueras defend the outlets of the defiles, and the French fort of Bellegarde secures the important gorge of Peitus. At the present time these passes across the eastern Pyrenees are no longer as important as they were when the Mediterranean was the centre of the civilised world, and must yield to the road in the west which joins Lisbon and Madrid to Paris.* • Altitudes in the AlWres :— Pic des Tennes, 3,618 feet : Col des Balistres, 853 feet ; Col de Banyuls. 1,182 feet; Col de Fertus, 951 feet; Coustouges, 2,724 feet; Col d'Aies, 4,920 feet. FRANCE. Mountains of considerable elevation attach the Alberes to the main range of the Pyrenees, which is hidden behind the bold mass of Mont Canigou (9,141 feet). With its spurs and foot-hills this majestic summit occujjies the entire area between the upper vaUeys of the Tech and the Tet. It is perfectly isolated on three sides, Fig. 13. — PvY DE Carlittk. Scale 1 : 240,000. \..fii<- =5 \yi r^'"- ^■■yfl - !hl,ie taji-rlVt/r '{ ' I if -'-^ -f .') Miles. and the summits which attach it to the main chain in the south are inferior to it in height. Its bold pyramid does not yield in grandeur to that of Mount Etna ; it is seen as far as Barceloua and Montpellier, and the astronomer Zach even claims to have seen its dark profile projected against the disc of the setting sun from Marseilles, a distance of 180 miles. Until recently it was held to be the THE PYRENEES. 27 highest summit of the Pyrenees. As a trigonometrical station it offers many advan- tages, and its slopes have proved a fertile tield of exploration to botanists. The Pyrenees, to which is attached the Cauigou, form one of the most barren and inaccessible mountain systems in the world. The passes leading across them are mere notches, cut to a depth of 600 to 900 feet at an elevation of about 8,200 Fig. 14. — The DEyiLES of tub Aide. Scale 1 : 140,000. . i MUes. feet, and the mountains near them are almost devoid of individual features. Even the Puigmal (9,542 feet) rises but little above the extended rampart formed by the mountains. A deep depression, excavated in the granitic rocks by mountain torrents, separates it from another mountain mass farther north. This is the Col de la Pcrche (5,322 feet), guarded on the French side by Montlouis (3,940 feet), and on that of Spain by Puigcerda (Puycerda, 4,074 feet), built on a knoll of 28 FRANCE. glacial origin ; and from it flow the rivers Tet and Segre, the latter a feeder of the Ebro. The sources of both these rivers lie on French soil, and the political boundary has been drawn in the most arbitrary manner. Some of the mountain valleys near the pass fairly deserve their cognomen of " paradise of botanists," for curious plants found nowhere else in the Pyrenees may be gathered there. The granitic mountains to the north of the fertile district of La Cerdagne, on the Upper Segre, rise from a huge quadrangular plateau which gives birth to the head streams of the Tet, Segre, Ariege, and Aude, and is separated in the west from Andorra by the much- frequented Pass of Puymaurens (6,293 feet). The highest of these summits is the Puy de Carlitte (9,561 feet). At its foot detached masses of rock are piled up in chaotic confusion, covered in places with moss, but for the most part still bare of vegetation. Lakes and lakelets are scattered over the plateau, and amongst these the Lanoux (black lake ?), 7,068 feet, is the largest, though by no means the most beautiful ; for its dark waters only reflect naked rocks and snows, whilst the lakes on the lower slopes are surrounded by verdant meadows and woods. Another lake, at the head of the Tet, emptied itself in the ninth century, and caused a fearful inundation. The mountaineers formerly looked upon the many lakelets scattered over the Carlitte as so many remains of the Flood, and Noah's ark they supposed to have stranded on the Puy de Priguo. The ground to the north and east of this granitic plateau descends gradually, sometimes forming terraces intersected by bold precipices. Some of these terraces are still covered with woods of beech-trees and firs, but elsewhere the forests have been destroyed, and the aspect of the mountains is forbidding. As in the French Alps, we meet with formidable defiles, or clits, excavated by mountain torrents to a depth of many hundred feet. The most famous of these is the defile of the Aude, which even impresses persons accustomed to mountains. If we descend from the Baths of Carcauieres into this abyss, we almost fancy we have penetrated into the very bowels of the earth.' Various passes lead across the spurs of Mont Carlitte. The Quillanne (5,644 feet), thus named after the town of Quillan, connects the valley of the Tet with that of the Aude. Another pass farther east is dedicated to Jau, or Jupiter (4,964 feet), but is hardly used now. Lower still is the Pass of St. Louis (2,254 feet), which joins the valley of the Aude to that of the Agly, and through which the road leads from Perpignan to Carcassonne. With it the Pyrenees terminate, for with the scarped Puy de Bugarach (4,038 feet), to the north of it, begins the region of the Corbieres, so remarkable on account of its geological formation, its coal beds, and bone caves, but deprived of verdure and running water, and difiicult to traverse in summer, when its bleached rocks reflect the rays of the sun. These hills long formed the boundary between France and Spain, and the fort of Salses, which defended the road leading along their eastern foot, as well as the ruins of many castles, recalls the struggle for the possession of this countrj', which only terminated in the seventeenth century. Mount Alaric (1,970 feet), to the north of them, and close to the Aude, bears witness to the still more ancient contests THE PYEENEES. 29 between Romans and Visigoths. It is one of the few remaining links of the transversal chain which formerly joined the Pyrenees to the Cevennes. The Pyrenees of Ariege, occupying the country of the ancient Sabartes, are far more regular in their structure than the eastern extremity of the range. From the Pass of Puymaurens (6,336 feet) to the gorge of the Garonne — a distance of 110 miles — the main chain extends without a break. Its summits, amongst which the Pique d'Estats (10,305 feet) and the Montcalm (10,102 feet) are the most elevated, occupy in nearly every instance the axis of this sierra. Mont YalHer (9,312 feet), which forms so striking an object when seen from Toulouse, is no exception to this rule. Huge blocks of weather-worn granite cover the Fig. 15. — The Isthmts between the CoasiiuEs axd the Cevexxes. Scale 1 : 1,100,000. if . 20 Miles. western slope of this mountain. From a distance these look like grazing sheep turned into stone by some sorcerer, as the legends have it. The lakes which formerly lent a charm to this portion of the Pyrenees have long ago been drained. Only a few swamps are now left, and near these M. Garrigou has discovered the remains of pile dwellings dating back to the age of polished stone implements. But even without their ancient lakes these Pyrenees, with their simple profile, terraces, and verdant slopes, are a noble sight. They are typical of the entire chain, and hence the name biren or piren, which in the valley of the Ariege was formerly applied to a sheep-walk in the mountains, transformed into Pyrenees, became general. VOL. lu n 30 FEANCE. Two lateral chains run parallel witli the Pyrenees of Ariege, the most elevated of ■which ramifies from Mont Carlitte, and to the north of the valley of the Upper Ariege attains a considerable height. Its culminating point, the Peak of Tabe, or of St. Barthelemy (7,704 feet), stands forth prominently. The momitaineers look upon it with dread, and on its summit may still be seen the traces of ancient excavations made by seekers after enchanted treasure. An inferior chain, farther north, cannot boast of summits covered with snow far into the summer, nor of the mountain pasture, lakelets, and limpid cascades of the Pyrenees. It is monotonous of aspect, of inconsiderable elevation, and in parts almost resembles the walls of a fortress. M. Leymerie, the geologist, has named it the Little Pyrenees. These parallel ranges belong for the most part to the cretaceous formation, and have been pierced by the rivers which descend from the snow-clad crest of the Pyrenees. The Ariege, having passed to the south of the range of St. Barthelemy, Fig. 16. — The Little Pykenees. Scale 1 : 200,000. "".>.5\V.of Tjri 0'\2i S Milei. the core of which consists of crystalline rocks, turns abruptly to the north, and enters the plain through the gorge of Tarascon. The Salat has excavated itself a passage through the granite of the gorge of Ribaouto, above St. Girons. The smaller rivers which rise on the northern slopes of the lateral chains likewise take their courses through gorges excavated in the tertiary soil, and one amongst them, the Arize, runs underground through the famous cavern of the Mas d'Azil (938 feet), scarcely a thousand yards in length, and passable on foot, except when the river is in flood. On leaving this tunnel the Arize propels a few water-mills, and lower down passes through the picturesque gorge of Sabarat. The upper basins of the Ariege and the Salat abound in caverns. The " galleries " of Lombrives and Niaux pierce an entire rrountain to the south of Tarascon. Equally curious is the cavern of Bedeillac, the traditional burial-place of Roland. These caverns have proved a rich field of exploration to anthropologists and geologists. Bones of animals now extinct, as well as traces of prehistoric OF THE UNIVERSITY ef ILLINOIS. |i||||||(!|i|(!lflllWKi:!l:It:ipf^^^^^^^^ "I hiiiiiii THE PYEENEES. 81 man, have been discovered in them. Until rceentlj' many of these galleries were used as places of refuge. That of Ornolac, near Ussat, gave shelter to several hundred Albigenses, but the soldiers of the Inquisition built a wall across its entrance, and they all perished, as did the Greeks in the cavern of Melidhoni. To the zoologist these caves of the chalk mountains of the Ariege are more especially interesting, on account of the insects without eyes which have been discovered within them. The Central Pyrenees. — The gorge of Pont-du-Roi, through which runs the Garonne, separates the Eastern or Mediterranean from the Western or Atlantic Fig. 17. — The Maladetta. Scale 1 : 160,000. O°lio E.ofGr, 3 Miles. P5'renees. Geologically this is the centre of the entire chain, which here consists of metamorphic rocks. The valley of Aran forms the marked feature of this central chain of the Pyrenees. Geographically this valley is part of the basin of the Garonne, but politically it belongs to Spain. To the west it is bounded by the giants of the entire range. From the hills around Bagneres-de-Luchon we are able to admire these mountains, with their forests, pastures, snow-fields, and glaciers. The latter resemble in every respect those of the Alps, but do not descend so far into the valleys. In the " amphitheatre," or Cirque d'Oo (9,850 feet), we even meet with floating icebergs similar to those of Spitzbergen or Greenland. Formerly the glacier of Oo was far more extensive than it is now, and its ancient moraine, 5,900 feet lower D 2 82 FRANCE. than the terminal face of the existing glacier, is 4,400 j'ards in length, on an average 1,640 yards wide, and 790 feet in height. The most elevated mountains of the Pyrenees rise within the Spanish frontier. The group of the Maladctta, or " cursed mountain," thus culled on account of its desolation, terminates in a serrated crest, the principal "needle " of which still bears its ancient Iberian name of Nethou (11,170 feet). This peak was first ascended in 184"2, but the region to the south of it was only revealed recently by an Englishman, Mr. Pucke, who discovered there tlie largest lake of the Pyrenees, that of Gregonio, and the delightful meadows of the Malibierne. Mont l"'ig. 18. — Mont Peudu. Scale 1 : 100,000. 2° ?^WofPaj 2 Miles. Posets (11,048 feet), on the west of the valley of the Esera, rivals its neighbour in height. It was first ascended in 1856. From its summit may be enjoyed what is probably the grandest panorama in the Pyrenees. Mont Perdu, the "lost mountain," the third great mountain mass of the Pyrenees, rises likewise on Spanish soil. It was first ascended by the illustrious Ramond in 1802, and since then its amphitheatres or cirques have become the liaunt of tourists. The limestone pyramid of Mont Perdu rises from an irregular plateau, cut up into terraces bounded by precipices, and dotted over by curiously shaped masses of rock. To the west the group is bounded by the famous " Breach of Roland" (9,197 feet), said to have been cleft by the paladin's sword (Fig. 19). THE PYRENEES. 83 Glaciers occupj' the area enclosed between the rocky precipices. That between ilont Perdu and the crest of Estaube, to the north of it, covers an area of 1 -5 square miles, and within it is enclosed a lake, frozen almost throughout the year. The waters descending from the plateau have excavated immense cavities, locally called oiih'i^, or "porridge pots," but more generally known as cirques. The largest of these amphitheatres is that of Troumouse, but the most admirable, the glory of the Pyrenees, is that of Gavarnie (Fig. 20), bounded on the one £iJe by a perpendicular precipice 5,500 feet in height, on the other by rocky Fig. 19. — The Breach of Roland. terraces. A magnificent waterfall, 1,384 feet in height, plunges down from the glaciers when the snow melts, but in winter this and the numerous minor cascades are converted into pillars of ice, which surround the amphitheatre like a colonnade of marble. The granitic peaks in this portion of the range are inferior in height to those formed of limestone. That of Xeouvielle (Pic d'Aubert), the most remarkable of the former, only attains 10,144 feet, whilst the limestone masses of Pic Long (10,479 feet), and Campbieil to the south of it, almost equal Mont Perdu in 84 FRANCE. elevation, and are joined in the east to the Pic d'Arbizon (9,286 feet) and other summits looking down upon the valley of the Aure, which rival the Pic du Midi of Bigorre (9,437 feet) in beauty. This latter is separated from the main range by a low saddle, over which runs the road of the Tourmalet, and being thus isolated, the prospect from its summit is one of the most magnificent, extending from the Pic du ^lidi of Pan (9,463 feet) to the pyramid- shaped Mont Vallier. Fig. 20. — The Amphitiieatue of G.WARNra. Neouvielle and the mountains in its vicinity are covered with boulders ; and the moraines of ancient glaciers bound the " lakelets " which fill depressions in the valleys. These glaciers have shrunk now to small proportions, but during the glacial epoch they covered a vast extent of country. The most important of them occupied what is now the valley of the Gave of Pau, as far down as Lourdes. Anciently it appears to have extended beyond Tarbes, but even if we credit it only with the dimensions given to it by MM. Martins and THE PYEENEES. 86 Collomb, it had a length of 33 miles, and spread over 500 square miles. It covered the site of the modern village of Gavarnie to a height of 4,430 feet, was 2,590 feet thick in the basin of Argeles, and 1,180 feet above the site of Lourdes. In comparison with this gigantic river of ice, the seriieilhes of Mont Perdu and the ilabore, the glaciers descending from the dark flanks of the Vignemale (10,795 feet), the most elevated summit of the French Pyrenees, and the patches of ice to the east of formidable Bala'itous (10,421 feet), are of little note, for the whole of the existing glaciers of the Pyrenees hardly cover 20 square miles, and in no instance do they descend beneath 7,200 feet above the sea-level. To the west of the Balai'tous the height of the Pyrenees decreases rapidly, and the Pic du Midi of Pau is the last of the great granitic peaks. With the pyramid-shaped Pic d'Anie (8,213 feet) begins the country of the Basques, who formerly believed that mountain to be inhabited bj' an evil spirit. Beyond Mont Orhy (G,618 feet) we only meet with hills traversed by numerous passes, amongst which the " Gate " of Roncevaux (3,600 feet) is the most famous. At the saddle Fig. 21. — Section of the Ancient Glacier of ArgelSs. Scale 1 : 50,000. According to MM. Martins and Collomb. ■ 1 Mile. of Aldudes the political boundary turns abruptly to the north, leaving to France onlv low spurs and outlyiBg hiUs. One of these latter is the Rhune (2,950 feet), or " angular rock," affording a magnificent prospect over the Bay of Biscay. Although the difference of latitude between the two extremities of the Pyrenees does not exceed 1°, they differ strikingly in climate and aspect. Near the Atlantic the mountains are almost wholly covered with mould, and, where trees are not met with, the soil is at all events thickly covered with shrubs and furze. Towards the Mediterranean, on the other hand, the rocks are barren. In the Western Pyrenees we might fancy ourselves in Scotland, whilst the aspres of Roussillon and the secanos of Catalonia resemble the arid hills of Greece. The granitic rocks which prevail in the east partly account for these contrasts, but the principal cause must be looked for in the rains. In the Basque country it rains abundantly, near the Mediterranean hardly at all, the boundary between the two districts being formed by Mont Carlitte. The snow-line descends rapidly as we proceed to the westward, and in the Mediterranean Pyrenees we meet 86 FRANCE. neither with glaciers nor with perennial snows. The snow that falls there soon disappears before the rays of the sun, the winds, and a hot south wind resembling thefoehn of Switzerland, and locally known as aittan. Fig. 22. — The Ancient Glacier of Argel{:s. Scale t : 400,000. According to C. Martins, and Ed. Collomli K^iK/JeBe ' /■■ '-^if^'^- '3!fe?f*r-o,-,^rf %^^*fe,IS^^: o^ 0°io Wnrr.T . 5 Miles. The contrast between the two slopes of the mountains is even more striking than that between their extremities. On the French slope we meet with snow, THE PYRENEES. 87 ice, running streams, luxuriant meadows and forests, with numerous villages scattered over the plain ; on the opposite slope the eye alights upon naked rocks, poor pasturage, and heaps of stone serving as human habitations. To the mountaineers the French slope is known as bach or hatch — that is, "lower" or " shady " side ; the Spanish slope as soulaue, or "sunny side." On the latter the sun is more powerful and the rainfalls are less ; but man, by destroying the forests, has made himself an accomplice of a hostile nature. "Wild beasts are more numerous there. The chamois (isard) abounds there; wolves are plentiful, as likewise on the French slope ; and sometimes one hears of the mischief done by a bear. In the district of Capsir, in Eoussillon, the Ijtix, the genet, and the marten are still seen, but several animals, including the stag, which were common in the Middle Ages, have disappeared. A few wild goats still inhabit the valleys of Ordesa and ilalibierne, in Spain, but in France the last animal of the kind was killed in 1825. The geographical nomenclature of the French Pyrenees is Basque and Latin, but not Celtic, and we may conclude from this that the whole of the country was formerly inhabited by men of Euskarian race. The ancient language is still spoken, not in the less accessible portions of the Pyrenees, but in the open valleys of the west, where we meet likewise with gipsies, cagots, and cascarots living in separate communities. There are three dialects, xi?.. those of Labourd, of Lower Navarre, and of Soule. The Basque does not appear to have lost ground since the beginning of the Middle Ages ; but what the uncouth dialect of Beam failed to accomplish, French will no doubt succeed in, and no sooner will the Basques have learnt to speak two languages than they will neglect that one which proves least serviceable to them, f p to the present it was ignorance which protected Basque against the inroads of French, for one-half of the men and two-thirds of the women of the country are illiterate. Thousands of Basques migrate to the neighbouring towns of Bayonne, Bordeaux, and Toulouse in search of employment, or seek a home in the New World, where their number is probably greater than that of those who remain behind in the old country. Hostility to the conscription is one of the great motives of emigration, for the Basque, though fond of adventure, is averse to military service, and more than half the young men called out annually fail to put in an appearance. The Pyrenees to the east of the Pic d'Anie are inhabited by Frenchmen and Spaniards. The crest of the mountains does not, however, constitute the ethnological boundary, for in numerous instances the Spaniards have encroached upon the northern slope. Various circumstances account for this. The luxuriant pastures on the northern slopes naturally attracted the Spanish herdsmen inhabit- ing a sterile plateau, whilst the French agriculturists preferred remaining down in the plains. The political boundary, for the most part, conforms to these ethno- logical eccentricities, and the valleys of the Bidassoa, Carlos, and Aran have been assigned to Spain, though situated upon the northern slope. Nevertheless the Pyrenees constitute one of the most perfect political boundaries in the world. 38 FEANCE. Between the two railways which skirt the extremities of the chain, the one connecting Bayonne with Madrid, the other Perpignan with Barcelona, the moun- tains, for a space of 280 miles, are crossed only by two roads practicable for carriages. One of these runs over the Col de la Perche, to the east of Mont Carlitte ; the other through the Somport (" summit gate "), to the west of the Pic du Midi of Pau. All other passes are practicable only during a part of the year, and that for mules alone. The distribution of centres of population in the region of the Pyrenees is singularly regular. In the upper valleys, from the Alberes to the Rhune, we only meet with small villages, military stations, or watering-places like Bagneres- de-Luchon. Along a line connecting the outlets of these valleys have been Fig. 23. — The Basques on the French Slope of the Pyrenees. According to Broca. built the secondary towns of these regions, such as Oloron, Lourdes, Bagneres- de-Bigorre, Montrejeau, St. Girons, Tarascon, Prades, and Ceret, where the mountaineers procure their necessaries. Another twelve miles farther to the north, and along a line running parallel with the former and with the crest of the Pyrenees, we reach the more considerable towns, such as Bayonne, Pau, Tarbes, St. Gaudens, Foix, and Perpignan, all of them situated either in the plain or on low spurs readily accessible. No mining industry has caused towns to spring up in the very centre of the mountains, for mineral waters, forests, and pastures constitute the sole wealth of the Pyrenees. Breeding of mules and horses is carried on successfully in the Cerdagne and elsewhere, and the cattle of some of the eastern valleys enjoy a certain reputation, but as a rule the resources of the country are allowed to lie neglected, and an acre of meadow THE LANDES. 89 land in the Pyrenees does not yield one-tenth, nay, one-twentieth, of what it is made to yield in the Swiss Alps. The low hills and plains to the north of the Pj-renecs are covered with debris and boulders transported thither by the ancient glaciers. Xliesc boulders diminish in size in proportion as we travel away from the mountains. At Pamiers, Tarbes, and Pau they are still as large as a child's head, but farther north we only meet with small pebbles and gravel, and finally enter a region covered with clay and sand, which heavy rains convert into mud. The quagmires of Lauraguais, between the Hers and the Aude, and of Armagnac, between the Garonne and the Upper Adour, have hardly their equal in France. The Landes. The vast plain of the Landes stretches westward of these deposits of glacial drift. Bounded by the ocean, the Adour, the cultivated heights of Lot-et-Garonne, and the vineyards of Bordeaux, this plain covers an area of 5,400 squai-e miles. It is evidently an ancient sea-bottom covered with sands of pliocene age, sometimes to a depth of 260 feet. At a short distance beneath the surface we meet with a layer of compacted sand, formed by infiltration, and sometimes as hard as iron, which is occasionally associated with it. This alios, as it is called, prevents the growth of trees, and being impermeable, after rains the whole of the plain would be converted into a swamp if cvasfes, or drains, had not been dug to carry off the water. There are several "sinks" (enfoniioirs), the most remarkable being that of Hucaou, on the water-shed between the Leyre and the Garonne. Formerly, before the Landes had been drained, the Landescots, or Lanusquets, could only traverse these solitudes on stilts, instruments supposed to have been introduced from England. Mounted on his stilts, the shepherd was able to cross swamps with impunity, and to look after his flock, a long wand serving him simul- taneously as a balancing-rod, a weapon, and an organ of prehension. This mode of locomotion is confined now to the more remote districts. In the beginning of this century the value of land in this region was ridicu- lously small, and for a few francs a shepherd might purchase all around him as far as his voice could be heard. At the present time, however, the Landes have kept their original aspect only in a few places. Shrubs, ferns, and golden-flowered broom are rapidly being replaced by fields and forests of Bordeaux pines. These trees are admirably adapted to the Landes, and have been cultivated there from the most ancient times, trunks of them having been found beneath thick layers of turf. In llaransin — that is, the southern portion of the Landes — the cork-oak is the favourite tree, and near Bordeaux we meet with woods equal to any park of Western Europe as to variety of foliage. These forests graduallj- prepare the soil for agriculture, but the shepherds, whose pastures they encroach upon, hold them in aversion. The dunes skirting the shore of the Atlantic formerly threatened to overwhelm 40 FEANCE. the whole of this region, for towards the close of last century they advanced to the east at a rate of 60 or 80 feet a year. This danger was created by man himself, who destroyed the forests which had sijontaneously taken root upon these hills of sand. The prevailing westerly winds then again drove the sand inland, and it encroached upon Landes and swamps, and even overwhelmed entire villages. The village of Lege twice retired before this invasion of sand, viz. 4,300 yards in 1480, and 3,300 yards in 1660. Mimizan retreated likewise, and when Fm. 2i. — View in the Landes. measures were at length taken to stop the invasion of the dunes, these latter had again approached within a few yards of its houses. The first experiment to stop the advance of the dunes was made in the beginning of the eighteenth century. It succeeded, but it was only after M. Br^- montier had overcome the resistance of the inhabitants, whom he desired to enrich, that any serious progress was made. Seven hundred and twenty acres were planted between 1787 and 1793, and since then the whole of the region of the dunes, extending from the Gironde to the Adour, and covering 222,400 acres, has been converted into a pine forest. These plantations have exercised a happy THE L.1NDES. 41 influence upon the climate, if it were only by facilitating regulation of the sheets of water in the rear of the dunes. Swamp fevers (medoquines), which formerly Fie. 25. — The Di xf.s and Laxues in the Pays de Rorx. Scale 1 : 400,000. 1" 30~1V of Paris & Miles. decimated the population, have disappeared, and the general health has improved in consequence of the increased wealth of the country. The ponds or lagoons which extend in rear of the dunes must be looked upon 42 FEANCE. as ancient bays of the sea, from which they became separated by a bar of sand. The salt water which they originally contained escaped through drains, and they became filled with fresh water. The largest of these lakes, that of Cazau, covers 15,000 acres, and its surface lies at an elevation of between 62 and 66 feet above the sea-level, according to the season. By means of a canal running parallel with the coast the level of this as well as of the other lakes might be lowered, and a safe water-way obtained connecting the Garonne with the Adour. The basin of Arcachon, about half-way between the Adour and the Gironde, is the only lagoon which still communicates freely with the ocean, but the time is not far distant when it too wiU be disconnected by a bar of sand. This ever-shifting Fig. 26. — The Basim of Arcachon. Sciile 1 : 325,000. Sand X nuL^ whicJi^ vji^vtr DcfdJv OVfr- Ji t'ect (hjstcr Bed* ■ 5 Miles. bar, as well as the violent tides, is the great obstacle to the conversion of this bay into a harbour of refuge, so much needed on the perilous coast of the Bay of Biscay. The rivers draining the Kttoral lakes of the Landes are turned to the south on entering the sea, for the coast current runs in that direction, and throws up a tongue of sand rmming parallel with the coast from north to south. The course of the river being thus virtually increased to the extent of several miles, its current grows sluggish, it performs its work of drainage less efficiently, the level of the lakes grows higher, and they encroach upon their banks. The eiforts of engineers to remove the obstruction to the unimpeded discharge of the rivers have THE LANDES. 48 not generally proved successful. The drainage of lakes and swamps has been attempted, though not on the same scale as in the Netherlands. The most important instance is that of the Lake of Orx, near Bayonne, which was emptied in 1864. Man and nature thus combine to modifj' the physical aspect of the coast of the Landes, but the submerged portion of the coast has been subjected to changes on a much vaster scale. A sand-bank marked on charts of the last century as being situated 15 miles to the west of the basin of Arcachon has completely disappeared. Floating ashes and seaquakes noticed by mariners point to the Bay of Biscay as a seat of submarine eruptions. Thus much is certain, that the sea has been encroaching extensively upon the land, and if we extend the slope of the Landes, as shown in Fig. 27, it will be found that the ancient coast-line must ha^-e lain 12 miles farther to the west than the existing one. In the time of Bremontier the sea gnawed away nearly 7 feet of the beach of Fig. 27. — The Slope op the Landes. The figures express the height or depth in metres (10 m. = 32-8 feet). Hourtin annually, and elsewhere its invasion was even more considerable, though there were not wanting localities where the land actually gained upon the sea. On first looking at the dunes facing the sea, it might be imagined that it is the land which is advancing. The waves and the winds are supposed to throw annually nearly 8,000,000 cubic yards of sand upon the beach of the Landes ; but this sand is derived neither from the hiUs to the south of the Bay of Biscay, nor from the coast of Saintonge, to the north. It is furnished by the Landes themselves, and by the submarine plateau upon which they rise, and in its minera- logical composition is identical with the pliocene formation occupying the interior of the country. Further proofs pointing to an encroachment of the sea are furnished by the remains of the ancient vegetation of the country and the traces of man which have been discovered on the narrow ledge bounding the eastern foot of the dunes. Nowhere are these traces more conspicuous than on the beaches of La Grave and Matoc, to the south of the basin of Arcachon, for we meet there with layers of alios, with turf-pits, and the trunks of trees still bearing the marks of axes, with bricks and broken pottery. 44 FBANCE. But not only is the coast being gnawed by the sea, it is also slowly subsiding, for traces of human residence have been discovered below high-water mark. The coast to the north of the Fig. 28.— The Ancient Coast of the Landes. Scale : 1,500,000. }" jWofTarir" WWofCr ^— ^— ^— 20 Miles. The figures express the height above the sea in metres (10 m. = 32-8 feet). Gironde participates in this movement of subsidence, and not only sandy beaches have disappeared there, but also rocks. One of the best examples of this kind is furnished by the rock upon which stands the hne light- house of Cordouan, which illuminates the entrance to the Gironde. When Louis de Foix erected that build- ing at the close of the six- teenth century, the rock upon which it now stands was an island sufficiently large to admit of dwellings for the workmen employed. It is now completely covered at high water, and the dis- tance between it and the peninsula of La Grave has increased from 3-1 miles in 1630 to 4-3 miles. Nu- merous villages named m old chronicles have been swallowed up by the sea or overwhelmed by the dunes marching before it. Soulac was an important town on the Gironde, below Bor- deaux, whilst the English held the country, but the Gothic church and the few walls which alone remain of it now stand upon the shore of the ocean, the dunes hav- ing passed right over them (see Fig. 35) . The Gironde itself would probably by this time have changed its bed had not the engineers prevented it by the construction of costly embankments. Nowhere else on the THE ADOUE. 45 coast of i'rance does man struggle so arduously against the assaults of the ocean, and sometimes the issue is doubtful. Between 1818 and 1846 the Pointe de Grave, at the mouth of the Giroude, receded 236 feet towards the south-east, but the coast now is eihciontly protected by embankments. The Adour. The geological history of the Lower Adour is connected with Ihat of the Laudcs, but the two Gaves, with their principal tributaries and head-streams, belong to the region of the Pyrenees. The xVdour rises between the Pic d'Arbizon and the Pic du Midi of Bigorre, about 12 miles to the north of tlie crest of the Pyrenees. Though fed by abundant rains and melting snow, the drought of summer would cause it to shrink into a riviJet insufficient even for purjDoses of irrigation if it were not for the Blue Lake {Lac Bleu), a natural reservoir, the outflow from which is regulated by means of a submarine tunnel, and from which 71 cubic feet of water are dis- charged every second, a quantity sufficient for irrigating the valley and supplying the manufactories of Bagneres and Tarbes. This is a work of our contemporaneous engineers, but the canal of irrigation, ■which leaves the river where it issues from the mountains to rejoin it 25 miles lower down, dates back to the time of Alaric, the Visigoth. The island lying between this canal and the river forms one huge garden, in which maize grows to a height of 15 feet. On approaching the region of the Landes the river sweeps round to the west, skirting the hills of Beam, the cultivated slopes of which contrast strikingly with the desolate plain on its right bank. At Dax, instead of flowing directly to the sea, the Adour turns towards the mountains, and, as far as its confluence with the Gave, winds between hills. The volume of the Gave is superior to that of the Upper Adour, but its current being rapid and its slope steep, the tide only ascends for a short distance, and is of very little service for purposes of navigation. The name Adour is therefore with justice applied to the lower part of the river. The Gave of Pau, in its ujjper valley, alternately forms cascades, flows tranquilly along the bottom of deep ravines, or spreads out over emerald meadows contrasting strikingly with rugged defiles. At Lourdes it leaves the mountains, but, instead of flowing north over the plain, it abruptly turns to the west, and pierces the hills of Beam, all covered with erratic blocks carried thither by the ancient glaciers from the high mountains in the south. Below the graceful bridge of Betharram it winds across a plain, but at Pau it again flows amongst hills, from which it finally emerges only 12 miles above its confluence with the Gave of Ossau. Throughout the whole of its course it retains the character of a torrent, and is useless for purposes of navigation. The debris piled up by glacial action at the mouths of the Pyrenean valleys have forced the Gaves repeatedly to change their course. The Gave of Pau VOL. II. K 46 FEANCE. originally flowed in the direction of Tarbes ; it then passed by way of Pontacq, and this outlet having been blocked up by the debris deposited there, the river opened itself a new passage through the defile of St. Pe. The bed of the Gave of Ossau has undergone similar changes. At first it joined that of Pau near the town of Nay ; subsequently it flowed north through the valley of Neez, and even now a portion of its waters finds its way to that valley through an underground channel 5 miles in length. Fig. 29.— Successive Changes of the Bed of the Gave of Pad. Scale 1 : 320,000. » " [ io' of Piri: U",i)\l9 L.otU 5 Miles. The estuary of the Adour, below Bayonne, has undergone similar changes. In the fourteenth century its mouth was 12 miles farther north, where the Boudigau now enters the sea, and the geological boundary between the regions of the Pyrenees and the Landes must still be sought for at that spot. There are no Clio's to the north of the Adour, but the nummxditic limestones of Biarritz extend north, beneath the waves of the ocean, as far as a spot lying off the " Fosse " of THE ADOUR. 47 Capbreton, anciently an important seaport, whicli gave its name to the island of Cape Breton, in Xorth America. The first change in the course of the river took place towards the close of the fourteenth century, when a violent storm threw up a formidable bar, the river Fig. 30. — The Mouth of the Asour. Scile I : SSO.OOO. Sililis. flowing along the rear of the dunes as far as the hamlet of Vieux-Boucau, or " old mouth," 22 miles to the north of Bayonne. The present channel of the river was excavated by human hands, aided by a great flood which occurred in 1571, and swept away the last remaining obstacles. £2 48 FEANCE. The ever-shifting bar at the mouth of the Adour is justly dreaded by mariners, and, in spite of the jetties which have been constructed, the narrow entrance to the river is occasionally obstructed. The Garonne. The Garonne rises on Spanish soil, on the southern slope of the Pyrenees. Its head-stream, fed by the snow and ice of Pic Nethou, is swallowed up by a sink known as Trou du Taureau ("bull's hole"), and after a subterranean course of 2 5 miles, reappears again as a gushing spring at the Goueil de Joueou ("God's eye"). At the hill of Castellcon this head-stream of the Garonne is joined by a second river of that name, which traverses the Spanish valley of Aran, and when it enters French territorj', at the marble defile of St. Beat, it is already a formidable river. The glacier-fed Pique of Luchon is the first considerable river which joins the Fig. 31. — Tub Subtebraneam Coukse ov the Uakonne. 1:1500000 o f a 3 4 SKilometrcft Garonne on the soil of France. Lower down it receives the Neste, which flows through the delightful valley of Aure, and its direct northern course being stopped by the masses of debris deposited by ancient glacial action, it turns abruptly to the east, and flows in a huge curve around that wonderful accumulation of shingle and gravel traversed by the radiating courses of the Gers, the Bayse, and numerous other rivers, all having their sources close to each other, as shown in Fig. 32. These rivers are gradually washing away the sediment deposited by glaciers, and nowhere else are we better able to study the influence which the earth's rotation exercises upon the formation of valleys. Almost without exception the western slopes of the valleys are gentle, whilst the rivers gnaw away the foot of the hills on the east, and a traveller who crosses over from one valley to the other in a westerly direction ascends by a gentle slope, but descends by a steep one. Very diflerent from these divergent rivers are the eastern or exterior tributaries of the Garonne, for their sources are far apart, they flow generally parallel with the equator, and, draining vaster areas, are more voluminous. One of them, the Salat, is thus named on account of the brine springs near its banks. Another, the THE GAEONNE. 49 Ariege, is not named thus because it carries gold {Atirigera), for its name is synonymous with Arega, Aregia, Ereya, and Arize, all of which simply mean river. Though draining a basin inferior to that of the Loire, the Garonne neverthe- less is a more voluminous river, thanks to the greater rainfall, the geological nature of the soil, and the snows of the Pyrenees, which feed many of its tributaries during summer. There are no torrent beds, as on the southern slope of the Cevennes, and the hills of Auvergne and the Pyrenees are amongst the best watered of all France. Floods, unfortunately, occur frequently, generally in May or June, when the snow melts and rain falls abundantly. At an epoch anterior to history the flow of the river was regulated by lakes. Fig. 32. — Radiating River Courses of Gers. Scale 1 : 1,876,000. 1' W. of Pans C v^ ^ /\^; one of the most important of which occupied the fertile plain of Riviere. But these lakes have been silted up and drained, and the floods occur now very suddenly. One of the most disastrous happened in 1875, when the river rose 40 feet above its ordinary summer level, sweeping away bridges, destroying nearly 7,000 houses, and doing damage to the extent of £3,400,000. These floods might perhaps be prevented if forests were planted upon the hills, but to this the pastoral inhabitants of the Pyrenees have a deep-rooted objection. The waters of the Garonne are not employed for purposes of irrigation, as they might be, and there exist no canals comparable with that of Alaric, in the valley of the Adour. M. Duponchel, however, has conceived the grand project of construct- 50 FEANCB. ino- a system of canals or drains, by means of which the hills of Gers might be levelled, and a portion of the fertile soil of which they consist spread over the barren Landes of Gascony* A navigable canal, communicating ^^■ith the Canal du Midi, follows the course of the Garonne from Toulouse downwards as far as the head of the tide, whence Fig. 33. — Valleys of Gehs. Scale 1 : 1,160,000. •i° IWof l^ru 0° ?0'E oi 1.1 the river is navigable throughout the year. Eelow Bordeaux, its great coiumercial port, the Garonne rapidly increases in width, and the triangular peninsula which lies between it and its twin river, the Dordogne, is known as Entre-Deux-Mers, with reference to the sealike expanse of these great tidal rivers. Sea-going vessels ascend the Dordogne as far as Libourne, at the mouth of the Isle. The bore Fig. 34. — The Plain of RivituE. Scale 1 : 320,000. which rushes up that river is said to have become more intense since the Garonne has been confined within narrower limits. The united waters of the Garonne and the Dordogne form a vast estuary, known as Gironde, varying in width between two and six miles, and dotted • " Creation d'un sol fertile a la surface des landes de Gascogne." Montpellier, 1864. THE GAEONNE. 51 over with numerous islands. There are many mud-banks, which interfere with navigation, but the depth of the channel is nevertheless very considerable, and at the mouth of the river, between Royan and the Pointe de Grave, it is no less than Fig. 35. — The Esti-aky of the Gironde. Scale 1 : G40,0iXI. 10 Miles. Erhard 105 feet. This estuary is in reality an arm of the sea, and at Mechers, 6 miles above its mouth, there are salt ponds and oyster beds. Cetacea and sea-fish ascend the river with each tide, and porpoises gambol around the vessels as in the open sea. Among these visitors from the Atlantic the maigre (Scin'm aquih), a singing 52 FEANCE. fish, is one of the most curious, and the crews of many a vessel have been frightened by the sound it emits. The banks of the Gironde exhibit many traces of geological action still going on. The hills on the right bank terminate in cliffs, the foot of which is continually Fig. 36. — The "Passes" of the Gironde. Scale 1 : 350,000. 3" I 20' W of Paris [~ ^a •■Vn,\ f \A '^' 5;'% T fui:rgf^ ^, ■^$^m r^/n. 1" |\V. ol' Cf. ^-id Dep.h 0-16 feet. 16-32 feet. over 32 feet. 5 Miles. being gnawed by the waves, and several villages have disappeared there, including Gerioset, which occupied the summit of a hill to the east of Royan, and Talmont, which stood at the extreme point of a peninsula. Swampy plains of recent origin, such as the "polders" of Little Flanders, Fig. 37. — Section of the Passes of the Gironde. 20 f' drained in the seventeenth century, and the old salt marshes of the Verdun, extend far into the peninsula of Medoc. The culminating point of the whole of this region, the hill of Jau or Jupiter, scarcely rises to a height of 40 feet, and a couple of centuries ago was an island. Ancient river beds can still be traced, and LISRARY OF THE UNIVERSiTV of ILLINOIS. TYEENEES OEIENTALES. 53 •what is now the Pointe de Grave was lorincrly an island near the northern bank of the river. The submarine relief is likewise undergoing continual changes, which endanger navigation. The channel, or "pass," of the jrasfclier, which was the principal one about the middle of the eighteenth century, is now occupied by a formidable sand-bank known as La Mauvaise. The contours of the banks and the direction of the currents are for ever changing, and in the course of less than a century the bank of La Mauvaise has shifted o miles to the west, whilst that of La Cuivre moves in an opposite direction. Still, thanks to lighthouses, buoys, and beacons, vessels can at all times enter the Gironde with safety, and even at low water the depth of the northern pass is nowhere less than 40 feet. At each tide no less than 265,000 Ions of water penetrate into the estuary of the Gironde, a quantity in comparison with which the discharge of the Garonne and Dordogne combined is almost inappreciable, even during floods. TOPOORAPHY. Pyrenees Oriektales. — This department is almost a portion of Catalonia as far as its climate, its productions, and the language of its inhabitants are concerned, but has formed part of France since the middle of the seventeenth century. It includes the valleys of the Tech, the Reart, the Tet, and the Agly, all of which debouch upon the plain of Roussillon. Each of these valleys is well watered, but, upon the whole, naked rocks form the predominant feature of the department, which is therefore able only to support a small population. The valley of the Tech or Yallespir — that is, " austere valley " — is the southern- most of continental France. Its scenery is delightful, and the customs of its Catalan inhabitants full of interest. At its head are the pastures of Costabona, and on descending it we pass the sulphur springs of Preste, the old town of Prafs-de-Mo/lo (1,320 inhabitants), formerly famous for its cloths ; Aries (1,871 inhabitants), the commercial centre of the valley, where rude cutlery is manu- factured ; Ceret (3,063 inhabitants) ; and the hot sulphur springs of Amelie-les- Bains. Across the naked range of the Alberes, defended by the fort of Bellegarde, the great Spanish high-road leads through the Pertus. This road is far easier than the one leading along the coast of the Mediterranean, through CoUiourp (3,446 inhabit- ants), frequented by fishermen, and Port-Vriidrcs (1,910 inhabitants), which boasts of an excellent harbour, much frequented by vessels in distress. Some wine is exported from here, including the sort known as " rancio," which only attains maturity after having been kept for ten years, and possesses tonic properties almost equal to those of quinine. The district of Aspres, which extends east of the Canigou in the direction of the Mediterranean, is sterile, as its name implies, but excellent wine grows upon its hills, and the lowlands, irrigated by the Reart, are of wonderful fertility. F/iir (2,463 inhatitants), the ancient Illiberri, subsequently named Helena in honour of 54 FEANCE. the mother of Const antine, is the only town of importance there ; its cathedral dates back to the eleventh century. The most important valley of the Eastern Pyrenees is that of the Tet ; the Col de la Perche at its head, and the roads to Perpignan, are defended bj' the fortress of Montlouis, constructed by Vaubau. Lying at an elevation of 5,250 feet above the sea, the climate of this place is most rigorous. Hot mineral springs abound in this portion of the Pyrenees, but only those of Vernef, on the northern slope of Mont Canigou, enjoy a world-wide reputation. Iron ores, suited to the Fig. 38. — Port-Vendres. Scale 1 : 15,000. laSIauAsqilt is r^v- \% --BaAiIj, Kdutarfe •>- Ui-iUniit a„ , •1 I'Jiare Beal^ ''■ manufacture of steel, likewise abound. There are iron works at Pia, between the small fortified town of Villeneuve de Conflant and Prades, but most of the ore is exported to Germany. Prades (3,725 inhabitants), Vinga (2,093 inhabitants), IHe (3,222 inhabitants), and all the villages of the Riveral, to the very gates of Perpignan, are indebted to the fertilising waters of the T^t for their prosperity. Ferjngnan (24,379 inhabitants) is a fortress of the highest importance, for it commands all the passes over the Pyrenees from the sea to the Pass of La Perche. ARIEGE. 65 Traces of Moorish architecture may be discovered in its huge citadel, in the Castillet, or little castle, and the "Loge," or old exchange of the Majorcans, but it is not in other respects a fine city. Its ancient industries have declined since Charles V. converted the town into a fortress, and its university, founded in the fourteenth century, only exists in name. The climate, however, is deliglifful, sub-tropical plants grow most vigorously, and the whole country might easily be converted into a huge garden of acclimatization. Wine is the great source of wealth of the country. Though ordinary roussillou is used merely for blending the lighter wiucs of Central France, tirst-rate wines are produced at Rivesaltes (6,077 inhabitants), on the Agly ; at Estagel (2,678 inhabitants), higher up on the same river, and the birthplace of Arago ; and at Salses, the Salsulfc of the Romans, ilost of these wines are exported through Barcares, a port near the town of St. Laurent de In Salanque (3,990 inhabitants). The country likewise produces olives. The tract along the coast, known as " Salobres," is impregnated with salt, and hardly produces anything, but fair harvests of cereals are gathered in the tract known as " Salanque," which bounds it inland, the vine and olive being restricted to the hilly districts. Akiege.* — This department includes the old district of Couserans, the basin of Salat, and the county of Foix, comprising the basin of the Ariege. Nearlj' the whole of it is mountainous, and the main range of the Pyrenees forms the boundary towards Spain for a distance of 136 miles. The only plain is that of Paumiers. The popidation is thin and exceedingly ignorant. The small canton of Querigut or Donnezan, on the Upper Aude, which is only accessible to the rest of the department by the difficult Pass of Paillers, sheltered the fugitive Protestants after the revocation of the Edict of Nantes, but is now ^•isited only on account of its sulphur springs at Carcanieres. The upper valley of the Ariege likewise attracts strangers on account of its hot springs, amongst which those of Ajt (Aqua?^ are the most famous. Hematite iron ores, lead, copper, and manganese abound at Vic de Sos, in a side valley of the Ariege, but owing to the difficulties of access, the want of fuel, and the restrictions imposed by mediaeval guilds, the metallurgical industry is not very important.t At Tarascon there are gypsum quarries, and travelling still 10 miles lower down the valley, we arrive at Foix (5,127 inhabitants), with its famous old castle, the capital of the department. Below that town the Ariege passes through a series of gorges, and then enters upon a vast alluvial plain, where stands Pamiers (7,837 inhabitants), the most im- portant town of the department. Lower down still is Sarerdun ('2,596 inhabitants). The vaUey of the Hers joins that of the Ariege beyond the limits of the department. It is one of the most charming of the Pyrenees, the pine woods of Belesta, the intermittent spring of Fontestorbes, and the ruined castle of Monts^gur constituting some of its principal attractions, whilst Lavehinct (2,792 inhabitants) and Mirepoix (3,102 inhabitants) are noted for their manufacture of cloth. On • Berg^s, "Description du dip. do I'Aricgo ; " Bordes-Pagds, " Notice sur le Couserans;" Aetnic, "Mem. pour I'hiet. naturelle du Lang^iedoc." t In 1873, 6,040 tons of cast iron, 5,045 tons of wrought iron, and 889 tons of steel were produced. 56 FRANCE. the Arize, which flows direct to the Garonne, stands the busy little place of Mas d'Azil (1,278 inhabitants), near which the river flows through a subterranean channel. The western portion of the department, ancient Couserans, is drained by the Salat and its tributaries. The upper valleys of this region formerly constituted as many self-governing communities, and the inhabitants, until quite recently, Fig. 39. — BAGNiRES-DE-LuCKON. Scile 1 : 215,000. r UOWof Pan 2 Miles. retained their ancient dress and customs. In winter they leave their inhospitable mountain homes in search of work in the more favoured plains ; and when bears were still numerous in the Pyrenees, many of them travelled as bear-leaders. Hot springs abound in these valleys, the most renowned being those of Aulus, accidentally rediscovered in 182'3, and deservedly popular on account of the delights of the surrounding scenery. St. Girons (3,993 inhabitants), the capital V5 o a o p a a a a < O HAUTE-GAEONNE. 57 of the district, occupies a site at the confluence of the Lcz with the Sulut. It carries on a lucrative commerce with Spain, tho road leading through the Port do Saluu, and boasts of various manufactures. At St. Lizicr, which was tho ancient capital, may still be seen the ruins of Roman walls and of a Gothic cuthotlral. The old episcopal palace has been very appropriately converted into an asylum for lunatics. Haute-Gakoxxe. — This department includes portions of the ancient provinces Fig. 40. — The Cosveboest Vaij,ey8 of tub Gaiionne, tue Aui£o£, anu the litiis. Scale 1 : 600,000. i" ^.. E ,.rCi I**' \V..trl\iri.H 10 Miles. of Ghucony and Languedoc, and is intersected from south to north, for a distance of 150 miles, by the river Garonne, which has given it a name. It extends from the crest of the Pyrenees to the foot-hills of the central plateau of France, and thus exhibits a great variety in its scenery, climate, and natural productions. In the very heart of the mountains lies the most famous hot spring of tho Pyrenees, that ui Bagnkrea-de-Luchoit (3,982 inhabitants), the surrounding scenery 58 FRANCE. of which — its glaciers, woods, and mountain gorges — forms its great attraction to all admirers of nature. -) O En or Tht UNIVERSITY of ILLINOIS. 1L\UTE-GAE0NNE. Fis inhabitants), and other places in the north, are mainly dependent upon agricul- ture ; whilst Vilkmur (2,3G7 inhabitants), on the Tarn, and Itiiel (3,782 inha- bitants), have some manufactures. Toulouse (120,208 inhabitants), the entrepot of the fertile plain of the Garonne, is one of those cities which cannot be dispensed with. Its favourable position for war and commerce at all times insured its prosperity, and when the Romans captured it they discovered in a sacred pond treasure valued at 15,000 talents, or £3,000,000. This prosperity is perhaps greater now than ever it was before ; but though Toulouse has been the capital of the Visigoths for nearly a century (418 — 007), it carries on no direct commercial transac- tions with the Iberian peninsula, but is the great intermediary be- tween the Mediterranean and the Atlantic. Including the subiu-bs. ■12. — The Canal of the Xeste. Scale 1 : 320.01X). ;• Wofrara the red-brick buildings of the town cover an area of over 3 square miles. The town-hall or Capitol, with its busts of illus- trious Languedocians, occupies the centre of the ancient city, which was superior to the towTis of Northern France in wealth and intelligence, until the henchmen of the Inquisition caused its street* to flow with blood, and in- stilled a spirit of ferocious ortho- doxy into the minds of its inha- bitants, who burnt Yanini at the stake in 1619, and in 1762 broke the limbs of Calas, the Protestant, upon the wheel. The church of St. Servan, the cathedral of St. Ltienne, and the ancient monas- tery of St. Augustine, now converted into a museum, are amongst the most interesting buildings of the town. The library, far inferior to what one might expect to find in an ancient university city, occupies another old monastery. Commerce and industry flourish. There are manufactures of paper, starch, tobacco, and textile fabrics, as well as foundries and saw-mills. The environs are almost bare of trees, and there exists no park deserving the name. II.vvtes-Pyrenees. — This department includes the whole of ancient Bigorre, 60 FRANCE. with portions of adjoining districts. More than half of it is filled with high mountains. Its principal rivers are the Neste in the east, the Adoiu- in the centre, and the Gave in the west. The alluvial hottom-lands are of exceeding fertility; hot springs abound in the mountains; there are famous marble quarries and busy manufactories ; but the j)opulation is still far from numerous. The valley of the Aure, or Upper Neste, is one of the most renowned of the Pyrenees, on account of its pretty scenery and grand perspectives. Arreau, its capital, is merely a village, and Sarracolin is only better known because it lies at Fig. 43. — BAGNkKES-DE-BlGORRE. Scale 1 : 380,000. '.;W of Pan J ^^r^w~w _ . ::. (f.^=^ N 5 Miles. tht head of the canal of the Neste, and boasts of marble quarries. The popula- tion, however, is more dense than might be expected, for hamlets and homesteads lie scattered in all directions. The valley of Campan, on the Upper Adour, is looked upon as typical of the beauties of nature ; but the men who inhabit it are repulsive, as most of them are subject to wens. At its mouth lies Bagneres-de-Biyorre (7,598 inhabitants), which has paper and saw mills, marble works, and manufactures of fancy hosiery, these latter giving employment to more than 2,000 women. The town is likewise the HAUTES-PYEENEES. (il seat of the Soci^te Ramond, which has undertaken the scientific exploration of the Pj'renees and established an observatory on the Pic du Midi of Bigorre. Turbes (11,080 iuhubitauts), the capital of the department, lies quite beyond the hills, and from the windows of its museum an unrivalled prospect over a Fig. 44. — The Timili or Ossux. AccortUng to Bourbier nud Letrone. Scale 1 : 62,000. 2'l 2«'\V »I ?aa o-tc \v MUe. verdant plain, bounded by blue mountains in the distance, may be enjoyed. There are foundries, woollen-mills, and manufactories of felt, as well as a Govern- ment factoiy of small arms and a cannon foundry. The surrounding country is famous for ita breed of saddle horses. Com and wine are the leading agricultural productions. VOL. II. V 62 FRANCE. The hilly country to the east of this smiling plain of the Adour, including the plateau of Lannemezan, consists to a great extent o-f heaths. The best-known village there is Capveni, with hot mineral springs. Heaths also occur to the west of the Adour, and one of them, near Ossun (2,400 inhabitants), is remarkable on account of its ancient entrenchments and tumuli. The basin of the Gave, in the west of this department, is perhaps more frequently visited by tourists than any other portion of the Pyrenees, and deservedly so, for it abounds in sublime scenery and natural curiosities. Its many thermal springs form one of its greatest attractions. The sulphurous waters of Bareges are efficacious in case of wounds, those of St. Sauceur are available against nervous disorders, but the various springs of Cautereta cure almost every disease that human flesh is heir to, and attract as many as 16,000 sufferers in a single year. The mouth of the valley of the Upper Gave is commanded by the old fortress of Lourdcs (4,577 inhabitants), become famous in our days through a miracle-working spring near which quite a town of churches and convents has sprung up. Basses-Pyrenkes. — This department includes Beam and the old " kingdom " of Navarre, with the districts of Soule and Lubourd in the Basque country. For the most part it is hilly rather than mountainous, though the Pyrenees to the south of the valleys of Ossau and Aspe still pierce the region of perennial snows. The ravined plateau to the north of the Gave of Pau consists of glacial drift. There are mines of iron, coal, and salt, many manufactories, and a great commercial port ; but upon the whole this 'is an agricultural department, the resources of which have not hitherto been developed as they might be. The touyas, or heaths, which cover 783,000 acres of the Pyrenean foot-hills, are quite capable of cultivation, but the peasants prefer to use them as pasture ground. It is only natural, under these circumstances, that the population should decrease. The Gave, on entering the department, flows past the church of Bethar- ram, an old place of pilgrimage, and then irrigates the fields of numerous villages, the centre of which is Nay (3,093 inhabitants), which boasts of numerous manufactures. Still following the river, we reach Pau (27,553 inhabitants), the ancient capital of Beam. It is built upon a terrace, and owing to the mildness of its climate has become a great resort of invalids. The terrace of its ancient castle commands a magnificent panorama of the Pyrenees. The entertainment of visitors is the great business of Pau, but there are also some manufactures of linen. Morlaas, the first capital of Beam, now an inconsiderable village, lies in the Landes, to the north-east ; and, proceeding still farther in the same direction, we reach the castle of Montaner, one of the strongest fortresses built by Gaston Phoebus. Orthez (4,727 inhabitants), on the Gave, below Pau, was formerly the seat of a universitj^ and is noted for its ancient bridge and the donjon of the old palace of the Dukes of Foix. There are numerous tanneries and other industrial esta- blishments, and amongst the exports of the town figure " Bayonne hams." The mountainous portion of the department belongs to the basin of the Gave OF THE UNIVERSITY of ILLINOIS. LIBRARY OF THE UNIVERSITV of ILLINOIS. I'll [Itl BvVSSES-rYREXEES. 03 of Oloron, the capital of which is 0/oron Ste. JUarie (7,223 inhabitants), ut the foot of the ouly I'yrenean pass available for wheeled traffic, viz. that of Somport. There are cloth and cotton factories, and smuggling is carried on extensively. High up in the hills, at the foot of the Pic du Midi of Pau, lie the sulphur sprin"8 o{ Hdiu-Jioiiius and E(uu-Cli(itu!es, and the vuUoy of Earctous, in the south-west, is famous for its cuttle. In descending the Gave we successively pass througli Navarreujr, an old fortress, and Sautftvrrc. At Oraas, near the latter, and at Sdlies (2,404 inha- bitants), there are salt works, now carried on by Government, but they arc far less productive than formerly. The villages in the interior of the Basque country arc remarkable only on Fig. 45. — Bavo.vnb axu the Moitu of the Adoir. Scale 1 : &l.l«.n>. JMl Wol'l'iir J,'. 7 account of their picturesque position. At MauUon-Licharre, the old capital of Scale, are the ruins of a castle ; Hasparren (1,573 inhabitants), a very ancient village, has shoe and cloth manufactures ; the fort of St. Jean-Picd-de-Port commands the Pass of Roncevaux and two others. Near it is a colony of cagots, a despised race formerly, but nevertheless intelligent, and superior in physique to their neighbours. Most writers now look upon them as descendants of the Visigoths. Bayonne (22,307 inhabitants), though slightly inferior to Pau in population, is by far its superior in commerce and industry. It is a fortress, but gaily painted houses, open squares, and fine promenades give it the appearance of an open city. Its Gothic cathedral is one of the finest edifices in the south of France. Its F 2 64 FRANCE. position at the bottom of the Bay of Biscay and on the most frequented road between France and Spain marks it out as a great place of commerce ; but owing to the bar which closes the mouth of the Adour, it has not attained a position amongst the great commercial ports of France such as might have been expected, and the numerous Spanish and Portuguese Jews are intent rather upon bourse speculation than upon legitimate commerce.* As to the other harbours along the coast of Gascony, such as Guethary and St. Jean-de-Luz, they are at present of no commercial importance whatever. And yet the mariners from this coast frequented America long before Columbus, though not before the Normans. Great efforts are now being made to improve the harbour of St. Jean-de-Luz Fig. 46. — KoADSTEAD OF St. Jean-de-Luz. Scale 1 : 200,000. 16 - 3i oxnj- I6A- F^UJuftns . (3,131 inhabitants), though that town can never again become a great place of commerce. Indeed, such importance as these coast towns possess is due entirely to their having become favourite seaside resorts ; it is this which has transformed the village of Biarritz (3,348 inhabitants) into a cosmopolitan water- ing-place, and is preparing a similar fate for Hendaye. Gers. — This department is named after a yellowish river which traverses it from north to south, and occupies the greater portion of the plateau of glacial drift piled up at the mouths of the Upper Adour and Neste, and cut up by torrents into numerous ridges of hills (see Fig. 32). It lies outside the usual • In 1872 there were 1,320 Jews. In 1875 1,460 vessels, of an aggregate burden of 164,324 tons, entered and cleared. TAEN-ET-GAEONNE. 65 roads of traffic, but its vallej's are fertile, and a fair wine grows upon its hill- sides. The most fertile portion of Gers lies on the south-west, and is watered by the Adour. Immediately to the east of this valley rises the plateau of Armagnac, the wines of which are to a great extent converted into brandy, ranking next to Cognac. Cazauhon (760 inhabitants), Eauzc (2,062 inhabitants), Montreal (690 inhabitants), and Vic-Fezemac (3,000 inhabitants), are some of the more important places in Lower or "Western Armagnac, separated from Upper Armagnac by the valley of the navigable Bayse or Baise, the more important towns of which arc Condom (4,933 inhabitants) ani.Mu-ande (3,230 inhabitants), the capital of Astarac. Audi (12,145 inhabitants),, the name of which recalls the ancient Ausques or Eskuaras who founded it, lies in the valley of the Gers. It is a fine town, with one of the most majestic cathedrals of France, an immense flight of stairs, leading to the terrace upon which it is buQt, and a mediajval tower dedicated to Caesar. Higher up in the valley lies the village of Saiixaii, which has become known through the paloDontological explorations of M. Lartet and others. The lower valley of the Gers is well cultivated, and the fields surrounding Fleurance (3,737 inhabitants) and Lcctoitre (2,963 inhabitants) are of great fertility. The patois spoken at the latter place is said to contain Greek words, and the rivulet formed by the fountain of Houndelie bears the Greek appellation of Hydrone. The towns in the extreme east of the department are in nowise remarkable, except for the ruins of mediaeval castles and abbeys. L'IsIe-Jounlain (2,248 inhabitants) and Lomhez, both on the Save, are the principal centres of population, and carry on some trade in cattle and geese. Tarn-et-Garoxxe. — This department, one of the smallest of France, includes the hills of Eastern Lomagne, the alluvial valleys of the Garonne, the Tarn, and the Aveyron, and a hill region in the north and east which forms part of Quercy and Rouergue. Some of the soil is exceedingly fertile, and there are manufacturing establishments at Montauban and elsewhere, but the population is nevertheless on the decrease. Beaumont (3,608 inhabitants), the capital of Lomagne, as well as all the places on the left bank of Garonne, is decreasing in population, and Cmtel-Sarmsin (3,547 inhabitants), on the opposite bank of the river, does so likewise, but never- theless carries on a considerable commerce in wine and the products of the fertile plain, too frequently devastated by the waters of the Garonne. Montauban (19,790 inhabitants) stands majestically upon a lofty bluff of the Tarn, spanned there by a fine old bridge. Its position is a favourable one for com- merce, but its greatness as a city passed away when it ceased to be one of the four towns of refuge granted to the Calvinists. It gloriously withstood the armies of Louis XIII. (1620), but twelve years later it yielded to Eichelieu, and its civil liberties and industries were annihilated. Linen and muslin, earthenware and leather, are manufactured, but a spirit of enterprise capable of striking out new paths is altogether wanting. The town-hall contains a fine library and a collec- tion of paintings, many of them by Ingres, a native of the place. 66 FRANCE. Moissac (5,675 inhabitants), iu the alluvial plain and neai' the confluence of Garonne and Tarn, is one of the great grain markets of France, and possesses a mediteval church and cloisters, which contrast strangely with a modern aqueduct and an iron railway bridge. Valence d'Agcn (2,926 inhabitants), lower down in the valley, is wealthy and industrious. An old house is still pointed out there in which sat the inquisitors who condemned forty-three heretics to the stake. Fig. 47. — The Alluvial Plain of the Gahoxne, the Tarn, and the Aveyron. Scale 1 : 320,000. 1°V. . 5 UUes. The plateau to the north of the Aveyron is but thinly populated, and the only town of any importance there is Caussade (2,438 inhabitants). The Aveyron, on entermg the department, passes through a series of picturesque gorges, bounded by limestone cliffs, the caverns in which have yielded numerous implements of palseo- lithic age. St. Antonin (2,520 inhabitants), the most considerable town in that LOT-ET-OAEONNE.— LANDES. 67 part of the country, boasts of a town-hall built in the twelfth century, and of nume- rous private dwellings dating back to the thirteenth. Lot-et-Gakonxk. — This department is named after the two rivers which effect their junction within its limits. The hills of Lomagne form a steei) escarpment towards the vale of the Garonne, and a considerable portion of the south-west consists of Landes, but the northern half is occupied by tertiary hills of great fertility. As a whole, the department is one of the most productive of all France ; its race of cattle is highly esteemed, and poverty is unknown. Agen (17,806 inhabitants), the capital, lies on the right bank of the Garonne, at the foot of a hill covered with gardens and "sillas. It is famous for its cattle markets and prunes, the latter grown in the vallej' of the Lot. Three bridges and an aqueduct cross the river. Descending the Garonne, we first reach Port Stc. Marie (1,699 inhabitants), near which the valley of the Baj'se joins from the south, and up which leads the road to Nerac (4,975 inhabitants), an old Roman town, with the ruins of a royal palace. Nerac has recovered from the injury inflicted through the revocation of the Edict of Nantes, and now carries on a considerable commerce in wine and brandy. Iligbcr up on the Bayse is IfoiicrabeaK (681 inhabitants), the Gascon " head-quarters of liars, babblers, and boasters." Mczin (1,989 inhabitants), which has exported wines to London since the fourteenth century, stands on the Gclise, a tributary of the Blayse ; and lower down, near the same river, rises the castle of Barbaste, nov converted into a factory. Farther to the north-west, beyond the forests recently planted in the Landes, lies Casteijaloux (2,074 inhabitants), with a mineral spring and some manufactures. AguHlon (1,993 inhabitants), near the junction of the Garonne and Lot, is but a small place. Ascending the latter river, we pass Clairac (2,388 inhabitants), known for its "rotten" wines, which are made from overripe grapes; Castelmoron (1,028 inhabitants), Sfe. Livrade (1,404 inhabitants), and Villcncucc-sur-Lot (9,681 inhabitants), a busy place, with an old abbej^, now used as a prison, the ruins of the castle of Pujols, and several mediaeval buildings, including a bridge. Penne (1,272 inhabitants). Fame/ (2,229 inhabitants), and Bonaijuil were known in former times for their citadels, that at the latter place having been one of the first con- structed to resist artillery. Returning to the valley of the Garonne, we pass Tonneins (5,803 inhabitants), entirely rebuilt since the Calvinistic wars, and Marmande (6,037 inhabitants), both of them driving a busy trade. Le Mas d'Agenais (1,245 inhabitants), and 3Icilhan (639 inhabitants), on the left bank of the Garonne, are mere villages. Nor are the few towns in the north of much importance, except, perhaps, Miramont (1,416 inhabitants), with its orchards of prune-trees. Landes. — This department does not include the whole of the Landes of Gas- cony, though, on the other hand, it comprises, in the south and south-east, some of the foot-hills of the Pyrenees and of Armagnac. The resources of the depart- ment are small ; there are no extensive tracts of fertile land, nor harbours along the coast, and the population is therefore very thinly sown. 68 FBANCE. Dax (9,085 inhabitants), on the Adour, is the natural centre of Chalosse, the most fertile district of the Landes. It is an old town, with remains of Roman walls and baths. The steam arising from its famous sulphur springs is seen from afar. Thermal springs abound throughout the region, as at Pouillon (250 inhabitants), La Gamarde, Tercis, and Prevhacq ; rock-salt abounds ; asphalt is found in the valley of the Luy ; and the iron in the western Landes is utilised in the forges of Castets (937 inhabitants). Peyrehorade (1,786 inhabitants), on the Gave, at the head of navigation, is likewise a busj' f)lace. Cap-Breton, in former ages one of the most famous seaports of France, has Fig. 48.— Cap-Breton (1872). Scale 1 : 33.614. />^UA /f^S 1 -tl U Miles. dwindled down into a poor village, but the harbour of refuge now constructing there may bring back some of its ancient prosperity. St. Sever (2,225 inhabitants) and Aire (2,906 inhabitants), both on the Adour, are quiet country tovms, though the latter is the seat of a bishop ; but Mont-de-Marsan (8,328 inhabitants), to the north of them, the capital of the department, is a busy com- mercial centre, from which are exported the brandies of ViUeneure (1,155 inhabitants) and Gabarret in Armagnac, the rosin of Roquefort in the Landes, and the wines and manufactured goods of Chalosse. Lahrit, the ancient capital of a duchy, is now merely a village, with the ruins of a castle built by Henri IV. 1.I8RARV OF THE UNIVERSlTVofttilNOjS. GIRONDE. GO Some of the stations along the railway which connects Bordeaux with Bayonno are rising into importance. Ic/ioux has iron works, Lahouheijre (La Bouverie) is famous on account of its cattle fairs, and Ifoiretix promises to become a place of commerce. The ancient towns of the littoral region of Born, however, which were joined formerly by a Roman road, have dwindled into insignificance. Mimizan, the most important amongst them, attracts a certain nimiber of seaside visitors during the season. GiRONUE. — The Landes occupy fidly one-half of this department, as fiir as the Garonne and the estuary of the Gironde, and even extend beyond that river, but the whole of the district known as Entre-Deux-Mcrs, as well as the hills of the Fronsadais and Perigord, is an outlying portion of the plateau of Central France. Bordeaux, so happily situated at the mouth of the Garonne, and on the great high-road which connects Paris with Spain, is the natural centre of the department, and would insure it a pre-eminent position, even though its agricultural produc- tions, its early vegetables, and wines had no existence. Bazas (2,859 inhabitants), the ancient Xovcm Populana, and the seat of a univer- sity at the time of Charlemagne, is an unimportant place now, but the tumuli, the dotes, or remains of Gallic habitations, and the castle of Roquetaillude near it, are fall of interest to the antiquarian. The arrondissement of Bazas lies completely within the region of the Landes, but its inhabitants have made considerable advance in agriculture, they breed a highh' esteemed race of cattle, and at Yillan- draut, in the valley of the Ciron, the)' grow excellent wines. The names of Preignac, Barsac, Bomme, and Sauterne are known throughout the world, and there are certain growths, such as Chateau- Yquem, which are appreciated by every connoisseur. The towns along the Garonne and the Gironde know no other trade or industry except what is connected with wine and agriculture. Castds, at the head of the tide, is a busy port ; Laiigoii (3,903 inhabitants) and the old city of i ,,rj'. y^vi ! Al\ , — • - "*/i*i.' . '* _.'-tA.' S' i» a » of . J Miles. with the granitic nucleus of the mountains of the Moors ; but the serrated chain of the Alpines or Alpilles (1,614 feet), which farther east rises above the stony pasture lands of La Crau, alreadj' belongs to the sj'stem of the Alps, being in realit}' only a prolongation of the chain of the Lcberon, from which it is separated by the valley of the Durance. A small volcano, now extinct, rises in the midst of these hills. The parallel ranges stretching towards the valley of the Var, in Eastern Provence, are also ramifications of the Alps. Some of these Jurassic ranges resemble the interior slope of a bastion ; others contrast by their barrenness with the smiling gardens of the Ilesperides at their feet, irrigated by the fertilising VOL. II. Q 78 FRANCE. waters of the Siagne. The highest summit of these ranges is Mont Cheiron (5,834 feet). The Maritime Alps. — The promontories which are reflected in the blue waters of Nice and Mentone, to the east of the Var, belong to the Maritime Alps. The bold terrace of the Tete-de-Chien, or " dog's head," at Monaco, with its steep precipices, bears a high tower dedicated to the Emperor Augustus, the "conqueror of all the nations of the Alj^s," and forms a good natural boundary between French and Italian Liguria. The political frontier between these two countries, however, as drawn in 1860, lies farther to the east, and follows an arbitrary direction. The Maritime Alps extend from the Pass of Tenda In the east to the Pass of Fig, 55. — The Vehdon at Quinson. Larche (6,480 feet) in the north. Their most elevated summits are covered with perennial snow. The torrents to which glaciers and numerous small lakes give birth on the Mediterranean slope, force their way through narrow defiles cut through lime and sandstones. Similar gorges, or clus, are met with in the lime- stone hills extending westward to the Durance, pne of the most remarkable being that of the river Verdon, above Quinson.* The Chtfian Alps. — Monte Viso (12,586 feet), which was looked upon for a long time as the highest summit of the Alps, and has only recently been ascended by Mr. Mathews, an Englishman, forms a connecting link between the Maritime Alps and the Alps of Dauphine. The geological features of these mountains differ widely from what we meet with in other parts of the Alps. * Highest summits in the Maritime Alps : — Clapier de Pagarin, 9,994 feet ; Mercantourn, 10,391 feet. GENKRAL ASPECTS.— MOUNTAINS. 79 Monte Viso itself consists of serpentine. Granite is met with on the Italian slopes, but schists and limestones predominate on those of France as far as the valley of the Durance. This district, with its gorges and piles of rock, lias not inappropriately been termed Qiicyras, or "land of stones." The roads which connect the valley of the Durance and Provence with the valley of the Po lead across these Alps of Qucyras and Monte Viso, collectively known as Cottian Alps. One of these paths crosses immediately to the north of Monte Tiso at an elevation of 9,821 feet. A tunnel, or iraccnctte, excavated as long ago as the fifteenth century, renders its passage practicable at all seasons, in spite of avalanches, mists, and storms. The Pass of Mont Geuevre (6,067 feet), Fig. 56. — The Gouge, oh " Clis," of the Yerdon. Scale I : ISO.OOO. i" K or I'd fc> ?\iajiini Is. ^_ now practicable for carriages, was first used by Hannibal and his army. These and other passes, however, are only of local importance now, and are frequented almost exclusively by Piemontese who cross over into France in search of work. During the iliddle Ages they were important, too, as military highways, and the mouths of the valleys leading up to them were guarded by fortresses, some of which are still maintained — as, for instance, Embrun (2,809 feet), Mont Dauphin, and Brian^on (4,333 feet), on the Durance. The inhabitants of these remote valleys might have maintained their independence if the country had not so frequently been overrun by armies. On both slopes of the Alps they speak the same dialect, and long before the Reformation they separated from the Roman G 2 80 FRANCE. Churcli. lu spite of massacres we there still meet with many Waldenses, or 7audois, St. Veran (6,592 feet), the most elevated village in all France, bein"- one of their principal seats. These Waldenses were formerly distin- guished for their superior education, and in winter as many as a thousand of them came down to the towns of the E,h6ue valley, and taught the mysteries of reading and writing in return for a miserable pittance. The establishment of village schools has put an end to this pursuit, and many of the natives have sought a new home in Algeria. The Alps of Dauphine. — Another Alpine group, that of Oisans, rises to the west of the valley of the Durance, which, with its southern ramification, the Fig. 57. — The Glaciers of Oisans. Scale 1 : 250,000. 5 Miles. Champsaur, lies wholly within France, and is bounded in the north by the deep valley of the Romanche and the Pass of Lautaret (6,792 feet), in the east and south by tributaries of the Durance, and in the west by the Drac. This mountain group consists of granite, encircled by Jui-assic and cretaceous rock. Mont Pelvoux (12,773 feet) is the most prominent summit of this group, but the Barre des :6crins (13,462 feet), and the Aiguille, or "needle " of Medje (13,078 feet), the latter immediately to the south of the valley of the Romanche, exceed it in height. Glaciers cover about one-third of the area of this mountain groujj, and fairly rival those of Switzerland. The most considerable amongst them, that of Mont de Lans (5,293 feet), covers an area of 8 square miles, and when making the tour of GENERAL ASPECTS.— MOUNT.VDfS. 81 the upper valley of Yeiieon, passing the glacier of La Grave and the Aiguille of Olun (12,740 feet), we walk for a distance of 35 miles over ice and snow fiolds. The most remarkable of these glaciers are, perhaps, those which descend from the slopes of Mont rdvoux and the Poiute des Arsiucs, and meet in the upper valley of the Vallouise. One of them, the " Black Glacier," is covered completely with rocks and earth so as to almost resemble a stream of mud, whilst the other, the " White Glacier," is of dazzling whiteness, and giscs birth to a torrent of bluish water. None of these glaciers reach very far down into the valleys, and we are Fig. 68. — Aioi'iitE op THE IfEnjB. not, consequently, charmed by the contrasts between verdant woods and ice, such as delight the ej-e in Switzerland. Indeed, there are but few trees left in these mountains, though there exist luxuriant pasture grounds, notably near the wealtliy village of Venose, the inhabitants of which export rare Alpine plants as far as Russia and America. A few Protestan'L congregations still remain, but the Waldenses, who formerly inhabited the fine valley of Vallouise, have been wholly exterminated. The present population of the country is wretchedly poor, and cretinism prevails. The famous 82 FEANCE. cliurcli of La Salette stands high above the valley of the Drac, in the midst of luxuriant pastures ; and near it, in the narrow valley of Godemar, there existed until recently traces of a more ancient worship. In spring, when the sim first appeared above the crest of the mountains opposite, the villagers of Andrieux used to walk there in procession, and sacrifice pancakes in honour of the conqueror of winter. Chaotic masses of mountains occupy the whole of the region bounded by the Fig-. .19. — The (tlacifr of La Grave. Durance and the Isere, and extend down into the valley of the Rhone. Going west from Mont Pelvoux, we reach the plateau of Matheysine (3,050 feet), covered with small lakes, pierced by crystalline mountains, and bounded by the precipices overhanging the waters of the Eomanche and the Drac. Crossing the latter, we reach the Quatre-Montagnes, or " four ranges," separated by affluents of the Isere, and running parallel with the Pennine Alps. In the north, beyond the Isere, the mountains of the Grande Chartreuse (6,847 feet) extend in the same direction, and OENEKAL ASPECTS.— MOUNTAINS. 83 in the south they are joiued to tlio mountains of Yercors (7,695 feet), uU three having the same geological formation. The latter are hardly Aljjine in their character, their great beauty consisting in the contrasts afforded between open valleys and sombre gorges through Avhich torrents escape in picturesque cascades, in the southern aspect of their sunny slopes, and the bold outline of some of their rocky declivities. The formidable Pass of Lus-la-Croix-IIaute (4,920 feet) separates the Vercors from a mountain group known as Di'voluy, a name which etyraologi.sts derive from the Latin decoliitnin, with reference to the immense masses of rock which have " tumbled down " into the valleys and gorges. The base of the great Peak of Aurouze (8,905 feet) is completely surrounded by mounds of detritus, which, seen from afar, have the appearance of white marble buttresses. Other mountains resemble huge piles of rocks. Of this kind arc the Obiou (!),1G0 feet) and Faraud, which a local legend " transforms into hostile giants \\ho hurled huge rocks at each other. This excessive weathering of the mountains is accounted for by their geological composition. As a rule, strata of hard rocks alteriuite with deposits of soft earth, and no sooner have rains, torrents, and frosts disintegrated or carried away the latter than the superimposed rocks slide down into the valleys, together with the villages which are built ujion them, or tumble into fragments. To a great extent, however, the improvidence of man is responsible for this rapid dis- integration of the mountains, for it was he who destroyed the forests which formerly covered and sheltered them. These forests, however, are gradually being replanted.* The mountain ranges which ramify to the south, towards the confluence of the Rhone and the Durance, resemble those just noticed in geological composition, and present the same white rocks and barren slopes. The forest of Saou (5,223 feet) has long since succumbed to t.he woodman's axe. Farther south rise the rampart- like mountains of Lure (5,095 feet), attached by a transversal chain to the rugged Leberon (^J.tiOU feet), the reddish flanks of which arc covered with patches of copse. Atmospheric influences acting upon rocks possessing such different degrees of resistance have resulted in some curiously grotesque formations. Thus to the north of Forcalquier may be seen a group of mushroom-shaped rocks known as Leis Jloiirrc, the tops of which consist of blocks of compact limestone supported upon stalks composed of clay marl. Farther west rises a mountain appropriately called Ventoux, or the " windy " (6,273 feet), which, owing to its isolated position, impresses the spectator more than its height would warrant. Its lower slopes are covered with a belt of verdure, and an ascent to its summit affords an opportunity for studying successive belts of vegetation. The paheontological discoveries made in this part of France shed much light upon ancient flora and fauna. The miocene strata of the Ventoux and Leberon abound with the remains of lions, gazelles, hipparions, and other animals now extinct. The miocene gypsum near Aix, on the other bank of the Durance, has yielded fish, insects, plants, and even feathers of fossil birds. • Between 1861 and 1871 234,760 nrres were plimtcJ wilh forest in the Froiidi Alps. 84 FEANCE. The fossil fisli discovered there prove conclusively that the Mediterranean formerly communicated with the Indian Ocean. Thanks to an agricultural discovery of great importance, the districts of the Yentoux and Leberon are now being rapidly planted with woods. Joseph Talon, a poor mushroom gatherer, discovered in the beginning of this century that this coveted fungus grew more luxuriantly in the vicinity of oaks. He quietly planted acorns in the retired sjoots to which he was in the habit of resortiag, and for many years he kept his secret. It is only since 1856 that this new industry has spread, and since that year no fewer than 1-18,000 acres have been planted with oak in the department of Vaucluse alone. This department and the adjoining one of the Basses-Alpes now supply nearly one-half the mushrooms gathered throughout Fig. 60. — Tiir. '■ Forest " oi- Saou. Scale 1 : 160.000. ■.'VEof Pans Cvp^t K' S.Vilftiui/ /'/-•,. ' '4^> . 2 Miles. '-1 France, and exported under the deceptive appellation of " truffles of Perigord." The indirect advantages which have accrued to the country through the introduc- tion of this industry are very great, for the flinty slopes and marls which are best suited to the growth of these mushroom oaks are not adapted to agriculture, and the newly jjlanted forests cannot fail to exercise a happy influence upon the climate, and put a stojD to the ravages caused by torrents.* T/ie Alps of Savoy. — The famous chain of Maurienne, across which lead the principal roads that connect France with Italy, separates Mont Pelvoux and the * In 1S75 32,000 cwts. of mushrooms were gathered throughout France, valued at £610,000. Vau- cluse yielded 8,000 cwts., the Basses- Aloes 7,000 cwts., and Lot 6,000 cwts. GENERAL ASPECTS.— MOUNTAINS. 85 \ipi3er valley of the Durance from Savoy. The Romans availed themselves of the easiest passes of that region, and on the summit of that of the Little St. Ber- nard may be seen a cromlech which thcj' dedicated to Jupiter, and which is still known as the column of Joux (Jove). At a subsequent date the Pass of Mont Cenis (6,885 feet) became the great highway between France and Italj^ ; but the fine carriage road which connects Lans-le-Bourg with Susa has been very little used since 1871, in which year the great railwa}' tunnel constructed by ilessrs. Grattone, Grandis, and Sommellier beneath the Pass of Frejus was thrown open for traffic. That tunnel connects Modane with Bardonneche ; it has a length of 40,092 feet, and its summit lies at an elevation of 4,-380 feet above the sea-level. The mountains of Mauricnne hold an intermediate position between the fine summits of Switzerland, with their forests and luxuriant pastures, and the arid Fig. 61. — Leis MourrS. slopes of the Devoluy and the .^Ups of Dauphine. In some of the valleys, and notably in that of the Arc, which constitutes the district of Maurienne proper, wc meet only with arid slopes. The ancient forests have been destroyed there, and the upper limit of vegetation seems to have retired in consequence. JIan will have to struggle hard if he desires to reconquer the ground that has been lost through his own improvidence. Though very inferior in height to ilont Blanc, and even to the group of Oisans, this chain of Maurienne, with its numerous raniiflcations, is of very great importance. Vast masses of ice have accumulated in its rock-surrounded amphi- theatres, and give rise to four considerable rivers, the Isere, the Oreo, the Stura, and the Arc. Formerly, when these mountains were yet unexplored, it was thought, on account of these snows, that Mont Iseran, in their centre, must attain 86 FEANCB. a very considerable heiglit ; but )no]if, in the patois of the country, simply means " pass," and that of Iseran lies at an elevation of only 8,034 feet. The Grande Casse (12,740 feet) and the Aiguille of Vanoise (12,675 feet) are culminating summits on French, and Mont Paradis (13,271 feet) on Italian soil. Valleys penetrate deeply into these mountains, and some of the more sheltered amongst them are permanently inhabited to a height of nearly 6,000 feet. The half-buried houses of Bonneval (5,900 feet), at the foot of Mont Iseran, are cut off Fig. 62. — Mont Blanc as seen trom Chamonix. from the rest of the world for several months in winter, and barley and rye take fourteen or fifteen months to ripen there. The want of pure air in these valleys, the long and severe winter, and the deep shadows thrown by the mountains during summer are popularly supposed to produce goitre and idiocj% which Dr. Grange ascribes to the magnesian limestone of the country. He estimates the number of persons suffering from goitre in Maurienne at 30 per cent, of the total population, and in certain localities of the Tarentaise the proportion is still higher. The long LISRAHY OF THE UNlVERSfTK of ILLINOIS, MONT r s I'r.H ... '.• ij'slliiili'hi* t.-s^ ' |4- />« '„/ ,/, 1,, /c./Vo/w $-.^i^: \i U■«ll.l^^tllfM^ '• f 4 t'Ju/otpf/ti f ■ *;, \i-i i'onlaiiiiiu' /•i ^^', ^ "i*^!^".'- ' -"^ l'U<-ier \. "• Hn b G°i,H.E.or«r. LONDON. J. S.' R le t;° GoKpi Knlre dou.isj Krili <.-^' l;i ('l\Uldr R»>s^.c< M.i:.l I ll-IlT I /; M \» Kit. tgff ■■'■V-.x •> v.iun.i l^ la Huuw U E & C LIMITED. GENERAL ASPECTS.— MOUNTAINS. 87 winters, however, enable these mountaineers to acquire some education ; and formerly many Savoyard teachers were to be found in tlie towns of the IthOne valley. The granitic ranges to the west of Muurionne run in a direction conformable to that of the Jura, and are intersected by the rugged gorges through which the Isere, the Romanche, and the Arc iind their way to the west. The group of the Grandes Eousses (11,910 feet) is the highest summit here. Farther west, above Grenoble, rises the thrcc-peakcd Belledone (0,778 feet), from the summit of which we look down upon the verdant valley of Graisivaudau and the limestone moun- tains which bound it on the west. From a geological point of view the mountain mass of which Mont IJlanc (15,777 feet) is the centre is but a norlliern continuation of these western ranges of Savoy. Its relief, however, marks it ofV verj' distinctly. Tlie enormous mass of talcose granite or protogine of which it is formed is separated by the Passes of the Little St. Bernard (0,897 feet) and Bonhomme (8,151 feet) from the other mountains of Savoy in the south ; sinks down steei^ly into the vallej^ of the Ehonc on the north ; presents steep, glacier-covered slojjes towards Italy ; and descends more gently towards the French valley of Chamonix. At an anterior period, when Mont Blanc was several thousand feet higher than it is now, it formed but a single mountain mass with the Aiguilles-Rougc?, now separated from it by the valley of Chamonix. The area occupied by Mont Blanc and its buttresses cannot compare with certain mountains of Switzerland, nor docs it give rise to any great rivers, for only the Arveiron, or Arve, and the Dora Baltea rise on it, the one flowing to the Khone, the other to the To. Its glaciers and snow-ticlds, however, are without a rival in Europe. They cover 104 square miles, of which 64 drain into the valley of Chamonix. The most famous of these glaciers is the Mer de Glace, or " sea of ice," which slides down the valley at a rate of 828 feet annually, and gives birth to the Arve. Discovered as it were by two Englishmen, Pococke and "Wyndham, about the middle of the eighteenth century, and ascended for the first time by Jacques iSalinat in 1780, Mont Blanc has since become one of the great attractions of all admirers of nature. Chamonix (3,444 feet), at its foot, has grown into a town of hotels; and other villages in its vicinity, sucli as St. Gervais and Cormayeur (4,007 feet), particijjate in the profits derived from tourists. The mountains in Northern Savoy, which occupy the region between Mont Blune, the Rhone, and the Lake of Geneva, form a sort of link between the Alps and the Jura, and from a geological point of view it is sometimes difficult to determine of which of either of these systems a certain mountain may be assumed to form a part. The cretaceous and Jurassic ranges generally run from the south-west to the north-east ; that is, parallel with the Jura. Such is the direction of the pine- clad ranges of the Grande Chartreuse (Chamechaude, 6,847 feet), of the parallel ridges of the Beauges (4,996 feet) to the north of Chambery, and of the ranges of Saleve (4,523 feet) and Voirons, near Geneva. 88 FRANCE. Most of the valleys of this region are of considerable width, and not mere eortres as in the Jura. There still exist, however, many defiles bounded by steep preci- pices, as if they had been cut by a sword, and amongst these none are more striking than those cut by the Rhone and its tributaries, Usses and Fier, through rocks belonging to the lower cretaceous formations. The transversal disposition of the mountain ranges of Western Savoy naturally Fig. 63. — Ancient L.\ke Beds in Savoy. Scile 1 : 200,000. i" 4o' E. oi' FarU. 6° UoE of Gr led to the formation of numerous lakes. But most of these pent-up sheets of water have long since disappeared, and there now exist only three of any extent, viz. the Lakes of Annecy, Bourget, and Aiguebelette. In the valleys of the Arve, the Giffre, and elsewhere, however, many old lake basins can still be traced. The agency of water likewise accounts for the numerous caverns which pierce the mountain sides of Savoy, as well as for frequent landslips. That of the Granier, ' l " >l ■ LIBRARY OF THE UNIVEfis;TY Bellegardk. i-6u' Eof Or. ;:cile 1 : lu.uuo. volume to the Rhone, the flow of which is regulated by the Lake of Geneva. When the snows melt in the Alps no less than 38,850 cubic feet of water are dis- charged into that lake in the course of a minute. But this water spreads over the • Surell, " Etude sur le« torrents des Hautes-AJpcs ; " Ch. Martins, " Aigues-Mortcs ; " E. Desjardins, '•Apcr<;a historique sur Ics embouchures du Rhone, 1866;" Adrien Germain, "Rapport 6ur I'etat de I'embouchure du lihSne en 18;2 ; " Ch. Lentheric, " liCs ^-illes mortes du golfe do Lyon." Hhdne (with Doubs) UilfB. Sadne- 1 „~- 63/ Area of Ba^in. Sq. m. 38,096 Discharec in Max. llToO Tons Uin. 5-39 Avemse Average minfliU. per 6ec. In. 16-86 37 Surface diuiuage. In. 22 Aude 138 2,062 29-43 4-9 61 29 15 Orb 90 591 24-53 2-4 25 (f) 35 20(?) H^rault 122 1,119 26-30 (?) 60 (?) 39 22(F) Argens C3 1,243 (?) 12-8 50 (?) 31 19(?) A'ar 75 880 39-23 27-4? 42(?) 3o 24(?) 90 FBANCE. whole surface of tlie lake, and issues only gradually tlirough the Rhone, the banks of which, as far down as Lyons, suffer in consequence but rarely from inundations. The Arve, on the other hand, possesses no such regulating reservoir, and frequently carries destruction along its valley. The Rhone, below its confluence with the Arve, crosses a district formerly covered by the Lake of Geneva, and then penetrates into a deep gorge, bounded by the eastern declivities of the Jura and by Mont du Vuache, or Chaumont, and Fig. 65. — The L/ike of Annecy. Height 1,453 feet, area 10 square mUes. Scale 1 : 230,000. defended by Fort I'lJ^cluse, which overhangs it. The river rushes through this gorge with great violence. At one spot it almost disappears beneath the rocks which have tumbled down from the precipices that overhang it. This is the " Perte du Rhone." A bridge there spans the abyss, and a short distance below it is joined by the Valserine, passing through a gorge almost equally grand. The great motive power of the river has been ingeniously utilised at that spot. A tunnel conveys the water upon tourbine water-wheels erected in the bed of the THE rh6ne and other rivers. fll Tnlserine, close to the confluence, and these wheels set in motion iron cables communicating with the mills of Bellegarde, built several hundred feet above. Thousands of tons of fossils are being ground there into dust, to be used as manure. At Bellegarde the Rhone abruptly turns to the south, flowing along the eastern foot of the mountain chain which terminates in the Grand Colombier (5,033 feet), overlooking the dried-up lake basin of Culoz. Within this portion of its course Fig. 66. — The Lake of Bocrget. Height 770 feet, area 16 square miles. Scale 1 : lUU.OOO. 1 Mile. it ia joined by two rivers, the Usses and the Fier. The former, having passed beneath the famous high-level bridge of La Caille, enters the Rhone near Seyssel, a place well known on account of its beds of asphalt. The Fier, ri.sing in the neighbourhood of Mont Blanc, receives from a side valley the water discharged by the Lake of Annecy. This lake consists of two distinct cavities or basins, and its depth nowhere exceeds 100 feet. In many places its banks slope down gently, a circumstance favourable to the construction of pile dwellings, the remains of 92 PEANCE. many of which have been discovered. Elsewhere, however, they are steep, and on the west the hike is commanded by the Semnoz (5,572 feet), or Rigi of Savoy. The existing emissary of this lake appears to be of artificial formation. The old outlet took its course farther east through a swampy plain. At Seyssel the Rhone becomes navigable, and soon afterwards spreads out in numerous channels enclosing sand-banks and willow-covered islands. It crosses, in fact, the bed of an ancient lake, of which the Lac du Bourget is the last remnant. Anciently the great glaciers of the Rhone and the Isere met in this depression, which subsequently was converted into a huge lake, fed by the Drac, the Romanche, the Isere, and the Rhone, The glacial drift and erratic blocks, which cover the mountain slopes to a height of 1,600 feet, sufficiently prove this. The Lake of Bourget has been immortalised by Lamartine's verse, and although its shores are comparatively barren, the bold grey wall of Mont du Chat reflected in its blue waters when the sun is about to set, and its wooded peninsulas, afford superb contrasts. On leaving the swampy plain of Chautagne and Lavours, with its sluggish ditches and coveys of wild ducks, the Rhone for the last time takes its course through a narrow gorge, overlooked in the north by the old Chartreuse of Pierre- Chatel, perched on the summit of an isolated limestone rock. Having received the Guiers from the south, the river turns abruptly to the north-west, and as far as the jDlain of the Ain flows along the western foot of the Jura. Throughout this portion of its course the Rhone has frequently changed its bed, and there is reason to believe that it formerly flowed west across the shingles and gravels deposited by ancient glaciers, and joined the Saone to the south of Lyons. The relief of this portion of France has undergone a rapid transformation ever since these glaciers retired from the vicinity of Lyons. In the valley of the Drac erratic blocks are scattered over the hillsides to a height of 4,260 feet above the river, and near Lyons up to 1,150 feet. Rock-groovings, locally known as marcs, or mud terraces, abound throughout these hiUs. Below its junction with the Ain the Rhone spreads out and forms innumerable islands, its bed near the hills of Miribel being no less than 2 miles wide. But soon after it loses its lacustrine character ; its waters are confined to a single bed ; and at Lyons it joins the Saone, and thence flows majestically southwards towards the Mediterranean. A sail down the Rhone from Lyons is a source of great delight to the traveller. Swiftly carried along,* he passes ever-varj'Lng scenes of beauty. Without much swerving to the left or right, the Rhone, overcoming every obstacle, flows due south, and ]\Iichelet aptly likens it to a " furious bull rushing from the Alps to the sea." Rapidly do we pass black rocks and willow-clad islands, woods, crum- bling ruins perched upon bold jDromontories, and populous towns. Looking up the tributary valleys, we now and then get a peep at the distant mountains, the white summits of the Alps on the left, the burnt- out volcanoes of Central France on the * Length of the Rhone, from the confluence with the Saone to the sea, 201 miles ; total fall, 532 feet, or 32 inches per mile. THE RHONE AND OTHER RIVERS. 98 right. In front the powerful mass of the Ventoux gradually grows in size until it shuts out one-half of the horizon. We are approaching a southern clime. Olive- trees appear in the vineyards, and the rocks assume that calcined appearance Pig. 67. — AscrexT Glacifrs op the Rhone asd the IsiiiB. Scale I : ssaooo. lu Miles. which is 80 characteristic of Greece and Sicily, At length the wide plain bounded by the Cevennes and the foot-hills of the Alps stretches out before us, only a few isolated hillocks rising above it like islands. The glacier-bom Isore is the fir^t, great tributary which joins the Rhone below VOL. II. H 94 FEANCE. Lyons. "Where it leaves the valley of Tiges it is a considerable torrent, whicli the accession of the torrents of the Tarentaise and of the Arc convert into a powerful river. Formerly the Isere fed a huge lake, but now it takes its course through the valley of Graisivaudan, the bed of an ancient glacier river wide enough to accom- modate a Nile or a Ganges. Formerly the Isere, when in flood, could spread itself over this vallej-, but embankments now confine its bed to a uniform width of 367 feet. These embankments sufficiently protect the country on ordinary occasions, but inundations, when they do occur now, prove all the more formidable to Grenoble. Close to that town the Drac joins from the south, its principal tribu- tary, the Romanche, rising in the glaciers in the west of the mountain mass of Oisans. In the twelfth century a landslip converted a portion of the valley of the latter into a lake, and when the barrier broke in 1219, the freed waters carried destruction before them, and even the inhabitants of Grenoble had to flee for their lives. Among the smaller rivers which join the Isere lower down, the Fure is the Fig. 68. — Plain of La Valloire. Scale 1 : 400,000. 3°lE of Taris '■J^r07Tns/ / SiTlin'; IMUe. most important. It rises in the Lake of Paladru, fiimous for its pile dwellings. As to the rivers which disappear in the swallows {avaloirs) of the plateau of Bievre, and passing beneath the huge moraine of Antimont, reappear again through the "eyes" [chiires) near St. Rambert, they flow direct to the Rhone. The discharge of the Isere varies exceedingly according to the seasons, and, owing to the grey tint imparted to its water by the triturated rocks suspended in it, can be traced for several miles below the confluence. A few barges navigate this large river, but the traffic is of no importance whatever. The Drome traverses several small lakes formed in the fifteenth century by landslips, or clajjiers, but not being fed by glaciers, its volume varies much according to the seasons. And the same may be said of the other rivers rising in the foot-hills of the Alps ; they are mere torrents, almost dry in summer, but carrying destruction before them after heavy rains. Very different from these are the rivers which cross the fertile plains of Car- pentras and Avignon, for they are fed from subterranean reservoirs in the lime- THE imuNE AND OTHER RR'ERS. 05 stone liills, and their springs do not dry up, even in the height of summer. Fore- most amongst these rivers is the Sorgues of Vaucluse, which rises a considerable river from a cavern surrounded by barren precipices. Flowing past a monument dedicated to Petrarch, it debouches upon the plain, and ramifies into numerous canals, which carry fertility wherever they go. Formerly the plain lying between the mountains and a range of limestone hills separating it from the Rhone valley was covered with lakelets and swamps, but drainage works have transformed it into a most productive district. The proximity of the mountains of Vivarais and of the C^vennes to the western bank of the Rhone has prevented the formation of long rivers, but the torrents which rise in these mountains rival even the Mississippi in volume when flooded. Fig. 69.— The Sorci-es of Vauclvse. Scale 1 : 260,000. |3' JO E. u ll*. fit- } tiu^luie io fc. ol C,r. : Miles. M. ilarchegay has calculated that on the 10th of September, 1857, the Doux, the Erieux, and the Ardeche, all of them lying within the limits of a single department, discharged everj* second 494,000 cubic feet of water into the Rhone. This is more than the discharge of the Ganges and Euphrates combined. Fortunately the floods occurring on both sides of the Rhone valley never coincide, for the western slope of the Alps is sheltered from the moisture-laden winds which precipitate torrents of rain upon the ilediterranean slopes of the Cevennes. If this coincidence existed the lower valley of the Rhone would be converted into a pestilential swamp. As it is, the damage done by inundations sometimes amounts to millions, and in 1840 the whole of Camargue and the plains on both banks of the Rhone were converted into a fresh-water lake 25 miles wide. The erosive power of these torrents is wonderfully great. The Ardeche more II 2 96 FEANCE. especially, rising seventy and more feet when in flood, has done maryels iu that respect. At one spot it has atandoned its ancient bed, forcing itself a fresh passage through a wall of rock. This is the famous Pout d'Arc, or the " Arch," one Fig. 70.— Pont d'Aro (Ard^che). Scale 1 : 400,000. 2°|5"E.of Pari.i :■" 2J'F,.of r.r. 1 Mile. of the curiosities of the valley, which boasts, moreover, of columns of basalt and of remarkable canons. The valleys of the Ceze and the Gard, or Garden, likewise abound in natural beauties. The latter disappears for a short distance between the rocks. Where it debouches from its gorge it is spanned by a beautiful Eoman aqueduct, which formerly supplied Nimes with water. It is a work of imposing grandeur, but the modern railway bridges and viaducts, close by, need not dread comparison with it. TILE RHONE AND OTIIEK EIVEES. 97 The Durance, which joius the Rhone a short distance below Avignon, is sup- posed by geologists to have formerly emptied itself into the Bay of Fus, to the east of the mouths of the Rhone. Subsequently it excavated itself a passage, severing the Leberon from the Alpines ; and this much is certain, that the canal of the Alpines is an ancient bed of it. The Durance, like the Iserc, is a son of the Alps, and though its head-stream, the Clairee, is not fed by glaciers, several of its tributaries are. These glaciers, however, are not very extensive, and the river, Tig 71. — Pont d'.:Vkc (AnnicHE). down to its mouth, has the character of a torrent, reduced at one time to a thin thread meandering amongst craiis, or fields of shingle, at others more voluminous than all the rivers of France together. The geological work performed by this river has been immense. .tVmongst the ancient lake beds now silted up, that extending from Sisterou to the mouth of the Verdon is one of the most remarkable, because of its earthy slopes of Mees, curiously carved into obelisks and pillars. In spite of its length of 236 miles and an average discharge of 12,2G0 cubic feet per 98 FEANCE. second (maximvim 320,000, minimum 1,906 cubic feet), the Durance is not navi- gable. During the Middle Ages vessels were able to proceed up to Pertuis, and we may conclude from this that there then existed lakes or barriers in its upper course which regulated its flow. But though not navigable, the Durance is invaluable for purposes of irrigation. The 18,000,000 tons of mud annually carried down it are computed by M. Herve-Mangon to contain as much assimilable nitrogen as 100,000 tons of the best guano, and as much carbon as could be supplied annually from a forest 121,100 acres in extent. On leaving the gorge of Mirabeau, where it is spanned by a bridge only 490 feet in length, the Durance enters upon a broad Fig. 72. — The Roman Aoueduct over the Gabd. valley, which would be scorched by the sun if it were not for the fertilising waters derived from it. One canal, that of Marseilles, taps it near Pertuis, and crossing the valley of the Arc at Roquefavour on a magnificent aqueduct, irrigates the gardens of Marseilles before entering the Mediterranean. Another canal, that of Crapponne, leaves the river lower down, and ramifies into numerous branches. It was excavated in the sixteenth century, and has converted the whilom barren tracts through which it leads into one of the most productive districts of France. A third canal skirts the Alpines on the north, and a fourth extends north in the direction THE Rh6nE and other EIVEES. 90 of Carpentras. Ou an average these four canals absorb about 2,440 cubic feet of water every second. Quite recently, iu 1875, tbo Vordon, one of the principal tributaries of the Durance, was tapped, and now supplies Aix with 210 cubic feet of water everj- minute. It passes throuf^h two tunnels, the one 13,000, the other 16,000 feet iu length. Several dams have been thrown across the gorges of the Upper Durance and Verdou to regulate the floods, and the conversion of the small Lake of Alios, near the source of the Vcrdon and at an elevation of 7,200 feet, into a huge reservoir, has been talked about. Next to the huertas of 8pain and the Fig. 73. — TuE Crau ant) the Canal of Ckapponxe. Scale 1 : 630,000. "iSoE.of Pnri'.. .^*" ■ '\ ^ .lit! 'If __ V , \' ^ H. I ii 11 i' ^^j ^ ' '-^ ,\ :■ '^^j- i|B^:.:„ ^ ....rJ:- I' ' ■ V,', ycj.J'crf'r' vwyff -^»*\ ♦ "ISoEoTOr. /rriyale^ MUes. plains of Lombardy, the valley of the Lower Durance is oven now the best-irrigated district of Europe. By means of these canals, planned by Adam de Crapponne, the whole of the stony desert known as Crau might bo converted into fertile land in the course of three hundred and twenty j-ears. This district, about 131,000 acres, is comi^letely covered with flints, some of them embedded in hardened mud. Six-sevenths of these flints have been deposited by the Rhone, the remainder by the Durance. The pudding-stones upon which they rest arc of marine origin, and the Crau has 100 FRANCE. altogether tlie appearance of an ancient bed of the sea. Formerly this waterless waste was visited only by baijles, or herdsmen, but the canals which now traverse it are skirted by trees and cvdtivated fields. Some of the rain which falls upon this tract finds its way through subterranean channels to the vicinity of the sea, and there reappears again in plenteous springs. More than three hundred such gush forth to the north of the lagoon of Galejon. They are known as Laurons, a name frequently given to springs in other parts of France. At some future time the Rhone itself may be utilised for purposes of irrigation, more extensively than at present. This river, owing to its rapid current, is of but little use as a navigable high-road, and since the completion of the railway from Lyons to Marseilles the sixty-two steamers which formerly navigated it Fig. 74. — The Canal of the Verdon. Scale 1 : 240,000. ■"' 1' "11' Paris ^( --nrtfe'^ F^.^ i^^i 'K'E of CirT even during the Middle Ages there existed a navigable branch which led into the lagoon of Thau. >!. Erailien Dumas has pointed out that each ramification of the river led to corresponding changes in the coast-line. When the Rhone first bifurcated at the Forks the beach extended to what is now the northern part of the deltoid island of Camargue. Since that time the fauna of the Mediterranean has undergone some changes. The Panopwa Aklrovandi, which is now fomid only on the coast of Sicily, was then common on the Lion Gulf, and the Pecfen maximus, at present very rare, abounded. The delta formed by the two main branches of the river wholly consists of an alluN-ial deposit of mud. It covers an area of 185,000 acres, about one-half of which is included in the island of Camargue, dusty in summer, half drowned in winter, and almost without inhabitants. If we may judge from the Roman 102 FEANCE. ruins discovered there, the country was formerly more salubrious. The embank- ments which now confine the Rhone are probably the cause of this insalubrity, for they prevent the drainage of the stagnant, fever-breeding pools in their rear, besides preventing the deposition of fresh alluvium. In the northern portion of this island there are a few fields, cutlivated by peasants who brave the fever, besides extensive pasture grounds, roamed over by white horses, half- wild cattle, and manacles of buffaloes {Bos buhahis), which figure on the racecourses of the towns of Southern France. The " Little Sea," or lagoon of Vaccares, in the south, with its fringe of marshes and tamarisk thickets, is an ancient arm of the sea, from which it is separated now by a chain of dunes. Near it are saline tracts {san- ionires) void of all vegetation, and rarely visited by man, but the resort of num- berless migratory birds. Even flamingoes are occasionally seen, and the beavers which have built their lodges in the embankments lining the Little Rhone are not interfered with. A beautiful tree, resembliug the aspen, grows on the more elevated sites of the Camargue, and the canals that traverse its northern portion are fringed with willows, poplars, and elms, but the forests which anciently covered the whole of its interior have disappeared. Scarcely one-fifth of the area of the Camargue is under cultivation now, and although the cold mistral interferes with the success of certain plants, the delta of the Rhone might nevertheless bo converted into a region equalling in fertility the delta of the Nile. No less than 27,500,000 cubic yards of alluvial soil are annually swept into the sea, instead of being utilised, and a bar closes all access to the river by large vessels. An artesian well near Aigucs-Mortes, in the Little Camargue, though bored to a depth of 330 feet, only passed through such alluvial soil, without reaching the solid rock. The delta of the Rhone has gained upon the sea ever since the time of the Romans. A watch-tower built at the mouth of the Great Rhone in 1787 now stands five miles above it, thus showing that the annual rate of growth since that date has amounted to 175 feet. Altogether between 80 and 120 square miles of land have been added to the delta of the Rhone since the Gallo- Roman period. We have seen above that the mouths of the Rh6ne are obstructed by bars, the formation of which is promoted by the almost entire absence of tides, the flood in the Lion Gulf only rising 16 inches. The embankments which have been constructed have failed to remove the obstacles to navigation, and vessels drawing more than 10 feet can scarcely ever venture to enter the river, even though the wind should be favourable. In the time of the Romans Aries communicated with the sea by a chain of lagoons and canals constructed by Marius, and hence known as Fossw Mariana'. But the canal of Aries, which replaces this ancient water-way, is navigable only for small vessels. At length, in 1863, thanks to the persever- ing advocacy of M. Hippolyte Pent, a ship canal 20 feet deep was constructed between the tower of St. Louis and the Gulf of Fos. This canal leads into a huge basin covering 34 acres, by the side of which a new commercial town is springing into existence, and a railway wlU soon establish rapid communications between this new port and the remainder of France. In spite of the vicinity of the marshes the mortality at St. Louis is not greater than at Aries, and might be very THE RHONE AND OTHER RIVERS. 103 luucli reduced by a proper attention to sanituiy laws ; and if the place has not prospered hitherto, this is due to the jealousies of Marseilles and of the powerful railway company, the one dreading the loss of its monopoly, the other the develop- ment of an important river traffic. One danger, however, threatens the prosperity of this canal — the Gulf of Fos is gradually being silted up ; but this danger might he removed by diverting the waters of the Great Rhone into the "Grau," or lagoon, of Roustan. The changes in the course of the Little Rhone are historically as important as those of the Great Rhone. St. Gilles, accessible now only to canal boats, was Fig. 76. — The Canal of St. Louis. formerly one of the great ports of Southern France, at which most of the pilgrims going to Palestine embarked during the twelfth century. Aigues-Mortes, lower down on the same branch of the river, sprang into existence subsequentlj'. But about the middle of the sixteenth century the Little Rhone took a more easterly course, and it now enters the sea through the Grau of Orgon, near which is the fishing village of Saintes-Maries, separated by vast sands and swamps from all other centres of population. There, as well as farther east, at the lighthouse of Faraman, the sea is gaining upon the land. The town of Aigues-Mortes, thus called on account of the stagnant waters 10-1 FEANCE. which surround it, has frequently been cited in proof of a remarkable encroach- meut 6i the sea, but erroneously in our opinion. The local guides point out the spot at which St. Louis is said to have embarked for the Holy Land, though it has been proved conclusively that he did so at a point five miles to the south-west of the town. The vessels which were to convey the crusaders cast anchor at the spot marked A upon our plan, close to the mouth of an old canal, still known as Grau Louis. The remains of embankments and the vestiges of a crusaders' burial- ground enable us to trace the direction of this canal, which anciently connected Fig. 77. — The Lagoons of Aigces-Moeies. Scale 1 : lOO.nOO. »<":.•. '-%. ■s %.\ 3'-' ' ' \t O'nuiiin (lii in , -_'---\^ i-l lo E.of Gt A A. *' Foreign " Roadstead where the crosaders embarked. B. Site of Port in thirteenth century. C. Site of Port, thirteenth to eighteenth century. 1 Mde. the town with its port at Grau Louis. Since then the lagoons have undergone many changes, partly owing to the alluvium deposited by the Ehone and other rivers, partly in consequence of the construction of a new canal by Louis XV., which enters the sea at the Grau du Eoi. If any further jDroof were wanted in support of the assertion that the sea along that part of the coast has not encroached upon the land, it would be furnished by the existence of four lines of dunes, which mark as many conquests of the land over the sea. The town of Aigues-Mortes undoubtedly occupies a site which was anciently covered by the floods of the THE Eh6nE and other ElVEES. 105 ireditcrranean. The outermost of tlieso lines of dunes, that of Boucanet, only supports a few tamarisks, but the innermost is covered with a forest of maritime Fig. 78.— The Delta of the Auuk. Scale 1 : 225,000. pines, which impart a character of mournful grandeur to the landscape. This fcSylve Qodesque, however, has been reduced to very small dimensions in our day. 106 FEANCE. A careful examination of this portion of the coast-line enables us to assert that it will remain stable for centuries to come. The Little Rhone annually carries about 5,232,000 cubic yards of sediment to the sea, but nearly all this is deposited near the lighthouse of Espiguette, to the east of the Gulf of Aigues-Mortes ; and supposing this point to continue to encroach upon the sea at its present rate, no less than two thousand years will have to elapse before the gulf is converted into a lagoon. The roadstead at Aigues-Mortes is, moreover, sheltered from the dangerous south-easterly winds, and the construction of a harbour of refuge at the Grau du Roi has consequently been advocated by competent engineers. Aigues-Mortes, which now hardly imports anything but the oranges of Valencia and of the Balearic Isles, might then become an important seaport. The rivers which flow from the slopes of the Cevennes into the Mediterranean may be considered as belonging geologically to the basin of the Rhone. Even the Aude, the first river to the north of the Pyrenees, bears a certain family likeness to the torrents of the Rhone valley, although only its northern tributaries rise in the Cevennes. Like all other Mediterranean rivers born in these mountains, the Aude presents all the features of a torrent, its volume fluctuating according to the seasons between 180,000 and 106,000 cubic feet per second. On leaving the gorges of Capsir and the forest of Sault the Aude flows due north until, below Carcassonne, it is joined by the Fresquel, when it curves round to the east. The delta of this river is proportionately more extensive than that of the Rhone, for it covers 50,000 acres, and between its two arms is enclosed the ancient mountain island of La Clape. No less than 2,224,000 cubic yards of mud are annually carried down the river, most of which is deposited upon the inland swamps, the mountain barrier at the mouth of the river preventing it from being carried into the sea. In the time of St. Louis there were salt-pans on the swamp of Capestang. It is now sepa- rated from the sea by 9 miles of solid land. The swamp of Montady has been converted into dry land since the middle of the thirteenth century. The site of Lake Rubrensis, which extended to the walls of Narbonne, is now occupied by fields ; and the lagoons of Gruissan and Bages, which formerly were one, are now separated by a strip of alluvial land. The Canal du Midi, or Great Southern Canal, with its branches no less than 339 miles in length, accompanies the Aude during the greater part of its course. Its supply of water is principally derived from the Alzau, Lampy, and other small rivers rising in the Cevennes. These are intercepted by a canal (Rigole de la Montagne) leading into the lake-like reservoir of St. Ferreol, holding 6,254,000 tons of water, whence another Rigole leads down to the navigation canal. Unfor- tunately, this great work of the seventeenth century, which connects the Rhone with the Garonne, has fallen into the clutches of the Great Southern Railway Company, and is but little used for the conveyance of merchandise. The Orb enters the sea to the east of the Aude. It discharges its waters through a single mouth now, that of Grande Ma'ire having almost become oblite- rated, and dwindles down into an insignificant stream during summer. The H^rault, THE RHONE AND OTHEE EIVEES. 107 its neiglibour, and the most important river between the Aude and the Rhone, on the other hand, is fed by plenteous springs rising in wild limestone gorges. The river is navigable for sea-going vessels throughout the year as far as Agde, and Richelieu began the construction of a breakwater at its mouth, which has never been completed, the engineers having since then devoted the whole of their energies to the creation of an artificial harbour at Cette. Amongst the small rivers between the Herault and the Rhone the Lez is the best known, because it flows past Montpellicr, but the A'idourle is far more tj-pical of the torrents descending from the Cevennes. During the dry season it does not Fig. 79. — RiGOLES OP THE Cax.^l du Mioi. Scale 1 : 320,000. I lu; W . of P Q n e . . ■ *■ a- Ejo[ Or. i iiiles. even reach the Mediterranean, but when iu flood its volume exceeds that of the Seine at Paris thirty times, and the inhabitants then utilise it for irrigating the reed-banks of the lagoon of Repausset, near Aigues-Mortes, the produce of which ia converted into manure or used for covering chairs. The Argens is the only French river to the east of the Rhone which can fairlj- claim that epithet. Like many other rividets in that limestone region, for a portion of its upper course it passes underground, but long before it falls into the shallow Bay of Frejus it becomes a placid stream, maintaining a fair volume throughout the year. There are several underground rivers along this Provenfal coast, which only rise as springs beneath the waves of the Mediterranean. -108 FEANCE. Perhaps the most remarkable of these is the spring of Port-Miou, near Cassis, which originates in the ancient Lakes of Aubague and Gemenos, drained by King Rene, and gushes forth with sufficient violence to create a veritable current. The Var, which for a long period formed the boundary between France and Italy, though longer than the Argens, remains a current down to its embouchure, being reduced at one time to a mere streamlet, at others rushing down with such violence as to overflow its embankments, though these are 2,600 feet apart. Fig. 80. — The MoniH op the Herault and Cap d'Agde. Scale 1 : 70,000. r 10 E ot I'jTis I.et.F? |J' Jo £ ^i Cr o-J^i Fa/Aorna . 2%- S FcuOuiTns IMile. Over S Pathoma . Co.iST-LINE AND L.4.G00NS. The difference between the configuration of the coast on both sides of the Rhone delta is most striking. In Provence we meet with bold cliffs and promon- tories, whilst to the east of the river we find ourselves in the presence of a beach formed of sand carried down from the granitic mountains in the interior of the coimtry. In Provence the cliffs sink down almost precipitously into the sea. and molluscs are found there only in a few sandy creeks, whilst on the coast of Languedoc the sea deepens gradually. This difference of physical configuration accounts to a great extent for the history of the two provinces. In the one case COAST-LTNE AND LAGOOXS. 109 towns were built close upon the sea, in tlie other they arc remote from it, and Languedoc thus possesses the characteristics of an inhind country rather tlian of a maritime one. In its details the beach of Languedoc is not without beauty. It is broken up by mountains, hills, or masses of rock into a number of sections. One of these Fig. 81. — Lkvcate Axn the R(hiistkai> op Fkansii. Scale 1 ; &S,UOO. S'll ol Or i'.i-f S~lo - 1 Mile Ovtr io FaUlom» extends between the Point of CoUioure and Cape Leucate ; a second sweeps round from the latter to the Cape of Agdo ; a third reaches thence to Cette ; whilst the fourth and last stretches from Cette to the sandy flats of the Khone delta. The promontories afford some shelter to vessels endangered by the dreaded tempests of the Lion GhJf, but the most secure anchorage along that coast, that of Franqui, to vol.. II. 110 FRANCE. the nortli of the peninsula of Leiicate, has not yet been converted into a port, although possessed of special facilities for the construction of one. With the exception of the Cape of Agde, which is an extinct volcano, the ancient rocky islands along that coast, now joined to the mainland by alluvial deposits, are composed of cretaceous or Jurassic limestone. The ancient crater of Agde has been converted into a vineyard. Streams of lava extend from it in all directions. A few minor volcanoes are near it. The ancient coast, such as it existed before the volcano of Agde had become a portion of the mainland, can still be traced by following the contours of the hills Fig. 82.— The Lagoon of Thau. . 5 Miles. bounding the alluvial plains. Lagoons, or etangs, extend along the whole of the coast, from the very foot of the Alberes ; and where no sediment-bearing rivers flow into them, they are of considerable area and depth. That of Leucate is a case in point. No river flows into it, but close by, at the foot of a limestone rock, rise the remarkable springs of Salses, now known as Font-Dame and Font-Estramer, discharging streams of water having nearly the same chemical composition as that of the ocean. At the side of the Font-Estramer grows a species of reed — Phrag- mites gigantea — which is not met with anywhere else in Europe. The lugoon of Thau (Taphrus), between the volcano of Agde and the hills of COAST-LINE AND LAGOONS. Ill La GartUole (774 feet), is the most important of all, on account of its great depth and tlie towns which line its shores. This little sea of 18,500 acres is separated from the Mediterranean by a narrow strip of land. A narrow clianncl, furnished with locks, and forming the eastern termination of the Great Southern Canal, connects it with the open sea. Another canal, nearly 40 miles in length, places it in communica- tion with the delta of the Rhone. The lagoon is thus of considerable importance to navigation. Its waters are as salt as those of the sea, except after heavy rains and near the mouths of some of the rivers which enter it. A bounteous spring. Fig. 83. — BioN'OMiCAL Condition of the Littoiial Region of Hkkaii.t. The drclea Indicate proportionaJly to what extent the mean age at death is inferior to that throngboat France. The asterisk denotes a locality where the mean age is higher than the average throughout France* known as the " Abize " (abyss), rises from the bottom of the lagoon in the north, and not far from it there is an intermittent spring which discharges fresh water during winter, up to April, but swallows up the water of the lagoon, a phenomenon similar to what has been noticed at Argostoli, on the island of Cephalonia. The lagoon of Thau is public property, and supplies annually £40,000 worth of fish and shells. Oysters are said to have abounded in it formerly, and an old bed has been dbcovered at a distance of 500 yards from the modern beach, but an attempt to breed oysters there has failed signally. There can be no doubt that these lagoons might easily be drained and converted i2 112 FEANCE. into fertile fields. Experiments on a small scale, which were made at Narbonne and Vic, have been attended by the most perfect success. This is not merely a question of converting 60,000 acres of lagoon, at present producing only fish, willows, and reeds, into productive arable land ; it is still more important in its bear- ings upon the salubrity of the climate. M. Regy has calculated that these swamps shorten the lives of the people who reside near them to the extent of ten, fifteen, and even nineteen j^ears. More than half the children at Mireval and Yias die before they have attained their sixth year, and strangers who settle in the country almost Fig. 84. — Etang de Berre. Scale 1 : 320,000. . 5 Miles. invariably suSer from marsh fever. Those lagoons which are over 3 feet in depth do not injuriously affect the health of the people who live near them, and the mortality at Cette and other places on the lagoon of Thau is hardly greater than in the rest of France. But when the water, owing to its shallowness, attains a temperature of 82° F., it becomes dangerous to health. These shallow lagoons ought, therefore, either to be suppressed, or be made to communicate freely with the open sea. In the case of the lagoon of Mauguio the latter has already been done, and the same treatment would prove eiBcacious with those of Vic and COAST-LIXE AND LAGOONS. lid Frontignaii ; but il. Rt^gy is of opiuion that all others, being very shallow, sliould be converted into polders without loss of time. The changes in the configuration of the lagoons have led, within the historical period, to a di>placement of the principal towns. Astruc, more than a century ago, observed that the names of the towns on the hills were Celtic, whilst those near the coast invariably bore Greek or Latin appellations. It may fairly bo inferred from this that the coast became habitable only at a comparatively recent epoch. The encroachment of the land upon the sea enabled the inhabitants to found quite a chain of new towns, including Agde, Cette, Frontignan, and Aigues- Mortes. Maguelone, however, which formerly stood upon an island, now joined to the mainland, appears to be of ancient foundation. It was a busy place of commerce as long as the Saracens held it. After their expulsion by Charles Martel it again rose from its ashes, but having become a place of refuge of the Fig. 85. — Tub Canal op Cabontb. Scale 1 : 8S.00O. Protestants, it was finally destroyed by order of Louis XIII., and there now only remains an ancient church, forming a prominent object in the midst of the sands. The only lagoons to the east of the Rhone which originated in the same manner as those on the Lion Gulf are those of Valduc, Engrenier, and several others, which formerly communicated with the sea through a channel, now closed by a bar, and known as the lagoon of Estomac (Stoma-Limne). As to the lagoons of Valduc and Engrenier, they are shut oflf from the Mediterranean altogether, and, owing to an excess of evaporation, their level, on an average, is about 30 feet lower than that of the sea. They are miniature Caspians, and yield a con- siderable amount of salt. The large inland sea known as Etang de Berre is not a Ugoon, but a gulf, separated from the Mediterranean by a rocky ridge. The Romans had a port on this gulf, but it is now only frequented by a few fishermen, and not a single town 114 FRANCE. rises from its shores ; and yet, by deepening the canal of Caronte, which joins it to the Mediterranean, this great natural harbour might be rendered accessible to the largest vessels. If the Etang de Borre belonged to England, it would long ago have been converted into a great commercial and naval depot. Vessels at anchor within it are not only beyond the reach of an enemy's guns, but, being hidden by the coast range of Estaque, the)' are actually out of sight. The owners of the fisheries, or bonligiies, are bound to dredge the canal of Caronte to a depth of 39 inches. AYere they to neglect doing so, it would quickly become choked, and the Etang de Eerre shut off from the sea. Climate.* Ho■^^'EVER striking the differences between the littoral regions on both sides of the Rhone, they enjoy the same climate, alwaj's excepting the fever-stricken neigh- bourhoods of the swamps. This Fig. 86.— The Preyailixo Winds at Aigues-Moetes. climate differs essentially from what is met with in the remain- der of France, for land winds predominate here, whilst sea winds prevail in all the depart- ments beyond the Cevennes and the wide valley of the Rhone. The air is drier, and it rains less frequently, though, as a rule, iu heavy showers. No visitor to the south of France can have failed to notice the gusts of north-westerly wind which blow from the Cevennes, and are jiroduced by local causes. This violent wind is known as " mistral " [mofjis traou) or " master," and it fully deserves that epithet, for its velocity sometimes equals that of a hurricane. Strabo tells us that this " black norther" lifted men off their cars and carried away their clothes, and in our days it has overturned railway trains. Not a tree in the plains of Avignon and on the islands of the Rhone but exhibits traces of its violence. The originating cause of this wind must be looked for in the great contrast between a sandy beach scorched by the raj^s of the sun and a snow-clad mountain range. The heated air above the former rises, whilst the cold mountain air rushes down the hillsides to establish an equilibrium. The gieater the difference between the temjjerature of these two atmospheric strata, the greater the violence of the wind. In the night, when the beach has cooled down by radiation, On the rains in Herault see a paper by M. Ch. Martins, in Mem. de I'Ac. de Montpellier, riii. 1872. ATJDE. 115 there is a lull, and at some distance from the land it is hardly felt at all. In spite of the dread it inspires, the mistral is a welcome visitor, for it purifies the air of the to\ms, which are not always remarkahle for cleanliness. The contrasts existing between the coast regions and the mountains, and the winds resulting therefrom, account for the frequency of thunder-storms in the low lands. As long as the mistral and the sea wind are not engaged in a conflict, the clouds drift towards the mountains, and there descend in rain. But when the mistral, blowing in the higher strata of the atmosphere, is mot by the cloud-laden sea breeze, an exchange of electricity takes i)luce between them, and the rain descends in torrents. As a rule the rainfall increases as we proceed from the coast towards the mountains, and is most copious in autumn. There are, however, many exceptions to this rule, and there have been years when it rained most heavily in February, and scarcely at all in autumn. This capriciousness of the climate appears to be reflected in the character of the " Gavaches " of the Cevennes and the " Franciaux " of Dauphin^. They, too, have their bursts of passion, but quickly calm down, being not unlike, in this respect, to the mistral or to a thunder-storm. Topography. Ai'DE. — This department, named after its principal river, is eminently a land of passage, bordering upon the Mediterranean, but partly lying within the basin of the Garonne. It is almost exclusively an agricultural country, manufactures existing only in the to\NTis and in the upper valley of the Hers. Less than one- third of its area is under cultivation, and although its vineyards are of some importance, the population is far from dense. Castelnaudary (7,628 inhabitants), on the water-shed between the Mediter- ranean and the Atlantic, has played a great part during the civil wars ; but the frequent sieges which it has undergone have prevented it from becoming a great commercial town. "Windmills now occupy the sites of its ancient forts, it is the busiest ship-yard on the Canal du Midi, and manufactures coarse cloths, like most other towns of that part of Languedoc. Bclpcch (978 inhabitants), 6Vc. Colomhe, and Chalabre (1,792 inhabitants), all of them to the south, on the Tipper Hers, are likewise noted for their cloths and linens. The river Aude enters the department thi-ough the terrible gorge of Car- canieres. Lower down it flows past QidUan (2,286 inhabitants), a busy place, with saw-mills supplied with fir-trees from the forest of Sault, in the Pyrenees. There are several noted mineral springs in the vicinity, including the suljjhur springs of Gino/cs, in the south-west ; the ferruginous springs of Eennes-les-Bains, in the valley of the Sals, to the north-east ; and those of Couiza and Alct, on the banks of the Aude. Alet was the seat of a bishop during the Middle Ages, and its ancient episcopal palace still overtowers all its other houses. Still following the Aude, we arrive at Limoux (6,037 inhabitants), on the white hills of which is grown a wine known as hianqiiette. Its manufactures of cloth and felt are 116 FBANCE. of little importance now. Carcassonne (23,517 inhabitants), the capital of the department, occupies a favourable site at the elbow of the Aude, and on the high-road connecting the Mediterranean with the Atlantic. The mediseval " city " occupies a hill, and its walls and towers, erected between the fifth and the four- teenth centuries, as well as several remarkable old buildings, still remain to it. The lower town, however, is h\ far the most populous. Its fortifications have been razed to gain space for houses and manufactures. Carcassonne, besides manufacturing much cloth, carries on a considerable commerce with wines and agricultural produce, and also exports the fine marbles of Caunes (1,998 inha- bitants) . Narbonne (18,325 inhabitants), the maritime capital of the department, was of far greater importance during the dominion of the Romans, when it boasted Fig. 87.— The Port or La Nouvelle. Scale 1 : 3,000. 1,000 Yards. of 80,000 inhabitants, and of magnificent public buildings, of which only few traces exist now. The church of St. Just is the most remarkable amongst its medifEval buildings. The geographical position of Narbonne is excellent, but, owing to the silting up of the lagoons and canals, it no longer enjoys the advantages of a maritime citJ^ The canal which connects it with its port of La Nouvelle is only navigable for fishing-smacks, and possesses no importance whatever. The environs of the city, however, have been brought under cultivation, and there is a busy trade in wine. The most important towns of the arrondissement of Narbonne are Lizignan (4,402 inhabitants), with numerous distilleries, and Sigcan (3,510 inhabitants), on a hill overlooking the lagoon and its salt works. Gruissan (2,382 inhabitants) is hardly more than a village of salt-makers and fishermen, whilst Coursan (2,507 inhabitants), in the valley of the Aude, stands in the most fertile district of the ■•4 'A O 03 CO P3 u LIBRARY OF THE ^INIVERSITY of ILLINOIS, HERAULT. 117 department. Anniir. b°\ui S°|>i' C^ Janet Ra de d e Marseille li ■atf j.a'P'd-Jf., ^■^p % ■ % aft57'E.i»fPai-i3 z'W T33 of Longchamps. The best view of the city is obtained from the tower of the Byzantine church of Notre-Dame, which crowns the most elevated hill to the south of Marseilles. The public promenades, including the Prado, lined with magnificent trees and numerous villas, and the Corniche, which follows the sinuosities of the coast, are a great ornament to the town, and afford magnificent prospects of the harbour and the picturesque promontories which bound it. Marseilles, besides being a great commercial town, may boast of numerous manufactories. In its metallurgical establishments the ores imported from abroad, and more especially lead ores, are smelted. There are huge corn and oil mills and MARSEILLES. 127 tanneries. Provisions arc preserved and salted for the use of the navy. The manufacture of soap (1,020,000 cwts. in 1875) equals that of the whole of the remainder of France. The supar retineries, too, are of great importance. The merchants of Marseilles own a fleet of 783 vessels (including 210 steamers), measuring 194,500 tons, most of these being built at Ciotut, La Seyuc, and even at Genoa. In 1875 8,757 vessels of 2,527,200 tons burden entered the harbour, the imports were valued at £34,781,000, and the exports at £35,485,120. Cereals constitute the principal articles of import, and next to them cattle, cotton, wool, and iron ores from Algeria, Spanish wines, tea, silk, petroleum, timber, hides, guano, sugar, coflfee, and oil seeds. Unfortunately most of the vessels are obliged to leave in ballast, for the high tarifls of the railway companies prevent Marseilles from exporting the coal of the Cevennes and the building stones of the Alps. Marseilles, in spite of the competition of Brindisi and Trieste, still remains the great intermediary for tha conveyance of passengers and costly merchandise between the north-west of Europe and the East. This superioritj', however, it is sure to lose whenever Saloniki and Constantinople become connected with the railway sj-stems of the rest of Europe. It will then have to seek compensation for this loss elsewhere. In this respect Algeria holds out much promise for the future. In 1874 Marseilles imjwrted thence 400,000 tons of ore, 200,000 tons of com, 50,000 tons of alfa, and 1,000,000 head of cuttle. At the same time it will be necessary to develop the railway connections of this great port, which is at present dependent upon a single line for its communication with Paris, and has no direct intercourse at all with either Cette or Bordeaux. The smaller towns in the neighbourhood may almost be looked upon as suburbs of the great city. Cassis, beyond Cap Tiboulen, produces the best wine of Pro- vence, but likewise manufactures muscatel for exportation. At Ciotat (8,104 inha- bitants), a little farther in the same direction, are the ship-yards of the Messa- geries Maritimes, which usually employ 3,200 workmen. Auhagne (5,087 inha- bitants), an inland town, has cement works; whilst Auriol (2,453 inhabitants), Jioqiiecaire (1,749 inhabitants), and Pet/pin, in the upper vaUey of the Huveaume, have coal mines, plaster works, potteries, and soap works. Crossing the hill knovni as La Yiste, to the north of Marseilles, we reach the valley of the Arc, the only important town in which is Au (23,407 inhabitants), the residence of a sovereign during the Middle Ages. Aix, in spite of its ancient Academy, its Court of Appeal, and an archbishop, is a decaying place. It may carry off the honours, but Marseilles has possessed herself of the wealth of Pro- vence. The famous springs are no longer fashionable. The town, nevertheless, is most interesting on account of many of its ancient buildings, including the Roman baths of Sextius ; it carries on a considerable commerce ; and the olives grown in its plain, irrigated by a canal derived from the Yerdon, furnish an oil of world-wide reputation. In the upper valley of the Arc, at Gardanne (2,268 inhabitants), Futeau (2,253 inhabitants), and Trets (2,694 inhabitants), there are coal mines yielding above 300,000 tons annually. k2 128 FEAXCE. An ancient Roman road conducts us from Aix to Salon (5,085 inhabitants), on the margin of the Crau, the fields of which are irrigated by the canal of Crapponne, and thence to Arks (15,563 inhabitants), after Xarbonne the most ancient Roman Fig. 94. — The Mausoleum at St. Eemy. f^/s.;^el^/fe^^ I colony on GfaUic soil. The position of this town at the head of the Rhone delta insures its prosperity. It attained the height of its power in the thirteenth cen- tury, when its flag was seen in aU the ports of the ^Mediterranean, but dissensions amongst its ruling families led to its fall. The town is rich in Roman remains. ARI.KS. 129 inclii(Hn<> an ampliithcatro, and in modiieval buildinjjs, and its women arc famous for tboir beauty and jjood taatc. Alios carries on a considerable conimorco in agri- cultural produce, cattle, horses, and sheep. A bridge connects it with the suburb of Trinquctuilles, in the Camarguo, a district formerly described as the " granary of the Roman army," but now a region of pestiferous swamps. In this district is the hamlet of Huiiitcs-JIdricti, before the church of which stood formerly two marble Fiar- 95.— Kino Rx.sfi's Castlb at Tauascok. lions, in allusion to which the neighbouring gulf is said to liuve been named Lion Gulf(Golfedu Lion). Like Aries, the neighbourhood abounds in ancient remains. At Fonfricile (2,237 inhabitants) there are huge artificial caverns, which served as places of sepulchre in prehistoric times. liaiij; on the Alpines, has an old baronial castle hewn out of the solid rock, and .S7. Riiiii/ (3,490 inhabitants), beyond that range of beauti- fully contoured hills, boasts of a fine mausoleum of the age of Caosar. Tarascon (7,777 inhabitants), the sister city of Beaucaire, has at all times been a great place of traffic. Up to the thirteenth century it stood upon an island, but 130 FEANCE. when King Rene built the castle, the massive proportions of which challenge admiration, the channel separating this island from the left bank of tlie river had been filled up. Var, most absurdly called after the river Var, which lies outside its boundaries, mifht more appropriately become known as Argens, from a river flowing right through its centre. It is a mountainous country, half of its area being covered Fig. 90. —Toulon. Scale 1 : 128,000. lT»r.-F tt f..r,. 2'/i FaOwm. Line 10 ■ 2 Miles. ^^'X with forests. The most flourishing towns lie on the coast, but those in the interior likewise manufacture cloth, felt, paper, and earthenware. Toulon (61,382 inhabitants) enjoys the double advantage of having an excel- lent port and of lying on the high-road connecting France with Italy. The excellent shelter afforded by its port has caused Toulon to be chosen as the great naval station of France in the Mediterranean. The arsenal and dock- yards, begun by Vauban in the seventeenth century, cover an area of 667 acres, and have cost no less than £6,400,000, although much of the work was per- TOULON. 181 formed by convicts. Forts occupy everj' point of vantage, and render Toulon one of the strongest fortresses in Europe. In commerce and industry, however, it ranks very low, in spite of its excellent harbour, on the western side of which are Fio;. 97.— HvKnr.s. ScaUe 1 : 100,000. s-iti K. of r OOJ^FH pE r.lE^S.S Si.lln ,1, ,. J- <- ■\ \ \ I^ADE D' JIYERKS <'1 ' Kadc dr /Cicns Ra* / " ■> ;H^- ,- :? . "■" •^ ^, ^^ . 1*1105* de'^Irfi'aiich' ^ 'J .T >; A IS T\2. V- ■^--iS", pvtr ^ FaUuffs. I Mile. climate, and though its vegetation is less luxuriant than that of Nice, its serene sky and distant horizons render it a most delight ful residence. The isles of Lerins lie ofE its bay, the largest of them, that of Ste. Marguerite, being famous on account of its prison-fort, from which Marshal Bazaine effected his escape, as the 130 FEANCE. " Iron Mask " had done before him. On St. Honorat are the ruins of a monas- tery which was destroj-ed by the Mooi-s in 725. Cannes, in spite of its shallow harbour, is next to Nice the busiest seaport of French Liguria. It is the jDort of Grasse (9,673 inhabitants), l3'ing about 10 miles inland, the vicinity of which produces the best olives of Provence, besides roses, jasmines, and other flowers. The manufacture of perfumery and liqueurs has one of its great centres at Grasse. Fi». 101. — The Caverns of Baousse-Rousse. These seaside towns of the Alpes-Maritimes possess immense advantages as summer resorts, and might be converted into sanatoria for the whole of France. They are supplemented by mountain villages, such as St. 3Tartin-Lantosque (1,956 inhabitants), Eoquebilliere, and others, within easy reach of the coast, and admirably suited for summer stations. Vaucluse, though lying inland to the north of the Rhone delta, is essentially one of the Mediterranean departments of France. Its western half consists of an AVTOXON-. 137 alluvial plain intersected by numerous canals, very productive, and abounding in industrious towns. Arigiion (33,1!^!) inhabitants), at the confluence of the Durance and lllione, was a prosperous town in the time of the Romans, and as an independent common- wealth it ranked amongst the first cities of the south during the twelfth century. The religious wars of the thirteenth century destroyed its wealth. Between 1309 and 137G it was the residence of the popes, and from that epoch in its history date its most striking buildings, its tui-roted walls, its cathedral, and its fortress-like palace on the rock of the Doms, or "lords." From that rock we look down upon the verdant plain, with its plantations of olive and nuilberry trees, its towns and villages, and upon the swiftly flowing waters of the lihone, spanned here by a Fig. 102.— Baous8£-Rou6s£. Accordmg to M. Rl^^^rc. Scale I : 3,000. r°|33' E. gf Cr _ Ear/A fi — ^^ EarUiy SUpfS Ir^""^ Rocky Slojies Carems ', Bone Brcccux^ *' Hearths SS^ Railroail I 1 ho^t^ol oTond. Hjocks lUO Ytuds. su.spension bridge, which replaces an old stone bridge built by the " Devil and St. Benezet" in 1188, but destroyed by a great flood in 1669. Avignon remained the property of the Pope until the great Revolution ; but though it abounded in monasteries, grass grew in its streets, and industry was a stranger to it. But since it has belonged to France it has become one of the busiest towns of the south — spinning the silk grown in the neighbourhood, manufacturing agricultural machinery, and colours from madder, and extending its commerce to the highest valleys of the Alps. The department has not only suffered much from the invasion of the phylloxera and the disease of silkworms, but its cultivation of madder is jeopardised through the invention of aniline colours. The towns and villages lying at the foot of the Leberon and of the hills of 138 FEANCE. Vaucluse are surrounded by verdant fields. CavaiUon (3,906 inhabitants) is environed by gardens irrigated by canals derived from the Calavon and the Durance. L'Ide (3,795 inhabitants) and Thor (1,667 inhabitants) are supplied with water from the fountain of Vaucluse ; Femes (2,801 inhabitants), Monteux (2,262 inhabitants), and Carpentras (8,127 inhabitants), have likewise their canals of irrigation. The latter, though proverbially a dull provincial town, is in reality Fig. 103.— Cannes and the Isles of Leki.vs. Scale 1 : 60,000. f iio F of ra,-L. sSpriHii .U V i !. i, {■: KINS ;:^*?n{o'^^ir- TIE.of Ci- rt: JO VAN \ {-■■': J i r^ i Iv \ Echellc d'> i:fipooo o 5. S-z-j, Tir.i sj-i5o, Over iSq Fajthoms — 1 Mile. a bustling place, supporting a library and museum, and proud of its Roman triumphal arch, its modern town-hall, and its aqueducts. Orange (6,782 inhabitants), the ancient Arausio, and formerly the capital of a county, is the rival of Carpentras in trade and industry, and boasts a Roman amphitheatre and a triumphal arch, which are amongst the finest ruins of that kind in France. Vaison (3,330 inhabitants) has a Roman bridge over the Ouveze, HAUTES-ALPES. 139 and is partly built with the stones of Gullo-Roman buildings. Malauceiie (I.GIO inhabitants) has a Roman aqueduct; Bollinc (3,168 inhabitants) has potteries, and Vdlreas (4,705 inhabitants) carries on a considerable trade in raw silk. Both these towns are surrounded by old walls. Perl ii is (4,905 inhabitants), thus called because of its situation near the gorge, or pcrtuis, of the Durance, has a few factories, but the mountain region beyond it is very thinly inhabited. Apt (4,278 inhabitants), the only town in the mountains, has sulphur mines and pits of plastic clay, from which its potteries are supplied. Hautes-Axpes. — The two departments on the Upper Durance constitute the Kg. lOi. — AVIG.NOX AND THE PAl_iCE OF THE PoPES. poorest and most desolate district of France. Hautes-Alpes, though enjoying the advantage of more extensive forests and pasture grounds than its neighbour Basses- Alpes, ranks, nevertheless, very low as to its agricultural produce ; and its resources not being sufficient to support its population, many of the inhabitants annually descend to the plains in search of work. Brian(O)) (■2,321 inhabitants) defends, with its seven forts, the road over the Mont Genevre, and is the most inhospitable garrison town in France. Descending the Durance, we pass the mountain fort of Mont Baiip/iin and Embrun (3,287 inha- 1-40 FRANCE. bitants), likewise a fortress, the most prominent building within which is a prison. Gap (7,249 inhabitants), the only large town of the department, and its capital, lies about 6 miles to the north of the Durance. The ores and marbles which abound near it have not hitherto been worked. Basses-Alpes is a country of naked mountains, lying almost completely within the basin of the Durance. It is the least-populated department of France, but by planting forests its resources might be considerably developed. Barcelonnette (1,921 inhabitants), on the Ubaye, and at the foot of the Col de Fig. 105. — Col de L.^kche. Scale 1 : 80,000. ■i;■^!,lu'^.'nJ.S^t^ l'-Ai-|ji'r\lT^V(- SuTtiint'^d ^..-r ;I Larche or of Ai-gentiere, is the chief town of the most elevated arrondissement, but otherwise insignificant. Sisferon (3,7G8 inhabitants), lower down on the Durance, is a picturesque town, with an old citadel. Manosque (5,162 inhabitants) enjoys a southern climate, carries on a considerable trade in wine, oil, and fruits, works a coal mine, and has several manufactories. It is the most important town of the department, superior by far to Forcalquier (1,816 inhabitants), the capital of the arrondissement within which it lies, and even to Digne (5,540 inhabitants), the departmental capital. This latter lies on a winter torrent, the Bleonne, 2,098 feet de6me. 141 above the sea, but nevertheless produces excellent fruits, which ils confectioners convert into confitures. Thero are likewaso efficacious sulphur springs. Colmars and Castellannc, on the Vordon, are of no iniportanco whatever. At lilez (Colonia Augusta llcioruiii, ^',.'370 inhabitants) and at Vitlemolea (■■2,182 inha- bitants), botli on tributaries of that river, and at GrtouLi; near its mouth, Uonian ruins have been discovered, and at the latter there are sulphur springs. v\s. lOi;.— Si Drome* has been cut out of ancient Dauphine, and is named after a river that flows through it towards the Rhone, which forms its western boundary. Its climate and productions are similar to those of Ardeche, on the other side of the Rhone ; but Drome is the more mountainous of the two. Nyons (2,4G2 inhabitants), the capital of the southern arrondissement, lies at the mouth of a gorge, from which a cold wind, known as pontias, blows every vol.. 11. • Scipion Gras, " Statistique minSralo de la Dr6ine." L 142 FRANCE. night. Its olive-trees perished ia the cold winter of 1829, and the vineyards then pLmted have recently been attacked by the phylloxera, which has likewise invaded the lowland district of Tricastin, of which St. Paul (1,G57 inhabitants) is the capital. Montelimar (9,512 inhabitants), at the confluence of Jabron and Roubiou, and not far from the Rhone, carries on a brisk trade in agricultural productions and the manufactures of the Protestant town of Dieu-lv-Fit (3,072 inhabitants), on the Upper Jabon. To the south-west of it, on the Lez, rises the sumptuous castle of Gfi(jn(in, kno^vn as the residence of Madame de Sevigne. Crest (4,8-18 inhabitants) is the most important town on the Drome. Its old castle has frequently seen Protestants and political offenders within its walls. Die (3,427 inhabitants), higher up the river, carried on considerable industry before the revocation of the Edict of Nantes. Lirron (1,874 inhabitants) and Lon'ol (2,181 inhabitants), at the mouth of the river, are indebted for theii- prosperity to the railway. Valence (20,476 inhabitants) maintained its municipal liberties until the thir- teenth century, and with its suburb, Bourg-les-Valence (2,o74 inhabitants), is now the seat of a considerable textile industry. ChuhcuU (1,300 inhabitants), near it, has likewise a few factories, but lioiiiaiis (11,024 inhabitants), on the Isere, and its suburb, Bourg-de-Peage (4,151 inhabitants), are at present the great industrial centre of the department, where cloth, silks, cottons, felt, and leather are being manufactured. Tain (2,381 inhabitants), on the llhone, lies close to the granitic hill which yields the famous " Ermitage," and an acre of which is worth £1,000. St. Vallicr (3,035 inhabitants) and the railway junction of St. Rambert are in the extreme north of the deiDartmcnt. IsEEE, named after its principal river, was formed out of the northern portion of the Dauphine. It is essentially a mountain country, the soil capable of cultiva- tion being confined to its western half, descending in terraces towards the Phone. About half the area of the department consists of cultivated land, one-fifth of heaths and barren rocks, and nearly the same proportion of woods. The breeding of cattle and manufacture of cheese are carried on extensively in its Alpine portion ; there are coal and iron mines, and even gold mines were worked not long since. Industry is increasing, and the paper-mills are the most important of France (produce in 1873, 105,650 cwts.). Alkvard (2,015 inhabitants) is the only town in the interior of the department, and is indebted to its sulphur springs for the position it holds. Orenohle (43,054 inhabitants), at the confluence of the Isere and Drac, occup^'es the centre of a mag- nificent amphitheatre of mountains. It is the focus of much intellectual activity, with colleges, libraries, and museums, and the seat of a considerable industry, the manufacture of gloves alone occupying 20,000 hands in the town and the neighbouring villages. VmUe (3,539 inhabitants), on the Eomanche, has numerous factories, but is better known in connection with the refusal of the delegates of the towns of LIBRARY OF THE UNIVERSITY of tl-UNOIS. IsfeRE. 1-13 Dauphiue, in July, 1788, to pay taxes not voted by rarliaiucut. Botiry-d' Oimns (1,400 iuhubitauts), higher up ou the Romauchc, is tho contro of ouo of tbo finest Alpine districts of France. Tho monastery of tho Grande C/iartrcim; in tho hillf to tho north of Grenoble, is famous throughout tho world for its liqueur. Fig. 107.— Valence. Scale 1 : TS.OOK. 3'l30'E.«r P«ru Pf JtoiunreA- »'iW E.of Or »'l>!> IMUc. At Voiron (7,909 inhabitants), to the north of the elbow of the Isere, as \ Saone are well defined, there are also included in it several outlying districts. The valley of the Saone is essentially a country of transit. In the south it leads to the Rhone, which it joins at Lyons; in the north-west numerous passages through the Cote d'Or connect it with the basin of the Seine ; in the north-cast the gate of Belfort opens commu- nication with the Rhine ; and intercoiu-se with the Loire in the west meets with no obstacles. The climate and vegetation of Northern and Southern France become blended in this valley, and whilst the pine forests in the Jura are quite northern in their aspect, the bleached rocks of Cote d'Or, on the other side of the vallej^ recall the foot-hills of the Cevennes and the Alps. Even the inhabitants, a mixture of Celts, Ligurians, Romans, and Teutonic Burgundians, exhibit the strength and earnestness of men of the north, in combination with the passionate temper of men of the south. The ranges of the Jura belong geologically to the same orographical system as do certain mountain masses of the Dauphino and of Savoy. They at first extend in a northerlj' direction, but by degrees curve round to the north-east, until they pass over into Switzerland. The Jura, very unlike other mountain systems, consists of a series of parallel ranges, rising from a platform sloping down towards the west and north-west. Looked at from an elevation, they resemble a series of parallel waves approaching a coast. Each of these ridges is intersected by one or more transverse gorges, or closes, and there are also combes, or valleys of erosion, at the bottom of which lie sparkling lakes or rivulets. The strata composing the Jura have been folded by exterior pressure, the ridges being formed of anticlinal, the valleys of synclinal folds. Denudation, however, has so much afiected the surface of the country that out of one hundred and sixty ridges there are but thirty the tops of which consist of Jurassic limestone, this having been carried away, exposing the lias and trias which underlie it. The THE JCTEA AND THE BASIN OF THE SAUNE. 110 limestones of the Jura are rich in fossils, and even ancient atolh have been dis- covered. The Jura abounds in forests : that of Chaux, covering nearly 50,000 acres, lies at the foot of the Jura, and consists principally of oaks and beeches. Firs cover the superior slopes ; and in the woods of Ilautc-Joux trunks 100 feet in height and over 3 feet thick abound. Tho moisture of the atmosphere, as well as the calcareous nature of the soil, promotes the growth of grass and herbage, and Fig. 111.— The .Tura. Scale 1 : S45,00O. ♦ " i. of Paris 10 Miles. cattle-breedinw and the makinjj of butter and cheese are carried on with much profit. The cows of the same district always pasture together, and co-operation is practised in the making of cheese. The numerous rivulets of the Jura supply motive power to a host of manufac- tories, besides which the mountaineers engage largely in sedentary industries, such 08 watchmaking. The emancipation of the peasantry during the French Revolution and the con- struction of roads have wonderfully aided the material prosperitj' of the Jura. 150 FEANCE. Not very long ago there existed no carriage roads at all, but at the present daj^ no less than three railroads and twenty carriage roads, some of them masterpieces of engineering, facilitate intercourse between the opposite slopes of the mountains.* Lakes and Rivers. The lakes of the French Jura are much inferior to those of Switzerland, but geologically they are full of interest. A few of them occupy the longitudinal valleys ; others are bounded by the steep walls of the cluses, these being the most picturesque ; others, again, occupy the combes referred to above. Fig. 112. — The Fokest of Chaux. Scale 1 : 320,000. j"|J« K. ol I'ans . 10 JEles. The Ain is the most characteristic river of the Jura. Born of plenteous springs issuing from mysterious caverns, the river winds through narrow defiles and cluses, and frequently disappears between the masses of huge rocks which have tumbled down from the surrounding precipices. Being bounded for the most part by two parallel ridges of the Jura, the Ain receives only a few tributaries, but these, being the effluents of lakes, are more abundant than might be expected. Amongst the tributaries are the emissary of the Lake of Chalin, the Bienne, and the Oignon, rising in the Lake of Nantua. Of the numerous waterfalls of the * Heights in the Jura :— Grande Colomtier, 5,033 feet ; Credo , 5,545 feet ; Reculet, 5,644 feet ; CrSt de la Neige, 5,657 feet; Pass of LaFauoUle, 4,356 feet; Col des Verrieres, 3,084 feet. LAKES OP THE JURA. 161 Ain that near the bridge of Poitte is one of the most considerable. It is 52 feet high, and its tumultuous waters supply the iron forges of La Saisso with motive power. Champagnole is the only town in the narrow valley of the Ain, which only widens out as it approaches tho Rhone, near which the river winds through the fertile and populous district of Valbonne, an ancient lake basin. In most mountain countries the water-shod runs parallel with the mountain ranges. Not so in the Jura, the ridges of which gradually decrease in height as we travel north or south from tho culminating summits on tho frontier between France and Switzerland. In the Jura the line which parts the waters flowing to Fig. 113.— The Lake or St. Point. Scale 1 : 115,7:i|. ^^' '■■yv U: T^/- 1 Mile. the Mediterranean from those wending their way to tlic north runs transversely across the whole system of ridges. Even tho Doubs, which finally finds its way to the Mediterranean, appears to have formerly flowed to the Rhine, and if a barrier were to be placed across the defile of Stc. Ursannc it might possibly do so again. Historically and geologically the Saone is tho main artery of the valley of the Rhone, and if its volume equalled that of the latter, its name would prevail down to the Mediterranean. The Doubs, however, though spoken of as a tribu- tary, is in reality the main branch of the Saone. It flows at first in a north- westerly direction. Having traversed the Lake of St. Point, it enters the narrow gorges of Pontarlier, where mills occupy every available spot. At the small Lako 152 TRANCE. of Chailleson the river reaches the Swiss frontier, which it follows for a consider- able distance. It there gathers itself up, and then leaps over a precipice 89 feet in height, forming the famous Falls of the Doubs. The course of the river Fig. 114. — The Lake of Chalin, Scale 1 : 83,000. p 3Q (ft 'Jl vf. ■Fqatcf u>\> ^ 1 Mile. is most erratic, but at length it turns abruptly to the west, piercing one chain of the Jura after the other. Below St. Ilippolyte the river turns to the north, forcing itself a passage through the mountains of the Lomont, and approaching Fig. 115. — The Lakes op the Cluse of Nai'tua. Scale 1 ; 80,000. E. "1 Gr. ^^r^. //, ■=??° 7— ^^^^77-7-^1^1 |S"40 i;?. -i >J^' 'A •%'"'^- ^^^ ^'1'^^ 1 5-20 -Et"! P. 1 Jlile. the gap of Belfort, through which runs a canal connecting the Doubs with the Rhine. Thenceforth the general course of the river is south-westerly until it joins the Saone, but it winds about much, passing alternately between steep precipices THE SAONE. 158 and over undulating valley plains. The course of the Louo, whicli is tlie principal tributary of the Doubs, is almost equally erratic. At Pontarlier the Doubs in summer was formerly shallowed up in sinks, and flowed uudcrj^round. But the mill-owners, who were much iiieuuvonieuced by this occasional disappearance, have built walls around the mouths of these sink-holes, and the water power furnished by the river is now available throu{>;hout the year. Manv of the tributaries of tlie Saouo likewise flow for considerable distances Fig. UC. — The Lower Valley ok the Am. Scale 1 : ieO,000. ^. ^ lUpovrrsw \,|,i naijs % \.\\\ S jl^l- t- ^.A 1. u — lUUe. underground. Near Yesoul there arc several rivulets of this kind. They reappear again in the spring of Champdamoy, and when the subterranean channels are full to repletion, a supplementary spring, about a mile higher, begins to flow. The Saone rises in the chain of the Faucilles (" sickle mountains "), and ha>'ing received numerous tributaries from the Vosges and the plateau of Langres, it flows 154 FEANCE. in a direction parallel to the hills which produce the famous wines of Burgundy. The canal of Burgundy connects the Saone with the Seine ; that of the Centre with the Loire. The Saone, for 407 miles out of a total of 732, has a fall of only 5'67 inches a mile, and is therefore excellently suited for navigation. Below Chalons it flows through the silted-up basin of an ancient lake, which towards the close of the tertiary epoch extended from the foot of the Jura to the promontories of Charollais and Beaujolais. To the east of the Lower Saone lies the remarkable clayey plateau of the Dombes, abounding in cavities filled with stagnant pools, and surmounted by a few isolated hillocks locally known as poi^Jcs, or paps. Most of these pools are of recent origin, for in the fourteenth centuiy the greater portion of the country was mider cultivation. But feudal wars led to the desertion of entire villages, the Fig. 117- — The Gueat Defile (Percee) of tue Doobs. ScoJe 1 : 3,750,000. W. ,1P V<^^ 4, I » • -J ^ ^ - - '' -• ...--^'— V^"^ U Sc gneie^ e "af>' |r-2o- channels of the rivulets became obstructed, and the stagnant waters occupied every depression in the soil. Subsequently a peculiar system of rotation got into vogue, which consisted in alternately inundating and draining the fields, which neverthe- less yielded but poor harvests, whilst the fevers bred by the numerous swamps annually decimated the population. At length, about a quarter of a century ago, the reclamation of this forsaken part of France was taken in hand. A railway and roads were constructed, and up to 1870 no less than half the swamps, or 25,000 acres, had been drained. The effect upon the health of the inhabitants was almost iumiediate. The population in twenty years has increased 30 per cent., and the mean age is now thii-ty-five years instead of twenty-five as before. The Saone, to the west of the plateau of the Dombes, continues its peaceable course for some distance longer, and the peasants say with unconscious pride — " From Villefranche to Anse — the finest mile ia France." THE SAONE. 166 But soon afterwards the progress of the river is stopped by a raugo of hills. Fig. 118. — The Fails op the Doi-ns. Twisting about to the east, the Saone is swallowed up by the gorge of Roehetaillee, widened, it is suid, by Roman engineers, and finally joins the lUiOno at Lyons, 156 FRANCE. On an average the Saone discharges 8,830 cubic feet every second, the discharge of the Rhone at Lyons amounting to 23,000 cubic feet. The Saone is usually in flood after the autumn and winter rains, whilst the Rhone, fed by the ice and snow of Switzerland and Savoy, carries the greatest volume in summer, a circum- stance most advantageous to the Lyonese. Fig. 119. —The Dombes in 1834. Scale 1 : IGll.OOO. j^g^ E of ( 1 , 2 Miles. Inhabitants. The men of the Jura are the taUest of all France. The pure race of Franche- Comte only exists on the Jui-assic plateau, and is distinguished by a short trunk, broad shoulders, long arms, and long legs. Families are numerous in the villages, and emigration goes on steadily, Comtois being met with in every town of France. Formerly, when Franche- Comte formed a part of the vast domains of AIN. 157 Charles V., no less than 20,000 of them lived at Madrid, and at Rome they occu- pied by themselves the so-called Burgundiun quarter. Powerful, silent, and circumspect, the mountaineers of Franchc-Comte have at all times been distinguished for their industry and tlieir spirit of independence. Until crushed by Louis XIV., who conquered tho country and converted its peasants into serfs, they enjoyed the privileges of self-government, Franchc- Comte only became truly French through the Revolution, but since that time has contributed more than its proper share to tho work achieved by tho entire nation. Topography. Am. — This rectangular department, enclosed between the Rhone and Saone, has been named after the river Ain, which runs through it from north to south. It comprises a level region in the west, and a mountainous tract in the east. Tho former includes the districts of Rrcsso and the Pombes, the latter abounding in small lakes and marshes. The district of Bugey lies on the Fi'ench slopes of the Jura ; that of Gex bej'ond these mountains, to the north of Geneva. Agricidturo, cattle-breeding, and the manufacture of cheese are the leading occupations. Gcx (1,469 inhabitants) is but a small place, but to those who first behold it on descending the Pass of Faucillc it will for ever be identified with the marvellous panorama of the Lake of Geneva. On that same route lies Ferney, associated with Voltaire ; and to the north of it is Nivonne, with its hydropathic establishments. Tracing the narrow valley of the Rhone downwards from the Lake of Geneva, we pass Collonges, the fort of L'Evhise and BcUcgarde (p. 89), and Sci/hscI, known through its asphalt. BeUeij (4,105 inhabitants), the old capital of Bugej', not being either on a river or on a railway, is doomed to dccaj', whilst Amhcricu (1,770 inhabitants), a railwaj' station at the mouth of the valley of the Albarine, St. Raiiihcrt-dc-Jou.r (1,571 inhabitants), and Tenay (2,459 inhabitants), higher up in that valley, are instinct with life. Naniua (2,940 inhabitants) is the only place of importance in northern Bugey, and carries on some trade with the cheese of Valromey and the lithographic stones of the Forest of Montreal. Bourg (14,289 inhabitants), tho old capital of Bresse, is actually the capital of the entire department. The mausoleum of the Dukes of Savoy, budt in the six- teenth century, is its most remarkable building. Bourg is a busy mart for agri- cultural produce. It was the birthplace of Lalande and Edgar Quiuet, and Bichat was bom in a neighbouring village. Pont-de-Vaux (2,910 inhabitants), lower down on the Reyssouze, the river of Bourg, is a small manufacturing town, the inhabitants of which differ essentially from those of the surrounding country, and are believed to be descended from Saracens. Trcroiix (2,217 inhabitants), the old capital of Bresse, had' its own Parliament formerly, as well as a mint, now repre- sented by a few jewellers' shops, and is mentioned in the history of literature as the place where the Jesuits printed their famous Dictionarj' and other works. Sathonay (3,958 inhabitants) is a military camp rather than a village. It was VOL. II. M 158 FRANCE. here tlie battle of Lyons was fought in 197, which gave the dominion of the world to Septimius Severus. Jura. — This portion of the old Franche-Comte is occupied to the extent of one- half by ridges of the Jura, but these are by no means the most elevated in France. It is one of the wealthiest districts of the Jura. More than a third of its area is covered with forests, and it has iron works and other industrial establishments. Fig. 120.— The SIountai.vs of Mouez and St. Ci.attik. Scale 1 : 147,123. f:/i rm' B. Ill ■ J^> 'r.'.^'\^- r-'M^ m W'^ > ^ ^Ajt^S/v^yffiumh •/.■; y 2 lilies. S(. Claude (6,632 inhabitants) is a mountain town at the foot of the Pass of La Faucille, the inhabitants of which depend on wood-carving and lapidary's work for their existence, and export the cheese known as " Septmoncel," from a village in the neighbourhood. The old abbey has disappeared, but on a plateau to the north may stiU. be traced the ruins of a Gallo-Eoman city. Morez (5,375 DOUBS. 1E9 inbabitants), bigbcr up in fbe samo vaHoy, depends solely upon its mauufucturc of ■watches, jewellery, glasses for spectacles, itc. Loiis-le-Saunier (11,2G5 inbabitants), at tho foot of tbo first terrace of tbo Jura, exports the produce of its vineyards and gardens, wood and cheese procured from the mountains, spectacles, articles in copper and iron, and textile fabrics manufac- tured in the town. At Montmorot, close b}-, are brine springs yielding annually nearly 10,000 tons of salt. Excellent building stones are quarried in the vicinity, as also at St. Amour (1,911 inbabitants), half-way to Bourg-en-Bresso. The terrace lying to tho east of tbo clifl's bounding this terrace of tbo Jura abounds in ancient remains. At Orgcht there ai'c bai'rows and stono walls of defence ; on the road thence to St. Claude a Roman bridge spans the Ain, and pile dwellings have been discovered on the small Lake of Clairvmix. Voiteur and Poligixj (4,783 inbabitants) occupy sites analogous to that of Lons-le-Saunier, and Poligny, like its more populous neighbour, has its vineyards, quarries, and brine springs. Arbois (4,809 inhabitants) is noted for its wines, but tho best growths of the department are the white wines of Chateau- Chalons, below Voiteur, and the red ones of tho hills of Arsures, near Mouchard. Sci/iiis (5,577 inhabitants), in a mountain gorge and on the banks of a river, appropriately called La Furieuse, is best known on account of its springs of brine, a portion of whicK is conveyed to the salt works of Arc and Senans, In addition to wine, salt, and cheese, Salins exports iron ore, plaster of Paris, lime, building stones, and timber. At Cliampaynolc (3,342 inhabitants), about 13 miles to the south, there are iron- mills and manufactures of tools. Bole (12,009 inhabitants), on the Doubs, occupies tho extremity of a range of hills, and commands an extensive plain. It was the old capital of Franche-Comt^, the scat of a university and of a Parliament, and valiantly defended its ancient liberties against the armies of Louis XL It is in every respect a more important place than Lons-le-Saunier, possessing not only libraries and museums, but also numerous industrial establishments, including corn and saw mills, machine shops, and manufactories of agricultm-al implcnieuts. On the Upper Doubs, at Runs and Fraisans, there are important iron works. Dorns. — Nearly the whole of this department drains into the Doubs. It is essentially a mountain country, the inbabitants of which depend largely upon watchmaking and other industries for their subsistence. Excellent " Gruyero " is made in the upper valleys. Pontarlier (5,1G3 inhabitants), the highest town on the Doubs, enjoyed its municipal liberties until 1G78. It is mainly indebted for its prosperity to its trade with Switzerland, with which two lines of railway connect it. Near it, on a precipitous rock, stands the fort of Joux, within tho walls of which Toussaint- Louverture, the negro patriot, perished from cold and miser)'. Mortcau, about 20 miles lower down, and near tho famous Falls of the Doubs, is the centre of French watchmaking, and a school has been established there to encourage this important industry. The vicinity of this busy hive abounds in natural curiosities, savage defiles, caverns, and waterfalls. M 2 160 FRANCE. "Where the Doubs emerges from the gorges of the Jura the aspect of the coun- try changes, and we enter upon a region of hills sloping down towards the great gap of Belfort. All along the river, at Ponf-de-Roidc (2,363 inhabitants) and Fig. 121. — The First Terrace of the Jvra, between Lons-le-Satjnier and SALiNa. Scale 1 : 230,000. E iP 3 iO <: y.Or 5 '50 Audincourt (4,258 inhabitants), factory succeeds to factory, until we reach Monthi- liard (7,625 inhabitants), the natural centre of this busy region, where textile manufactures and watchmaking constitute the leading industries, llontbeliard, up to the French Eevolution, belonged to Wiirtemberg, and this circumstance BESANqON. ICl accounts for its large Protestant population. The strong castle has been converted into a prison, but the town, for all that, has lost none of its ancient strategical importance. A monument has been erected to Cuvier, tho most famous of its sous. Near it are ruins of ;i Roman city. Below Montbc'liard tho Doubs enters a second defile, within which is situated the small town of Buume-ks-Bamcs (2,497 inhabitants), thus named after a convent occupied by ladies of noble birth, whoso furo in Lent has passed into a proverb. Besainon (42,808 inhabitants), the largest town in Franchc-Comte, stands on Fig. 122. — BES.VX90N. Scale 1 : Jj.OOO. 3° 4s' EofParis. fonJ'^.'.r..-, L, M,.vj,ll, L/ l5c': \ I'h.ll Ei'hai'J iMilc. one of those sites marked out by nature as a place of strength. A rock 410 feet in height rises boldly from the narrow neck of the peninsula occupied by the town. It is crowned by a citadel, and detached forts placed upon the surrounding hills render Besan^on a formidable fortress even -when attacked by modern artillery. Amongst tho public monuments of the town are a Roman gate, a cathedial, a mansion built by Granvelle, the famous chancellor of Charles V., but now devoted to the objects of the numerous scientific societies of the town. There are colleges, a rich library, a gallery of paintings, and several museums. Tho town has at all 162 FRANCE. times been, jealous of its liberties, and only surrendered to Louis XIV. on his pro- mising to maintain its municipal institutions. Victor Hugo, Charles Fourier, and Proudhon are natives of it. Watchmaking is the great industr}' of Besancon : in 1875 419,984 watches ■were manufactured there, and in the French Jura, and only 2,050 in all the rest of France. But there are also important metallurgical establishments, and iron forges are numerous on the Doubs and its tributary, the Loue. At Miscrc)/, to the north of the town, there are brine springs. Ontans (3,033 inhabitants) on the Loue, is a manufacturing town, and the cherries Fig. 123. — Besancon, as seen fkom La MouiLLtu'E. grown in its orchards are converted into a favourite liqueur. Near it, m the pic- turesque valley of the Lison, are the ruins of the Roman city of Alesia (Alaise), where Ca3sar is believed to have finally overthrown the forces of the Gauls. Belfort. — The gap between the Vosges and the Jura is defended by the fortress of Belfort, which offered so valiant a resistance to the German besiegers. French is spoken iu three out of the four cantons depending upon the town ; Gei-man and French in the fourth, that of Delle. Belfort has lost somewhat of its strategical importance since Metz has become a German fortress, but it still closes one of the great gateways of France. Its citadel was built by Vauban, and other IIATJTE-SACNE. 1C3 fortifications of more recent date crown tlio surrouuding heights. The only remains of mediicval works of defence are the " Citizens' Tower," in the town itself, and the " Stone " of Lu Miotte, on the snniniit of a hill, occupied by one of the luodoru forts. Military rule, as usual, has i)reventcd the growth of industry, and the only manufacturing place of the territory is Giromaijiii/ (3,058 inhabitants), on the Upper Savoureuse, where there are cotton-mills. HAtTE-SAoxE comprises nearly the whole of the upper basin of the JSaoue. From the gi-auitic " Ballons " of the Vosges the department slopes down towards Fig. 124. — Belfout. Scilc i : 10«,C«0. ! lIUcs. the south-west. Nearly one-third of its area is wooded, and the villages are embosomed in orchards. There are no large towns, but though agriculture is the chief pursuit, we meet also with coal, iron, and salt inincs, iron works, potteries, and other industrial establishments. Ilcricoiirl (3,402 inhabitants) is the only town in that portion of the department which lies within the basin of the Doubs. It is mostly inhabited by Protestants engaged in the cotton industry. Lure (3,S00 inhabitants), near the Ognon, the capital of the eastern arrondisse- mont, is a place without importance, surpassed in industry by lioiic/i(imj)s (1,895 164 FRANCE. inhabitants) and Chcunpagney (2,080 inhabitants), occupying a valley of the Vosges, and surrounded by coal mines yielding 200,000 tons annually. Luxeuil (4,047 inhabitants), a famous watering-place, not yielding to Plombieres in the abun- dance of its springs, lies to the north-west, in the midst of a delightful country. Near it is FougeroUcs (1,282 inhabitants), a large village embosomed in cherry gardens. Vesoul (9,097 inhabitants), the capital of the department, lies in the verdant valley of the Durgeon, and being the junction of four railways, is a bustling place, Fif?. 125. — Belfoet, from the Port La BIiotte. though exceeded in that respect by its rival, Graij (7,345 inhabitants), which, in addition to railway communications, possesses the advantage of lying upon a navigable river, the Saone. Gray is a great corn market, and has numerous corn- mills. Cote-d'Or. — The department named after the range of hills producing the famous wines of Burgundy is one of the most important coimtries of passage in France, belonging partly to the basin of the Saone, and partly to those of the Seine and the Loire. The whole of it formerly constituted a portion of the pro- vince known as Burgundy (La Bourgogne), and consists geographically of several cOte-d'ok. 1C5 well-defined didsions. The granitic hills of tlio Morvon, with their woods, ponds, and sparkling rivulets, form one of these. The plateau of the Auxois, farther cast, intersected by numerous deep river valleys, is another. The plateau of Langrcs extends thence in the direction of the Vosges. It, too, is wooded, but the most extensive forests arc met with on the limestone plateau of Chatillounais. Tho most fertile region of tho department lies to the east of the famous raugo known as Cotc-d'Or. The department, in addition to its wines, exports iron and marble. Un the Saone, which flows through the plaiu in the south-west of tho depart- ment, there are no large towns. Aiuoiiiie (4,904 inhabitants), an old fortress, Fig. 126.— Vesovl. Sc-Uo 1 : 60,000. 3'|6t tj" iti t uf Or , Haifa Mile. carries on some trade in agricultural produce; but St. Jean-de-Losne, at the mouth of tho canal of Bourgogne, and Scurre (2,514 inhabitants), lower down, exceed it in activity. Dijon (4.5,G07 inhabitants), the old capital of Burgundy, is most favourably situated for commerce. The canal of Bourgogne connects it with the Saono and the Seine, and it is the principal town on the road between Paris and Lyons. It carries on a considerable trade in corn, possesses a variety of manufactures, and its mustard, gingerbread, and sweetmeats enjoy a wide reputation. Dijon is one of I'oO FEANCE. those provincial towns which have not taken Paris for their pattern. It has produced many men of eminence — St. Bernard, Bossuet, Raraeau, Guy ton de Morveau, JoutTroy, and Rude ; and its scientific establishments, its schools of art and music, its libraries and museums, are amongst the most important of France. The old Fig. 127.— The Wine Distrkt op Cotb-d'Ok. Scale 1 : 320,000. L ^ I i " -J 2° f E of r 10 Miles. raniparts have fallen, but there still remain many fine old churches and mansions, which impart originaUty to the town. The old palace of the Dukes of Burgundy, erected in the fifteenth century, is now used as a town-hall and museum, the guard-chamber containing the tombs of Philip the Bold and John the Fearless, LIBRARV OF THE UNIV£RaTyof«UNOIS. >5 SAOXE-ET-LOIEE. 1G7 and other works of art. In the old Charter-liousc arc preserved the statues of tho prophets, tho work of Claux Sluttcr, u sculptor of tho fourteenth century. The public park was laid out by Le Notre. The famous white slopes of Cote-d'Or begin almost immediately to the south of Dijou. In succession we pass here the hills of Chanibcrtin, Chambolle, and the famous "clos" Vougcot. The best wines are produced on Oxford clay, and they have undoubtedly influenced the temperament of the people who drink them. As Stendhal says, " Logic alone does not suffice to make superior men ; a fiery tem- perament, too, is requisite ; " and that temperament the wines of Burgundy arc supposed to give. Knits (3,003 inhabitants) is the farthest point reached by the Germans during the late war. In the monotonous plain to the east of it stands the old abbej' of Citeaux, upon which formerly depended three thousand convents and monasteries, but which has been converted into an agricultural penitentiary. Beaunc (10,G96 inhabitants), the second town of the department, the seat of a Parliament before Dijon, and long its rival, is an interesting old town, with a hospital built in the fifteenth century by Flemish workmen, and famous, too, on account of its wines, Pommard, Yoluay, Montrachct, and !Meursault (2,550 inha- bitants) being nearr it. Nolai/ (2,355 inhabitants), the birthplace of Caruot, is the last place noted for its wines, for to the west of it hardly any vineyards are met with. ChatiUon-sur-Seine (4,89-1 inhabitants), the principal town of the uortheru arrondissement, was a place of some importance formerly, but its schools exist no longer, and the manufacture of cloth is of verj' little note now. There exist, how- ever, important iron works. One of these, near the village of Ste. Colombe, is surmounted bj' Mont Lassois, upon which Gerard of Eoussillou, one of the heroes ol romance, built himself a castle. Commercially the valley of the Oze is far more important than that of the Upper Seine, for the railway from Paris to Dijou runs along it, passing Mont Auxois, upon the slope of which stands the village of Alise Ste. Peine, which has been identified with A/esia, where Vercingetorix oflercd his final resistance to the legions of CaDsar. A colossal statue of the Gallic chief has been erected hero, although the learned are by no means agreed as to the site of ancient Alesia. In a side vallej' close by, near the village of Bmisij-k-GramJ, there is a famous castle. Soon after the Brenne and the canal of Bourgognc join from the south. At Jloxfl/ard (2,427 inhabitants) the mansion in which Buffon was born is pointed out. Below Mont- bard the Brenne joins the Arman9on, and proceeding up the valley of the latter, we reach SeiiiKr (4,022 inhabitants), a curious old town, with a castle perched upon a rock of granite, and an ancient Gothic church. Studicu (3,113 inhabitants), the ancient Sidolocus, farther south, lies upon the granitic plateau of Morvan. It exports timber, cattle, and wine casks. S.\6xE-Er-LoiRE. — This department lies partly between the two navigable rivers after which it has been named. The plain to the east of the Saone is a contiimation of that of La Brcsse, and ascends gently towards the foot of the Jura. A more varied country lies to the west of the Saone, being boui^ded by the hills of 168 FRANCE. Autunais and CharoUais, whicli form the water- shed between, the Atlantic and the Mediterranean. The wooded mountains of Morvan rise to the west of Autun, and the valleys of Brionnais, sloping down to the Loire, are occupied b}^ magnificent meadows. The department ranks high as an agricultural country, and the coal mines around Autun have led to the creation of flourishing manufactures. Louhans (3,498 inhabitants) is the only town to the east of the Saone, the great centres of population having sprung into existence on the banks of that navigable river. Chalons-tiur-Saone (20,571 inhabitants) is the most important Fig. 128.— Le Crevsot. Scale 1 : 23,000. 2° 1 6' K. of Paris 1."TJ6'F. of (n- nalf-illile. town of the entire department historically, and only cedes in population to the modern upstart, Le Creusot. Formerly a great river port, and a station of a Roman admiral, it is now a most important railway centre, and exports corn, iron, and wines. There are ship-yards, and barrels in large numbers arc made. Chagny (3,950 inhabitants), on the Canal du Centre, which joins it to Chalons, has recently developed into a busy place of traffic. Travelling down the Saone, we pass Tournus (4,412 inhabitants), the birthplace of Greuze, and reach Macon (16,579 inhabitants), the capital of the department. In the upper town, formerly inhabited by priests and nobles, Lamartine was born. LE CREUSOT. 1G9 In the lower town tlicre are manufactories and huge wine vaults, in which the famous growths of TJiorins and Romaneche aro stored. St. Laurent, a suburb on the other side of the river, is famous on account of its fairs. The country around Macon abounds in places of interest. Archnoologists will seek out the village of Solurre, where the fossil skeletons of a hundred thousand horses have been discovered. The castles of Montceau-les-Mines (4,375 inhabitants), Milhj, and Si. Point allure the admirers of Lamar tine's poetry, whilst the famous abbey of Chinij (4,007 inhabitants) must ever attract historians and artists. Autini (I1,3-jS inhabitants), in the north-western angle of the department, the Augustodunum of the Romans, has fallen from its high estate, and its buildings now hardly cover two-thirds of the area enclosed by its ancient walls. Its Roman ruins are of small importance, some of the most interesting amongst Ihem haA-ing been utilised in the construction of modern buildings. The 3Iiddle Ages are represented by the fine church of St. Lazarus, with one of the best pictures of Fig. 129.— Le CracsoT. Ingres. Mont Beurray (2,GG0 feet), one of the highest summits of the Morvan, rises about 12 miles to the west of Autun. Upon its summit may be seen the remains of an ancient city, identified with the Bibracte of the Romans, but evidently of much older date, as is proved by cromlechs and entrenchments. Annually in May a fair is held on the summit of this raoimtain. The country to the west of Autun is purely agricultural, but to the cast of that town lies one of the great manufacturing centres of France. At Epinac (1,G70 inhabitants) there are coal mines, yielding annually about 150,000 tons, and bottle works. Couchcs-les-Miiies (1,597 inhabitants) produces iron, lime, and gypsum ; but the great centre of industry lies still farther south, near the old Charbonniere. This is Le Creimt (26,432 inhabitants). A cannon foundry, glass works, and iron works existed there at the close of last century, but it is only since 1837 that the place has rapidly grown into importance. Its coal mines now extend to a depth of 1,300 feet, and their produce is utilised in innumerable iron 170 FEANCE. Avorks, forges, and locomotive workshops, a considerable portion of the iron ore and coal consumed being imported from abroad. Other places to the south of Le Creusot participate in its industrial prosperity. Montchanin-Ics-Mincs (3,-33-l inhabitants) has vast brick-kilns. Blanzy (1,88G inhabitants) has the most productive coal mines of the district. Montceau (4,375 inhabitants) has iron mines. Charollcs (2,969 inhabitants), a sleepy town, is the capital of Charollais. Tliat district, as well as Brionnais, adjoining it on the south-west, is engaged in the Fig. 130.— Lyon'S. SVile 1 : 80,000. 4°Uo F. of Gr . 1 Mile. fattening of cattle. Cliauffailles (1,993 inhabitants), in that part of the country, is becoming of importance on account of its coal mines. Digoin (2,721 inhabitants), on the Loire, carries on a considerable commerce. Bourhon-Lancij (1,604 inhabit- ants) has been noted from immemorial times for its saline springs. Paraii-le-Monial (2,895 inhabitants) has an abbey modelled after that of Cluny, and has recently become known through the visions of Marie Alacoque, which led to the " worship of the Sacred Heart." * * In 1874 the department produced 1,110,000 tons of coal. Le Creusot, in 1872, employed 15,500 persons, and produced 330,000 tons of iron and steel, 308 locomotives, &c., valued at £620,000. LIBRARV OF THE UNIVERS/TYofftUNOIS, i' 1 I I LYONS. 371 Ehoxe. — Tills department includes the slopes of the hills of Lyonnais and Beaujolais (3,320 feet), and is bounded by the rivers Saone and Rhone on the cast. It is one of the smallest departments of France, but owing to its industry, the great centre of which is Lyons, one of the wealthiest. Li/oiis, or Lyon, as it is called by the French (322,G12 inhabitants), occupies a most favourable position at the confluence of the Saone and Rhone, and is marked out as a natural intermediary between north and south. The surrounding heights oflTer excellent sites for forts. The great advantages of Lyons have been recognised from the earliest times. L. Munatius Plancus planted a Roman colony upon the height overlooking the confluence of the two rivers ; and Lugdioicnnis is spoken of by Strabo as the " heart of Gaul." It remains to this day the primatial city of all France, and the wealthiest societ}' for propagating the Catholic faith has its seat there. The force of tradition still exhibits itself in the veneration with which the Lyonesc regard the hill of Fourvieres and its old church, built upon the site of the old Forum [Fore tieux) of the Romans. Another church, that of Ainay in the lower town, is partlj- constructed from the materials of the temple which sixty tribes of Gaul constructed in honour of Augustus. The lowest quarter of the existing city, that of Perrache, only dates from the last century, and bears the name of the engineer -who converted its site into dry land. It suffers more from floods than any other part of the town, and the fogs are densest there. In it are situated tho arsenal, a huge goods station, gas works, and the docks for vessels navigating the Saone. Every one of the other quarters of the town has a distinctive character. The centre of the town, around Place Bellecour, is the seat of wealth and luxury. The business quarter lies at the foot of the hill of La Croix-Rousse, itself occupied by the dwellings of the workmen. Brotteaux, to the east of the Rhone, is inhabited by clerks and tradesmen, and adjoins the beautiful park of Tete-d'Or. La Guillotiere, to the south of it, is a workmen's quarter. Vaise, beyond the Rhone, abounds in manufactories. Suburbs extend in all directions. The traces still existing of the dominion of the Romans are limited to the remains of three aqueducts, baths, amphitheatres, and other structui'es. The Palace of Arts, one of the most sumptuous buildings of modern Lyons, aboimds not onlj' in Roman antiquities, but contains likewise a valuable collection of paintings, a library of 70,000 volumes, and a natural history collec- tion. The busts of celebrated men born in the town, including those of Ampere, Bernard de Jussieu, Flandrin, Delorme, and others, have been placed within it. The Exchange and Merchants' Hall contains an industrial museum modelled upon that of South Kensington. Public monuments abound. Science is represented by colleges and schools, by a public library of 180,000 volumes, and by numerous societies, including one of agriculture, which possesses a model farm on the heights of Ecully. Lyons is one of the great industrial centres of the world. There are machine shops, chemical works, and manufactories of paper-hangings ; but the town is most famous for its silks. The latter industry was introduced by Italians, whom Louis XL encouraged to settle in the town. The revocation of the Edict of 172 FEAKCE. Naates threatened destruction to this industry, but it survived the blow then inflicted, and, in spite of wars and revolutions, Lyons has maintained its pre- eminent position. In 1872 there were 120,000 looms in the department, 240,000 persons were employed in the silk industry, and the average value of silk stuffs produced annually is estimated at nearly £20,000,000 sterling. Most of the weavers work at their own homes, and their demeanour and character differ very favourably from those of ordinary factory hands. At the same time the solitary Fig. 131. — The Envikons of Lyon'S. Seal e oiiu^ooo , 10 Miles. life which most of them lead nourishes a spirit of mystical exaltation which rises to the surface whenever there is a revolution. Formerly nearly all the weavers lived in the town, but the manufacturers, desirous of weakening their unions and of obtaining cheaper labour, have trans- planted the silk industry to most of the neighbouring towns and villages. Villcur- hanne (8,163 inhabitants), Venissiciix (1,943 inhabitants), Ste. Foy (4,337 inha- bitants), Oullins (4,886 inhabitants), St. Genis (2,246 inhabitants), Caluire et Cuire (7,207 inhabitants), and Neuville (3,207 inhabitants) are inhabited to a large LYONS. 178 extent by weavers. Nay, the great industry of Lyons extends far beyond the limits of the department, for the looms of Chamb^ry, in Savoy, work on account of Lyonese houses. L'Arhreslc (3,091 inhabitants), to the west of the liills of Lyons, has quarries, lime works, and, at St. Bel, almost inexhaustible deposits of pyrites, which supplj' nearly all France with the material required for the manufacture of sulphur and sulphuric acid. The village of C/icssi/-/es-Mi)ics, close by, was formerly important on account of its copper mines. Tararc (13,563 inhabitants), on the railway to Roanne, enjoys a high reputation for its muslins and embroidery, its plush and velvets. Aniplfjmis (4,047 inhabitants), Tliizij (3,170 inhabitants), and Coiira (3,897 inhabitants), near it, are likewise manufacturing places. Beaujeu (3,043 inhabitants), which gives its name to the district of Beaujolais, ViJlffranche (11,994 inhabitants), and Belleville (2,691 inhabitants), have some manufactures, but agricultural pursuits predominate in that portion of the depart- ment. The wines of Beaujolais enjoy a high reputation, the most famous growths being produced on porphyritic granite. Giiors (10,856 inhabitants), on the Rhone, to the south of Lyons, is a dependency of St. Etienne rather than of the city just named. Its iron works, glass works, and brick-kilns are supplied with fuel from the neighbouring coal mines. The famous wine known as Cote-Rotie grows on the slopes of sunburnt Mont Pila, close by. vor.. 11 w CHAPTER V. THE PLiTEAU OF CENTRAL FRANCE. G£vAUDAN, Velay, Auvergne, Roueroue, Limousin, Peihgoud, Marche, Bourbonnais.* The Ceatinnes. 51 HE granitic protuberance in the centre of France, wtence the rivers radiate towards the Atlantic and the Mediterranean, has not inaptly been called a " pole of divergence," from which the people emigrate in all directions, and more especially towards the basin of the Seine, within which lies the "pole of attraction." The plateau under consideration covers an area of 31,000 square milesi and interposes a barrier 190 miles in length between the north and south of France. Its heights had to be scaled before the people dwelling on its opposite slopes became one, and although this national fusion was not accomplished without wars and bloodshed, it led in the end to the common enjoyment of the blessings of civilisation. The plateau, as a whole, slopes down gently towards the north-west, and is boimded in the south and east by steep mountains. The Cevennes constitute the most important portion of the semicircular chain of mountains which envelop the plateau on the south-east, and form the water- shed between the Mediterranean and the Atlantic. They begin with the Montagne Noir (" black mountain," 3,970 feet), to the east of the gap of Revel, through which runs the railway connecting Castel- naudary with Castres. The valley of the Thore, tributary to the Tarn, separates these Black Mountains from the moimtain rampart of Espinouze (4,198 feet), rising almost precipitously above the valleys of the Jaur and Orb, but sloping down gently towards the north-west. In the east this portion of the Cevennes terminates in a savage mountain mass, where granites and sedimentary strata intermingle in strange confusion, and which has been pierced in several places by volcanic eruptions. It almost apjsears as if a subterranean lake of lava extended in former times from the dome-shaped mountain of Auvergnc to the shore of the Mediterranean ; that is, along a line where the contrasts between north and south are most striking. On one slope of the mountains we have rivulets, meadows, and * Poulett vScropc, "Volcanoes of Central France;" Eames, "Geogenie du Cantal;" A. Jullien, "Des Phenom^nes Glaciaire dans le Plateau Central de la France ; " Burat. " Geologie de la France." THE CfiVEXNES. 175 forests ; on flic other, stony torrent beds, odoriferous herbs, and rare trees. Tlio contrast between the inhabitants is equally great, and the dweller in tho plain, proud of his ancient civilisation, looks with disdain upon tho Gavacho inhabiting the plateau, though tho latter does not yield to him in industry. In the cast of the Orb the Garrigues — thus named from tho kcrmes oaks, or ffarnis, which cover their slopes — form tho southern edge of a scries of lime- stone plateaux known as causses, from the Latin caU, lime. The most southern of these is that of Larzac (2,9S0 feet), but tho most typical is the Cuussc of ^Mejeau (4,200 feet), a huge mass of limestone 100,000 acres in extent, and bounded on all sides by steep precipices. There can bo no doubt that these causses were formerly continuous, though separated now by deep cailons, which excite the Fig. 132.— The Mountaixs op Espinouzb. Scale 1 : 240,000. Jo? 30' E. ol Paris :?5o-E. ofGr. Miles. admiration of geologists. No running streams are met witli on these limestone "tables," the rain disappearing almost immediately beneath tho surface. The inhabitants carefully collect tho rain-water in cisterns ; and in summer, when the supply fails them, they are obliged to descend into the canons in search of it. Springs of sparkling water abound there ; and the shrubs and trees which flourish near them contrast most strikingly with the barren rocks around. The causses are covered with herbage, and the inhabitants, very few in number, confine them- selves to the cultivation of oats, barley, and potatoes. The herbage, however, scanty as it is, supports thousands of sheep, which furnish excellent wool, and from whoso milk is manufactured the famous cheese known as Eoqiicfort. In winter, when these plateaux are covered with snow to the depth of several tvct, and N 2 176 FRANCE. most of the inhabitants have deserted them, it is sometimes dangerous to cross them. Dohnens abound on these limestone plateaux, whilst scarcely any are met with in the crystalline region which adjoins them. It has been concluded from this circumstance that the ancient inhabitants of the plateau differed in origiu and religion from their neighbours. Even at the present day the dwellers on the limestone plateau of the Lozere differ in many respects from the men inhabiting the district of granitic hills which slopes down westward in the direction of the Aveyron, and cidminate in the Levezou (3,785 feet). On the one hand we have sweet herbage, a little barley, and oats ; on the other the granitic slopes are covered Fig. 133. — The Causse or Mejean. Scale 1 : 315,000. l'?E.ofP. 3»20'E.ofCc; 5 Miles. •with shrub, and rye-fields, or s4galas, extend along their foot. The peasant of the Gausses, or Caussenard, who eats bread made of barley or oats, and drinks clear water, is tall and bony, and far stronger than his neighbour of the granitic district, who lives upon rye and chestnuts, and drinks cider. To the east of these Jurassic limestone plateaux lies the principal mass of the Cevennes, surmounted by the Esperon (4,658 feet) and the superb granite dome of Aigoual (5,141 feet). This is one of the wildest districts of France; but the bears, stags, and wild boars which formerly inhabited its forests have disappeared, and there now remain only wolves. A rugged granite region, anciently known as Gevaudan, occupies the south- eastern corner of the department of Lozere, and expands farther north into a L13RARY OF THE •JNIVERSITY of ILLINOIS. THE VOLCANOES Ai'BtrssoA^^ m yy c^' ^" v* I i '■■■J' / ji ,^B^ cs Wf^^i. •?■ ' ''^■^j^.S'f^^'^^ "a^ 'kill «/a<)j CENTRAL FRANCE Trias Clmlk Tertiatrv I 1 /\lhl\-i»riii E i C" LIMITED. MEZENC AND VIVAEjVIS. I77 dome-shaped mass of granite 116 square miles in extent, and attaining in Mont Finieils a height of 5,638 feet. The limestone, which to all appearance formerly covered this plateau, has been removed by denudation. Even the crystalline rock has been subjected to erosive action. "We meet with huge blocks of >Trauite, and every cavity is tilled up with shingle or coarse gravel. There are few vilk'^-es, and their inhabitants are very poor. Whilst the south-eastern portion of Lozere is diversified by mountains, that part of the department which lies to the north of the Lot is one of the most desolate regions of all France, consisting of barren plateaux traversed by a few sparsely wooded granitic ridges, such as the hUls of the Goulct (4,918 feet), the forest of Mercoirc {4,92^ feet), the mountains of La Margeride (5,098 feet), and the region derisively called " King's Palace " (■1,'212 feet). Mezenc and Vivarais. TiiE volcanic region of Mont Mezenc and Coiron, to the east of this granitic plateau, separates the southern Cevenucs from the northern prolongation of that mountain chain, terminating in the pyramid of Mont Pila (4,703 feet), from the summit of which the view extends across the Rhone valley to the snowy heights of Mont Blanc. The diversified eastern slopes of the Cevennes, with their mulberry plantations, vineyards, and chestnut forests, contrast most strikingly with the elongated slopes stretching towards the north and west. The first volcanic cones are met with immcdiatelj' to the north of Mont Tanargue (4,785 feet), a buttress of the plateau of Vivarais. The southernmost of these extinct volcanoes is that of Jaujac, the slopes of which are for the most part covered with chestnut trees, which here, as in Italy, flourish most on disintegrated basalt. Streams of lava extend from the old " cup," or cratei*, northwards into the valley of the Lignon, which flows between cHfis of basalt and granite. Lower down on that river, where it joins the Ardeche, rises the " Gravenue " of Souillols. The village of Thueyts, higher up in the valley of the Ai'deche, stands upon a stream of lava terminating in a magnificent range of basalt 100 feet in height. Close by rises the regular cone of the Gravenne of Montpezat, surroimded with fields of lava, tlirough which the Ardeche and its tributaries have cut themselves a passage. The crater, or cup, of Aizac (2,126 feet), which rises in solitary grandeur in the valley of the Volane, is better known than any other of tho volcanoes of Lower Vivarais, o\ving to its proximity to the cold mineral springs of Vals. Spiings discharging mephitic gases have been discovered farther west. But these six old volcanoes hing at the foot of the granitic plateau of Vivarais are very insignificant in comparison with the volcanic mountain range which forms the water-shed between Rhone and Loire, and in the centre of which rise the three " teeth " of Mont Mezenc (5,755 feet), surrounded by subsidiary cones, amongst which the Gcrbier de Jones (5,124 feet) is remarkable as giving birth to the river Loire. The phonoUthic lava of Mont Mezenc must have burst forth in a high 178 FRANCE. state of fusion, for it spread rapidly over the granitic plateau, and tte height of the volcanic cones here is less than that of the Cantal and Mont Dore, although the latter rest upon a much lower basis. Mr. Poulett Scrope even thinks that the lava currents extended as far north as the phonolithic cones of Meygal (4,717 feet). These lava beds would thus oversijread an area of 154 square miles, their average thickness being 390 feet. They arc now for the most part clothed with forests of Fig. 134. — The Defile of the Ardeche, near Euoms. oak and firs. Other streams of lava flowed towards the east, covering the granitic hills of Coiron (3,380 feet), and even descending into the valley of the Rhone. This latter, since the last eruption of lava, has been scooped out to a depth of nearly 1,000 feet, whilst the hills of Coiron, protected by their cap of lava, offered a greater resistance to the destructive action of geological agencies ; but they, too, are gradually being destroyed, and huge blocks of basalt sometimes slide down into the valleys, the castle of Rochemaure being built upon one VELAY. 179 of them. These hills are remarkable, moreover, on account of their promon- tories formed of columnar basalt, and resembling the castles of an ancient race of giants, Velay. Tiiii deep valley of erosion scooped out by the Loire separates the volcanoes of Mdzenc from the volcanic plateau of Velay, covered with basaltic lavas vomited from at least a hundred and fifty craters, most of which can scarcely be distin- guished now. Streams of luva have frequently blocked up the valley of the Fig. 135. — Tiir. Kills of Comoif. Scale 1 : HW.W. b ilUc-B. Loire and of the Allicr, but these rivers have scooped themselves out new channels, frequently laying bare magnificent columns of basalt. One of the grandest of these defiles is that of the Loire at Chamalieres, excavated in granite and basaltic lava to a depth of 980 feet. The volcanic formations in the vicinity of Le Puy (O.OIO foet) are bettor known than any others in this region. They include columnar basalt, sheets of lava, and dykes. Close to the black houses of the town the " Needle " of St. Michel, an obelisk of lava, and the rock of Corneille (2,484 feet), raise their heads. Beyond the dismantled walls of Polignac, in the north-west, we reach the columns of basalt of La Dcnise, known as the '• Cross of Straw " and the " Organ " of Espaly. It was here M. Aymard 180 PEANCE. discovered the fossil remains of animals whicli roamed over this region when the surrounding volcanoes were yet in a state of eruption. Two human skeletons have likewise been discovered, dating back, in all probability, to the same epoch. The flora of the country does not appear to have changed since then. Fine garnets and sapphires abound in the basalt of EsjJaly. Around Le Puy every available sj)ot is covered with vegetation, but the plateau which extends thence to the south is of grievous uniformity. It consists of a wide Fig. 136.— Le Puy. Scale 1 ; Uu.OOO. plain covered with turf or stunted trees, over which are scattered the black cones of extinct volcanoes, the largest amongst which, that of the wood of L'Hopital (4,663 feet), rises but little above the general surface. A cavity pro- duced by the escape of a prodigious bubble of gas is occupied by the Lake of Bouchet (3,926 feet). The Lake of Limagne, farther north, is supposed to have originated in the same manner ; but the old Lake of Bar (3,828 feet), now drained and converted into a beech wood, occupied the crater of an extinct volcano. THE VOLCANOES OF AITVEEGNE. 181 The Volcanoes of Auvergne. A THIRD volcanic region, that of Auvergne, lies to the east of the deep vullcy of the Allier and of the granitic spur of Margcride. The volcanic nature of this region has at tdl times been kuown to the peajuuts liviug there, and many of the mountains are called by them Peyre Arse ; that is, " burnt mountain ; " but Guettard, in 1751, was the first who revealed the existence of these French volcanoes to the world of science. The southermost volcanic group of the Auvergne occupies the granitic plateau of Aubrac (4,825 feet), rising steeply above the valley of the Lot, and covered for the mo^t part with pasture grounds, which support in summer about 30,000 cows and 40,000 sheep. Dolmens, locally known as " fairy bowers " or " magicians' castles," are scattered over the plateau, but the only human dwellings met with are the clusters of burons inhabited by cheese-makers. The people of this remote part of France have preserved their ancient manners, and even something of their ancient religion. On the second Sunday of July, as in the time of Gregory of Tours, they walk in procession to the Lake of St. Andeol, bathe in its turfy waters, and throw into it the clothes of the sick and propitiatory offerings. The extinct volcanoes of Aubrac possess no special features, but to the north of them rise the hot springs of Chaudes- Aigues, yielding a supply of water amply sufficing for all domestic purposes as well as for heating most of the houses in winter. The principal of these springs has a temperature of nearly 180^ F., and the soil in the neighbourhood is so warm that in spite of the elevation of the town (2,130 feet), snow never remains on the ground. Crossing the valley of the Truyere, we reach the most considerable volcanic group of France, that of Mont Cantal, which can faiiiy compare with Mount Etna and other great volcanoes. The various summits of the Cantal form collectively an isolated cone 95 miles in circumference, and resting upon a base of granite. Up to the tertiary epoch the centre of this granitic base was occupied in part by huge fresh-water lakes. The first eruptions took place in the miocene age, the last and most terrible of all during the quaternary period. The lava then ejected enveloped all the cones which existed at that time ; it over- whelmed the forests, converting them into a thin layer of coal, and HUed up the valleys to a depth of nearly 400 feet. The old volcano probably rose to a height of 8,200 feet, but there remain now only the shattered and worn fragments of its semicircular ridge, the most elevated points of which are the Plomb du Cantal (6,025 feet), the Puy Mary (5,863 feet), and the Puy Cha- varoche (5,722 feet). Valleys, scooped out by ancient glaciers, some of which had a length of nearly 20 miles, and by torrents, radiate in all directions from the central heights. Those of Cere and Alagnon are connected near their summits by the two tunnels of Lioran, which pierce the mountain at a height of 3,870 and 3,800 feet respectively, and are traversed by a road and a rail- way. Those deep valleys lay open the geological structure of the mountain, and exhibit beds of gravel, carboniferous sandstones, and granite, subsequently 182 FEANCE. covered by currents of basaltic lava. The slopes of the Plomb du Cantal, and especially those exjjosed to the moist westerly winds, are covered with forests of beeches and firs. In the east the forests are confined to the valley bottoms. The currents of lava there form a monotonous treeless plateau known as Planeze, and terminating in promontories of columnar basalt, upon one of which is perched the old capital of Upper Auvergne, St. Flour (2,903 feet). The Alagnou separates Fig 137. — The Puy de L'AicriLLiEn, Mont Dore. the Planeze from another basaltic plateau to the north of it, which terminates likewise in curious columnar formations. The basaltic plateaux of CezaUier, stretching from the Dordogne to the Allier in the east, separate the Mont du Cantal from the most ancient and conspicuous volcanic mass of Auvergne, that of Mont Dore. Though covering a smaller area than its neighbour of Cantal, it is here that the highest moimtain of Central France, the Puy de Sancy (6,180 feet), raises its head, surrounded by other peaks hardly inferior to it in altitude, such as the Puy Ferrant, the Puy de TAiguillier (5,076 THE VOLCANOES OF AUVERGNE. 183 feet), and the Cacadogiic. No regular crater can now be traced, but one probably existed in the vicinity of Mont Doie (3,a30 feet), a trachytic cone, near wliich the Dordogno and the Couzo of Chumbon take their rise. The bods of lava descend from this mountain, often in uninterrupted sheets, until tlicy reach and spread themselves round its base. At a later period Mont Dore had its cap of ice, and glaciers descended from it to a distance of 25 miles. AVhcn the great central volcano of Mont Doro became extinct, other vents Fig. 13S. — The Ply of yANcv axd the Lake Distuict. Scale- 1 : 80,000. Ilich.' '■^r I ^' ^itcvt^i/l*e^ \ Milr. opened in its vicinity, and amongst these Mont Tartaret (3,156 feet) discharged its lavas, now covered with beeches and pines, right across the valley of the Couze, and, by drawing up the waters of that river, led to the formation of the Lake of Chambon ('2,887. feet), the most delightful sheet of water in Auvergne, surrounded by meadows and trees, and having several small wooded islands. 184 FEANCE. Fig. 139. — The Chain of tub Pcy de Dome. Scale 1 : 100,000. |S;^ :m #• ( /rr/noM cf ;?'^:- The plateau to the north of Mont Dore is covered with volcanic cones of comparatively recent origin. Two of these, the Montsineyre (4,372 feet) and the Montchal (4,628 feet), are mirrored in smaU lakes, the one formed by the damming up of a rivulet, the other occupying an old crater. Amongst the many other lakes which fill depressions of this plateau, that of Pavin (3,925 feet) is dis- tinguished by its aspect of solemn grandeur. The inhabitants formerly dreaded it as the seat of evil spirits, but having been stocked with trout, it has lost its terrors. Its depth is 308 feet, and it is fed by sub- terranean streams. Thermal and mineral springs abound in this region, those of Mont Dore and of La Bourboule, near the source of the Dordogne, being the most frequented. The springs of St. Nectaire are the best known of those on the eastern slope, their water resembling that of Ems. Altogether there are no less than 200 springs, carbonate of soda asso- ciated with chloride of sodium predominat- ing in the hot springs, whilst the cold ones are almost without exception charged A^'ith carbonic acid. A chain of volcanic ptii/s rising from the granitic plateau bounded by the valleys of the Allier and Sioule forms the termina- tion of the volcanic region of Central France towards the north. Some of these puys are dome-shaped, others have the appear- ance of truncated cones ; and craters and old lava currents, or cheircs, can still be distinguished. The Puy de Dome (4,805 feet), a dome-shaped mass of trachyte, is not onl}^ the highest summit of the whole range, but, on account of its regular shape and commanding aspect, is the most, famous. A temple dedicated to Mercury formerly stood upon its summit, and a physical observatory has recently been erected there. Immediately to the north of it lies the crater of the Little Puy de Dome, locally known as the "Hen's Nest." The Puy de Come (4,116 feet), near Clermont, has two distinct craters on its summits, from which broad streams of lava have poured down into the valley of the Sioule, filling the ancient river channel for the distance of more than a mile. The Sioule, thus dispossessed of its bed, has worked out a fresh one between the lava and the granite of its western bank. Its ■ 4 Miles. THE TOLCANOES OF AUVEEGNE. 185 neighbour, the Puy de Pariou, is remarkable on account of the sharpness of the brim of its crater. Farther north lies the dome-shaped Sarcouy, the clinkstone of which is used in the manufacture of filters and glass. But the most curious volcano of that region is the Puy Chopinc, a dome rising from a crater formed of scoritD, and consisting of granite placed " like the ham of a sandwich " between layers of basalt and trachyte. The range terminates in the north with two great volcanoes, the Puys of Louchadiere and Xugere, from both of which immense sheets of lava extend to the east or west. At Volvic there are vast quarries, from which the towns in the neighbourhood procure most of their building stones. Most of the cones to the south of the Puy de Dome have craters on their summits. The combined lava streams of the Puys of Lassola, de la "N'ache, and Yichatel have dammed up the valley of the Yeyre, forming the Lake of Aydat (2,710 feet), upon the borders of which stood Avitacum, the residence of Sidonius Apollinaris. Amongst old volcanoes forther south are the Gravenoir Fig. 140.— Volvic. Scale 1 : 70,000. . 1 MUo. (" black gravel "), thus called from the colour of its ash, and the Tazanat, the crater of which is occupied by a lake. Near Aigueperse there is a "poison spring" discharging carbonic acid. Numerous traces of volcanic activity are met with between the eastern slope of this range and the plain of the Allier ; amongst others, the famous basaltic plateau of Gergovia (2,440 feet), the ancient capital of the country, defended by Vercingetorix against the legions of Julius Cnesar. The integrity of many cones of the Auvergne is due, according to Sir Charles Lyell, to the loose porous nature of the soil, which instantly ab.sorbs all moisture, and thus prevents the formation of rills. The water thus absorbed is discharged lower down as bounteous springs, some of which are valued for their medicinal properties, whilst others cover the rocky surfaces over which they flow with a coating of calc-taff, and incrustate all objects exposed to their action. The most famous of these is that of St. Allyro at Clermont, which has built itself an aqueduct 250 feet in length, terminating in a superb arch thrown across the rivulet of Tire- 186 FEANCE. taine. Lecoq and otter geologists trace the existence of limestones and gypsum in Auvergne to the action of this and other calcareous springs. They have con- tributed, too, towards the formation of the fertile plain of the Allier kno-wn as Limagnc. This plain, during the miocene age, was a vast fresh-water lake, but long before the volcanoes surrounding- it had ceased their activity this lake had been drained. The calcareous and other springs then deposited lime, silica, and gypsum, but it is to a layer of volcanic ashes that Limagne is indebted for its marvellous fecundity. Amongst the mineral productions of the Auvergne are argentiferous lead, which is most abundant on the western slope of Mont Dome, and coal, the car- boniferous strata extending along the western foot of the volcanoes, from Mauriac to Moulins and Montlucon, being bedded with surprising regularity. Fig. 1-11. — TuE Meandertngs op the Lot. Sciile 1 : 2.;o,OJO.. [VO'-'" \ in.. ibJ^i . 6 Miles. LiMorsiN. The granitic platform of Auvergne penetrates like a blunt wedge between the Jurassic and tertiary rocks in the west, and forms a series of sterile plateaux or terraces, the most elevated of which is that of Mille Vaches (" thousand cows," 3,228 feet), in which the Vienne, the Yezere, and the northern tributaries of the Dordogne take their rise. The. I'ange of hills which thence extends to the west is even less elevated. These hills and plateaux have for the most part been robbed of their forests, and their sole covering consists of shrubs and heather, but the valleys which pierce them are often delightfully beautiful and of great fertility. Potter's earth abounds, and has given rise to much industry ; metallic veins traverse the granite ; and beds of coal are met with occasionally along a line UBRARY OF THE UNWERSlTY-fH-UNOlS. LIMOUSIN. 1«7 separaliug iho crystullinc rocks from the scclimcnfnty ones. The western prolonga- tion of the plateau consists almost exclusively of Jurassic limestones and chalk. The limestone region lying between Figeac, Cahors, and ^Fontauban resembles in every respect the causses of Avoyron (page 175), though, owing to its smaller elevation, it enjoys a milder climate. The hilly district farther north, traversed by the Dordogne and its tributaries, is very different in aspect. The sinuous course of the rivers traversing these secondary strata clearly marks out the difference between them and the granite. The Lot, flowing in a deep ravine fixcavated in Jurassic limestone, abruptly twists to the right and left, whilst Fig. 142. — The Kapids op Lamxbe. Scale 1 : 150,000. ^, W nf Pi. i>o Eof Cr "llUes. the Dordogne and other rivers, taking their course between gentle hills, wind about them in a more placid fashion. Of all the rivers rising in Central France the Dordogne is the one which for the greatest part of its course belongs to the plateaux, differing in that respect essentially from the Loire and the Allicr, which even in their upper course traverse ancient lake basins. The Dordogne, on the other hand, is confined within a narrow ravine until it debouches upon the lowlands of Aquitaine. At Bretenoux it escapes from the region of granite, and then winds about amongst limestone hills, its bed being frequently obstructed by rocks. One of these raj^ids, that of Lalinde, occurs only a few miles above Bergerac, and even below that 188 PEANCE. town navigation is interfered •with by rapids. Thougli rendered navigable for a distance of 250 miles above its tidal head for barges drawing 12 inches, the Dordogne, owing to these rapids, is very little used as a commercial highway. FoREZ, Beatijolais, Charollais. The surface of the granitic plateau to the east of the Allier is far more varied than that to the west of the river, and more especially in the hills of Forez (5,380 feet) wo meet with landscape scenery quite Alpine in its character, the bottom of the valleys being covered with meadows, and their slopes wooded. One of the most delightful valleys of this part of France, the scene of the pastoral plays of Honore d'Urf^, is that of the northern Lignon. Beyond this valley porphyr}^ enters largely into the structure of the hills, including the Bois-Nolrs, or "black forest" (4,2:i8 feet), and the range of La Madeleine (3,820 feet). The wide valley of the Loire and the coal basin of St. Etienne, one of the most productive of France, separate the heights of Forez from the ranges form- ing the northern continuation of the Cevennes, and constituting the water-shed between the Mediterranean and the Atlantic. Granites predominate in these ranges, but are associated with a great variety of other rocks. The heights usually known as those of Lyonnais (3,293 feet) consist of granite and meta- morphic rocks. The mountains of Beaujolais (3,320 feet) are composed of lime- stones, marls, and sandstones, pierced by porphyries which form picturesque j^romontories along the Saone, and extend westward across the valley of the Loire until they join the porphyries of Forez. In the hills of Charollais (2,540 feet) granite plaj-s but a subordinate part, most of the area being occupied by Jurassic limestones and still more recent formations abounding in fossils. There are several coal basins, the best known amongst them being that of Le Creusot. The Canal du Centre, which joins the Loire to the SaAne, passes across a depression in this range (1,100 feet) which completely severs the outlying porphyritic and granitic mountains of Morvan (2,960 feet) from the great central plateau of France. Inhabitants. Sterility of soil, an inclement climate, and remoteness from the great high-roads of commerce sufficiently account for the sparse population of the central plateau of France. Only the fertile plains of Limagne and of the Loire and the mining districts can boast of a population exceeding the average of France. In the coal basins of the Loire the population has doubled since the beginning of the century ; but though the cattle breeders inhabiting the regions of pasturage have been benefited by this increase, the country, nevertheless, is not capable of supporting the whole of its children, and emigration to the more favoured regions of France is continuing steadily. Auvergnate canvassers are met with throughout France, and even in some of the neighbouring countries, and many of the new buildings in Paris have been constructed by masons imported from Correze, Haute- Vienne, and Creuse. The emigration from Cantal to Spain, first called into existence by LIBRARy OF THE UNIVERSITY of rtLINOIS. •J* LOZERE.— nAUTE-LOIEE. 189 the pilgrimages to the holy shrine of Compostella, where the monks of Aurilluc had a church, has not yet ceased. The peasants of Ytrac and Crandelles, two villages to the west of Aurillac, are those who visit Spain most frccjucutly, and this familiarity with the couiitiies lying beyond the Pyrenees is siiid to be reflected in their customs, and even physique. In former times the Aiivergnates regularly returned to their homes to enjoy the fruits of (heir thrift. They kept aloof from strangers when abroad, and though honest, their love of gain supplanted all other feelings. They were hospitable and .straighttbrward only when dealing witli llieir own eountryineu. In our own days, however, many Auvergnates never return to their native home, and become merged in the general population of modern France. Topography. LozicKE. — This is one of the poorest regions of France, and its popular designa- tion as Gevaudan — that is, country of the Gabales — is involuntarilj' associated in our mind with a barren, storm-beaten plateau. The rivers Lot and Tarn drain most of the department into the Garonne, only a small portion of it being drained by the Allier and the Ardeche, the former a tributary of the Loire, the latter of the Ehonc. There are profitable lead mines (produce 435 tons of lead), but hardly any industry. Mciulc (G,239 inhabitants), lying at a height of 2,460 feet above the sea, is looked upon as a place of exile by the functionaries who are stationed here. Coarse woollen stuffs arc manufactured, and many strangers pass through the town in summer on their way to the sulphur springs of Bagnols, in the valley of the Lot. Manrjok (4,638 inhabitants), in a side valley of the Lot, manufactures coarse woollens. To the north of it, near the Truyere, lies Javols, the old capital of the Gabales, and still farther north the small town of Sf. A/ban (1,148 inhabitants). Florae (1,845 inhabitants), near the Tarn, and in one of the canons hounding the Causse of Mejean, and Cahis (584 inhabitants), near which are lead mines, are the only places of any importance in the south, where Protestant Camisards and the dragoons of Louis XIV. waged a bloody war. Clidfcauncuf- Randon recalls the death of Duguesclin in 1380. The principal town on the rail- way which runs through the cast of Lozere, up the valley of the Allier, is Laiigogne (•''i,228 inhabitants). Haitk-Loike includes the whole of ancient Yclay, together with some adjoin- ing districts, and though much of its surface consists of sterile granitic plateaux and sheets of lava, its population is relatively dense, for there are mineral treasures, fine pastures, and manufactures of ribbons and point-lace, known as dent elks du Puy. Le Puij-en-Vcla; to the river Lot and beyond, its principal centres of population being Aiiln'n {2,17'2 inhabitants) and Decnzccille (5,908 inhabitants). The coal, unfortunately, is of inferior ipiality, but iu spite of this, iron works, forges, foundries, machine shops, and glass works have sprung up near the mines, contrasting curiously with the ruined castles crowning the neighbouring heights. At Cranmr there arc mineral springs. Tlie coal near this place took lire centuries ago, and still keeps burning. ViUefram-hc (7,819 inhabitants) is a curious old town, charmingly situated on the Aveyron, near the western frontier of the department. The north, including Pig. 113. — RoQlEFORT. Scale 1 : 100,000. the valleys of the Lot, the Bourdon, and the Truyere, is equally noted for its picturesque scenery, though rarely visited. The principal towns there are St. Geniez (3,1G7 inhabitants), in the "country of Olt," and Espalion (2,o8() inhabit- ants). Conques and Buzoith are delightful villages in the valley of the Dourdou. Taux, the ancient vUbigeois, embraces a mountainous crj'stalline region iu the ea.st, and a fertile hilly region in the west, the latter a productive agricultural district, the former more adapted for the breeding of cattle and sheep. The coal basin of Carmaux, yielding about 2-50,000 tons a year, lies within the department. Two towns in the picturesque valley of the Cerou, which traverses the northern portion of the department; contrast strangely with each other, the one, Carman r (5,384 inhabitants), having but recently grown from a small village into an impor- o 2 192 FEANCE. tant town, owing to its vicinity to productive coal mines ; whilst the other, Cordes (2,115 inhabitants), perched upon its high rock, has retained all the charac- teristics of a town of the thirteenth century. AM (15,874 inhabitants), the principal town on the Taru, the birthplace of Fig. 144. — Decazeville. Scale 1 : 90,000. The Coal Basin is shade3. 0° i3'0 of Pari;s 2"ioIi E.uf (il tiht dc btaiiiiioiik IMile. Lapeyrouse, and the original seat of the Albigenses, upon which the hand of the northern crusaders weighed heavily, abounds in curious old buildings, including a cathedral built in brick, a fortified archiepiscopal palace, and a remarkable bridge LOT. 198 over the Tarn. Xear it are many old castles. At Leseiirc there is an old church said to have been built by the Albigcnscs, and still farther to the east a series of rapids, known as Saut-dc-8abo, stops the navigation of tlie Tarn. The lower valley of that river is noted for its fertility, fuiilluc (G,090 inhabitants) was the great centre of the wine trade during the dominion of the English, whilst L'Isle d'Albi (1,743 inhabitants) and Babiisfeiis (3,108 inhabitants), in addition to vineyards, have a few manufactories. Casfres (20,520 inhabitants), the great manufacturing centre of the department, occupies a favourable position on the Agout, wliich is joined hero by the Thor^. The manufacture of cloth is carried on there on a large scale, and there are also dyeing-houses, tan-j'ards, paper-mills, and machine shops. Mazamd (10,770 inha- bitants), on the Thore, has likewise grown into an important manufacturing town, and there as well as at metum of the Romans, was a populous town in tho time of the Gallo-Romaus, M'hen its Fig. 145. — Clbumont and Muntfeiuianu. Scale 1 : 40,0(10. fo&Z.df Cr. If '$• i 1 ililc. temple of Mercury proved a great focus of attraction. The Franks, and after them the Saracens, destroyed the town, and Philip the Fair established the royal courts in the neighbouring Montferrand. The latter, however, lost these advantages when the courts of law declared Clermont to be the property of the Crown. Montferrand, since that time, has been deserted, and life pulsated all the more briskly through the streets of Clermont. Most of the houses are built of black lava, and their sombre aspect contrasts strangely with the smiling country around. There are several remarkable buildings, including a magnificent Gothic cnthedrul and the Byzantine church of Xotre-Dame, near which the stone upon which sat Pope Urban IL when presiding over the Council of Nemetum is pointed out. 19G FEANCE. The fowu is noted for its semolina and other farinaceous preparations, its confec- tionery and apricot patties. Cutlery, wooden ware, and textile fabrics are likewise produced, and a brisk trade in agricultural products carried on. At the same time Clermont has not forgotten that it gave birth to Pascal, and there are several fine museums. The environs are highly interesting to geologists. An incrusting spring rises in the suburb of St. A lyre, the thermal springs of St. Mart are above the town, and old volcanoes and currents of lava arc met with in every direction. Eiom (10,004 inhabitants), formerly the second capital of Lower Auvergne, occupies a site very much like that of Clermont, and is likewise built of sombre lava. It is famous on account of its law school, and has given birth to Fig. UG— TiiiEus. Scale 1 : 40,000. 3" , JJ'E "t Or 1 MUe. some of the most illustrious lawyers of France. The environs are delightful. Volric (2,265 inhabitants), which supplies Riom with building stone and water, is commanded by the ruined castle of Tournoel, whence the eye ranges over the verdant plains of La Limagne, and as far as the town of L'Aiguejjerse (2,410 inhabitants), in the north-east, the wooded heights of Montpensier, the castles of Effrat and Randan, and the busy little town of ^laringua^. T/iicrs (11,182 inhabitants), in the valley of the Durolle, and suspended, as it were, upon the steep slopes of the Hill of Besset, is mainly engaged in the manu- facture of coarse cutlery, but there are also paper-mills, &c. Chdteldon, the old centre of industry in this part of the country, has dwindled down into an insignifi- cant village, visited only for the sake of its cold mineral springs. LIBRARV OF THE UNIVERSITY of ItlJNOIS. !l||||lHj|'fll rORRfeZK. 197 Ainlert (3,882 inhabitants), tlio old cajjital of Livradois, is tho only town in the upper valley of the Dore, and engages in tho manufacture of linen, cloth, and paper. Arlanc (1,8J0 inhabitants) and several other villages in that valley likewise manufacture coarse linens and laee. There are no towns whatever in tho hilly district lying between tho valleys of the Dore and tho AUier, for Billom, which had its own mint during tlie Carlovingian age, and a famous school in tlic thirteenth century, has dwindled down into a poor village Jssoivc (0,089 inhabitiints), the principal town on the Allier, was almost levelled with the ground during the religious wars, and the Duke of Alen(;on erected a column inscribed " Hero stood Issoire ! " The town has now recovered from these disasters, but is principally known ou account of tho natural curiosities met with in its vicinity, and more especially in the valleys of the Couzc-l'avin, the Northern Couze, and the Veyre, all of them rising in the volcanic region in the west, and descending to the Allier. Brasmc, on the Allier, close to the western frontier of the department, has become known througli its coal-fields. Another mineral district lies in the north-west, being intersected bj- the valley of the Sioule. At Pontgibaud there are argentiferous lead mines ; at St. Gervais Fig. 147. — Section of the CAiiuo.viriiKots Strata of St. Elov. coal mines; atMciiat deposits of tripoli; at C/idfeauneuf iimnevous mineral springs, cold and warm ; and at Sf. Eloij coal mines. The valley of the Dordogne, in the south-west, is visited principally on account of its fiimous hot springs of Mo)it Dore and Bourhoule, the latter being richer in arsenic than anj^ others discovered hitherto. CoRKEZE lies almost wholly within the basin of tho Dordogne, of which tho Correze is merely a tributary. Its eastern portion consists for the most part of elevated granitic plateaux affording scant pasturage to herds of cattle. Usscl (2,822 inhabitants), its principal place, is known rather on account of its claiming to be the representative of ancient Uxellodonum than for its woollen stuffs, which are also manufactured at Mcijmac (1,570 inhabitants) and other villages, and exported from Bort (2,298 inhabitants), on the Dordogne, here bounded by columns of basalt. At Argentat (2,094 inhabitants) the Dordogne becomes na\-i- gable for barges. Tulle (11,038 inhabitants), on the Correze, in the centre of the department, is 198 FEANCE. mainly indebted for its prosperity to its being the seat of a goveruracnt small-arras factory employing 1,500 workmen. The manufacture of the land of lace named after this town has ceased long ago. The neighbourhood abounds in wild gorges and picturesque waterfalls, amongst which are those of Montane and Gimel. Br ire (9,417 inhabitants), also on the Correze, is by far the most pleasant town of the department, its fine cathedral, ancient walls, and reddish hills presenting a delightful ensemble. The castle of Turenne, to the south, is the ancestral home of the famous captain of that name. The valley of the Vezere, which joins the Correze a few miles below Brive, abounds in picturesque sites. Ascending it, wo pass Alktssac (1,338 inhabitants). Fig- H8. — Tayac and Les Eyzies, on the VizliiE. Scale 1 : 90,000. -77* 1°|5-E JUj T~jra_ 1 JlUe. {jjuxd. an ancient village ; Uzerche (2,146 inhabitants), one of the towns claiming to be the ancient Uxellodunum ; and Trehjimc (1,772 inhabitants), where the manu- facture of arms is carried on. A stud for breeding horses has been established close to the old castle of the Marchioness of Pompadour, in the west. DoRDOGXE includes nearly the whole of the old province of Perigord, together with portions of adjoining districts. The rivers which traverse it divide it into several distinct regions. The granitic plateau of Nontronnais, in the north, is barren ; in the south there are extensive forests, and between the Isle and the Dordogne also heaths, now gradually being brought under cultivation. There are HAUTE-VIENNE. 199 iron mines, iron works, and paper-mills, but P^rigord no longer monopolizes the trade in truffles. Sorlat (4,521 inhabitants), the capital of the south-eastern arrondissemont, is an old city carrying on some export trade through Vitrac, on the Dordogne. Close to the latter are Dontme, a picturesque old village, and the mediaeval castle of Beynac. The principal places in the valley of the Vezcre are Terrasson (2,586 inhabitants), Muiitigiiac (•,?,o61 inhabitants), and Le Biigue (1,685 inhabitants), which export iron, wine, and truffles. The environs of Lo Bugue are famous for their caverns, which have yielded prehistoric remains of the higliest interest, and some of the more remarkable of which are near the villages of Tayac and I^es Eyzics, on the Vezere. Descending the Dordogne, we pass Laliiule {S^il inhabitants), and reach Bci-gcrac (10,610 inhabitants), which exports wines, bat is merely a shadow of what it was before the revocation of the Edict of Nantes. In the vicinity there arc several mediaeval castles, including those of Montaigne, the birthplace of the famous writer of that name. Perifjueux (23,290 inhabitants), the capital of Perigord, stands on the Isle. It abounds in Roman and mediaeval ruins, but its glory is the church of St. Front, a huge basilica, built in the tenth century, in the purest Byzantine style. Coach- building, the manufacture of cloth, the casting of iron, and other industries are carried on at Perigueux, as well as a brisk commerce ; but the other towns and villages of the valley are hardly remarkable for anything but ruins and historical associations. Ilauicfort is commanded by the castle which Bertrand de Born, the warrior and troubadour, inhabited. Tliiriers (2,114 inhabitants) exports cattle and cheese, and manufactui-es earthenware. The lower valley of the Isle is one of the most productive agricultural districts of France. The most important towns there are Mumdan (1,886 inhabitants) and Moiifpont (1,697 inhabitants). Brantome (1,292 inhabitants), with the ruins of an abbey ; Bourdcillcs, with two old castles and curious grottoes ; and Eiherac (1,818 inhabitants), the capital of the forest district known as La Double, are the principal places in the pictu- resque and well-cultivated valley of the Dronne, which forms the boundary between French and the Romaic dialect, known as Perigourdin. At Noutron (2,378 inhabitants), in the extreme north of the department, are forges and cutlery works, in which knives with box-wood handles and movable copper ferrules are manufactured. IIaok-Viexnk includes a portion of Upper Limousin, and lies wholly upon a g;ranitic plateau, having an average elevation of 1,000 feet, and intersected by the river Yienne and its numerous tributaries. Tlie soil, however, is not very favourable to agriculture, and the breeding of cattle, pigs, and horses is the chief occupation. Chestnuts form the principal food of thousands of the population. Excellent kaolin and potter's earth are found. n*. Ch^ck^ c/ytton ntuffi are -red ax Ticfar. Th* ridtdtj ot tbene tr/wns abounds in pictareiiqae '/Id catfk* are tboK 'of Bcnrbon-BujMx^ft .-; 'Tt. er the cliazact«r of the c*>nntry c> - - " - we • Mfoa. a broad Tale, •wsmpr in part. At a pojxit .j/,-ti «aad.« Jfr/x/.^A 21,1 >2 ;'.-.- the eapital ^>f the dif;partment and the birth- place of Viiian, There are tie rains of the (Ad castle of the iHike* of JJourlxjo- ALT.TFB. 203 nais, a fine Gothic church, and several other medioDval buildings of interest, but Moulius is nevertheless a to\ra of modem growth. Agriculture has made great progress in the enviions, and vast tracts of heath have recently been brought Fig. 1-51. — St. ExrENVB. Scale 1 : 30aW. r: i V ^"-ia>. T :^^ Lr. / f -.v.* H&vIbM'^ -' NM-iiir^ -4 V iit ■a.Zi: t }E^ Toooder cuItixatMU. «S«r«>»y (l,o§l iiib..ibiEauts>, in a dde vsJlev which op^is at Moulins;. is th* ciatUo of the house oi BourKni. It was here that Adhtaaar, the h«ttd o£ th« JSuuify, boQt himsielJt a castie in the teutii ctemury, luid to i-^. iS?^3>*>i:::. v^ /"% °ii»' I'lWoirfa ■ 5 Miles. with old castles. St. Uiitrojic, a village near Montmoreau, is inhabited by a colony of Limousin potters, who have retained their dialect. Charente-Ixfekieure (Lower Charente) includes nearly the whole of Sain- tonge, with portions of Poitou and Aunis. It is divided into the hilly district of Bocage ; the lowlands along the Gironde and the Atlantic, still known as " marshes," though for the greater part drained ; and the two islands of Oleron and Re, which constitute a little world apart. It is one of the richest agricultural departments of France, producing excellent vegetables and fruits, wines, and cattle. The sea yields fish, oysters, and salt, and there is also some industry. Commercially it is dependent upon Bordeaux. The population is decreasing. The southern portion of the department consists of wooded hills and extensive landes, which are gradually being brought imder cultivation. Jonzac (2,446 inhabitants) and Pons (3,440 inhabitants), both on the Seugne, the latter town CnAREXTE-mFEEIEURE. 215 having an old castle now used as town-hall, school, and prison, are the principal places in that part of the country. Saiiites (ll,loO inhabitants), the ancient Santonos, on the Charonte, is the capital of Saiutonge. A triumphal arch and a luige amphitheatre recall the Koman age. Other remarkable buildings are the Gothic cathedral, a vast crypt in the suburb of St. Eutrope, and a museum rich iu antiquities. Saintes has potteries, with which Bernard Palissy's name is houourablj'' connected, and carries on a brisk trade in brandy. Following the course of the Charonte, ■we pass Titillchourg, where St. Louis defeated the English ; the castle of Crazanncs, and the busy port of Fig. 160. — La Eochelle. Scale 1 : 30,000. ^•■f^^VJ^ ^»*^e>^^:--'-<.-^""-inF<', I'llo'WofCr . 1^ Miles. St. Savinien (1,458 inhabitants), near which are famous quarries; and finally reach Rochcfort (25,454 inhabitants), the largest town of the department, and one of the five great military ports of France. The foundation of the town hardly dates back two centuries. It is regularly built, has fine public gardens, but no remark- able buildings except those connected with naval or military matters, including an arsenal, dockyard, and huge hospital. The navigation of the Lower Chareute is intricate, but men-of-war are nevertheless able to proceed up to the to^vn, where they are safe from every hostile attack. The roadstead is defended by several forts, and well sheltered. Tomiay-Charente (2,203 inhabitants), only 3 miles above 210 FRANCE. Rocliefort, is a commercial port, much frequented by English vessels in search of brandy. Marennes (1,863 inhabitants), in the marshes to the south of Rochefort, was famous in former times for its salt-pans, which j'ielded as much as 100,000 tons, but this industry has disaj^peared almost entirely, and the salt-pans have been con- verted into pasture- grounds, fish, or mussel ponds. Commerce, too, has nearly deserted the town ; and the tower of its church, 256 feet in height, no longer serves as a landmark to the mariner. The fattening of oysters, however, is carried on now with considerable success here, as well as at the neighbouring La Tremhlade Fig. 161. — La Rochelle. (2,568 inhabitants), no less than 30,000,000 being sold annually. La Trem- hlade likewise attracts a few visitors, but the great seaside resort of the depart- ment is Eoijan (4,198 inhabitants), at the mouth of the Gironde. A few miles inland from that place is Saujon (2,209 inhabitants), with a Roman obelisk (Pire Longe) 72 feet in height. The island of Oleron has grown rich since the introduction of the vine, the value of land having quadrupled in the course of forty years. The principal towns on the island are St. Georges (999 inhabitants), Le Chateau (1,578 inha- bitants), and St. Pierre (1,545 inhabitants). CH^LREXTE-IXFEEIEURE. 217 La Eochelle (19,030 inbabitants) is the principal commercial port of the depart- ment, and its capital. In the fourteenth and fifteenth centuries the town was one of the great ports of France, and on the eve of St. Bartholomew its Protestant citizens forced the royal army to retire, after a siege which cost it 20,000 men. Fifty years later Richelieu compelled the surrender of the town, after nearly the whole of its population had died of hunger. From this disaster tho place has never completely recovered, but its citizens are still noted for their public spirit, and there remain in it many buildings dating back to the Middle Ages. There Fig. 162. — Aks-es-R£. are " rows " (porches) as at Chester, an old town-hall, and four huge towers, one of which was formerly used as a lighthouse. Tho commerce of the town has considerably increased since railways connect it with Paris and Bordeaux, and it is proposed to construct docks capable of receiving trans-Atlantic steamers. The island of Re, close to La Rochelle, supports a dense population, who cultivate the soil, grow wine, fish, and make salt. Their M'inc, however, like that of Oleron, has the flavour of the seaweed with which they manure their vine- yards. The principal towns on the island are tS'Vf of Paris P^deS^&MM^'--, Z''2SVWof Gr. 3/>ef,ti. 10 /lei I X^/aiAiOtu E— _i DepOt S Fathoms ^ ■ ■! n Jo aiidmore, . 5 Miles and a local proverb says that " no bowl can be thrown in the village but stops in front of an honest man's house." Topography. NiEVRE, thus named after a little river entering the Loire at Nevers, is the modern representative of Nivernais. It is within this department that the Loire first assumes the character which it retains throughout its middle course. The crystalline heights of Morvan in the east are drained into the Seine. The soil is not very fertile, but carefully cultivated. There are mineral springs, iron and coal NIEYBE. 281 mines, clay pits, and ninnufactorios of china, cutlery, and hardware. The iron industry of the country dates back to a very remote age, and the remains of Gallo- Homan forges are met with by hundreds. The population, owing to the hilly nature of the department, is not dense. Of lute years it has decreased. Decize (3,547 inhabitants) occupies an island of the Upper Loire, and has several iron works, supplied with coal from the neighbouring mines of La Machim (3,091 inhabitants). Ncccrs (20,(i01 inhabitants), the capital, occupies a favour- able site near the junction of the Loire and AUicr, and is the centre of a busy manufacturing district. It enjoyed some importance in the time of Julius Cicsar, but its finest edifice is the old castle of its dukes, now used as a court of justice. The manufacture of china was introduced by the Gonzagos of Mantua, who were proprietors of the town in the sixteenth century, and still flourishes, but the Fi^. 173. — Le Cuoisic and Batz. Scale 1 : 150,000. I »" So \V .if I'.li-is 2 Miles. largest establishment is the Government arsenal for the manufacture of cannon and artillery carriages. At Imphy (1,437 inhabitants), above Nevers, are iron foundries ; ai FourchumhanU (5,G8G inhabitants), below, iron works and a foundry ; and at Guerigny (1,870 inhabitants) the Government foundrj' of La Chaussade. Travelling down the Loire we pass Poiigues, with its steel springs ; the old monastic city of La Charity (4,776 inhabitants), with an old abbey, a " daughter " of that of Cluny, and exceedingly wealthy in the eleventh and twelfth centuries; rouilly-Kitr-Loire (1,939 inhabitants), witli famous ^•incyal•ds planted by the monks of La Charitu ; and Cosiic (0,711 inhabitants). St. Amand (1,443 inhabitants), in Puisaye, at some distance from the Loire, has potteries, while Donzy (2,560 inhabitants), to the south of it, is known for its hardware. 232 FE.iNCE. Chateau-Cliinon (2,593 inhabitants), the old capital of Morvan, in the eastern portion of the department, occupies a most picturesque site overlooking the Yonne and the wooded heights beyond it. Descending the river just named, we reach the busy little town of Clamccij (4,663 inhabitants), which carries on a considerable trade in timber. CiiER includes about one- half of Berry and a small portion of Bourbonnais. It is bounded by the Loire in the east, whilst the Cher, with its tributaries, Yevre and Auron, traverses its western portion. The department produces corn, hemp, and sheep, the latter noted for their fine wool. Its iron mines, yielding 274,000 tons of ore annually, are of considerable importance. Sancerre (2,830 inhabitants) is the only town of importance on the Loire. It has become known through the heroic siege which its Protestant inhabitants sus- tained in 1573. Proceeding up the Aubois, we pass Gucrchc (1,837 inhabitants) and Sancoins (2,970 inhabitants), and following the canal of Berry, reach the valley of Auron, the richest iron district of the department. The town of Dun-Ie-Roi (4,357 inhabitants) occupies its centre. Bourses (31,102 inhabitants), the old capital of Berry, occupies a low site at the confluence of the Auron with the Yevre. It is the Avaricum of the Romans, and a council was held here in 1225, which led to Louis VIII. taking the field against the Albigcnses. The most remarkable buildings of the town are a cathedral of the thirteenth century ; the mansion of the silversmith, Jacques Coeur, a masterpiece of the Eenalssancc, now used as a court of justice ; and the Hotel Cujas, converted into police barracks. A vast arsenal, including a cannon foundry, a laboratory, stores, and artillery ranges, occupies a considerable area to the east of the town. Passing 3Ichun (5,25G inhabitants), with its manufactories of china, and a castle in which died Charles VII., we reach Vierzon (10,053 inhabitants), at the confluence of the Yevre and Cher, the most important manufacturing town of the department, where china, glass, cutlery, textile fabrics, and agricultural machinery are produced. St. Amand-Mont-Bond (7,719 Inhabitants) is the only town of importance on the Cher. Near it are Roman ruins, including a temple, a theatre, baths, and an aqueduct. A castle of the Duke of Mortemart, sumptuously restored, lies to tlie north of the town, in the forest of Meillant. Indee forms a portion of the old province of Berry. The river Indre traverses its centre, whilst its north and south are respectively drained by the Loire and the Cher. The south of the department is occupied by granite moimtains, but the greater portion of it consists of Jurassic limestone or tertiary plains. In these latter three districts are distinguished, viz. the Brenne, a tract abounding in pcnds, woods, and heaths ; the Bois-Chaud, a pebbly tract covered with forests ; and the Champagne country, a limestone district, not exactly distinguished for its fertility. The iron industry, which was of great importance formerly, is declining steadily. Issoiuhm (11,293 inhabitants), the largest town in the basin of the Loire, and one of the oldest in France, has suffered much through the revocation of the Edict LIBRARY OF THE UNIVERaTyofltLiNuIS. LOIHET. 2C3 of Nantes, but still engages in the manufacture of leather aud of woollen stufl's, drawing most of its raw materials from the surrounding country. The valley of the Theols, as well as the country to the west of it as far as Vafaii (2,045 inha- bitants) and Lcrroujc (3,293 inhabitants), abounds in prehistoric remains and medixval castles. One of these latter is at Vakii^ay (1,812 inbabitants), and within its walls Napoleon conBned King Ferdinand VII. of Spain. La Chatre (4,39-4 inhabitants), on the Upper Indre, has important markets. Near it is the village of Xoliunl, where Georges Sand resided. Cliuteaiiroux (1(3,980 inhabitants), lower down on the Indre, and the capital of the department, has manufactories of tobacco and army cloth. It was founded in the tenth century, but for a long time remained inferior to the abbatial city of Diok (2,334 inha- Fig. 174. — Oia^ANa. Scale 1 : tOO.OOO. VV ,.fl'. u*f:-^''''*"|«'y^^ "Trsf lUUe. bitants), on the opposite bank of the river. The other towns on the Indre are Buzaiigaiii (3,470 inhabitants) and ChCdiUon (2,123 inhabitants). Argcnton (5,003 inhabitants), on the Creusc, is an important town, having tan-yards, cloth factories, paper-mills, and brick-kilns. Le Blanc (4,724 inha- bitants) has cloth factories. At Neuvtj St. Scjnikre (1,292 inhabitants), in a side valley of the Crcuse, there is a curious old church imitated from that of the Holy Sepulchre at Jerusalem. LoiRET, named after a subterranean river which rises to the surface near Orleans, includes the greater part of old Orleanais. It occupies that portion of France where the valleys of the Loire and the Seine approach nearest to each other. The vallcj* of the Loire, with its fertile fields aud populous towns, traversse the centre of the department. To the north of it lie the forest-clad hills of Puisaye ; the Gatinais, partly wooded ; the forest of Orleans ; and the corn-fields of Beauce. To the south of the river are the sterile sands of Sologue. 234 FEANCE. Bn'nre (3,970 iuliabitaiits) is the first town met witli on descending the Loire. Its position at the month of the canal which connects the Loire with the Seine enables it to carry on a profitable commerce. Gien (G,493 inhabitants), a few miles lower down, has potteries. We then pass Sit?/// (1,980 inhabitants), with an old castle of Henri IV.'s duke ; and Sf. Beno'it, a very important town in the time of the Carlovingians, with the remains of an old abbey ; Cliatcaiinciif (2,799 inhabitants), an old residence of the Kings of France ; and Jargcau (1,558 inha- bitants), where Joan of Arc was wounded during the siege of Orleans. Orleans (49,896 inhabitants) is one of the great historical towns of France, and has played a part quite out of proportion to its pojiulation. "Upon the fate of Orleans frequently depended that of all France; the names of Cscsar, Attila, Joan of Arc, and De Guise record the sieges which it has sustained." Amongst its ancient buildings arc a tower captured b)^ Joan of Arc during the memorable siege of 1-429 ; an old town-hall, converted into a museum ; several churches, including a cathedral erected in the seventeenth century ; a fine town-hall of the Renaissance ; and several noteworthy private houses. Woollen stuffs are manufactured, but the town is prominent rather for its commerce than for its industries. The vicinity abounds in nurseries and market gardens. Lower down on the Loire are St. Ay, noted for its wines ; Jilcung (3,122 inhabitants), an old town ; Cleri/ (1,225 inha- bitants), with a church containing the tombs of Louis XL andDunois; and the picturesque town oi Bcaugcncij (3,901 inhabitants), frequently mentioned in mili- tary history. Couhnicrs, where a battle was fought in the last war, and Patay, where Talbot was taken prisoner by Joan of Arc, are north of the latter. Pithh'iers (4,899 inhabitants), in Beauce, exports almond cakes and lark patties- Passing thence through Beaune hi Rolande, a place mentioned in connection with the events of 1870, we reach Montaryis (9,175 inhabitants), the chief place of Gatinais, built upon several islands of the river Loing. Lorn's (1,438 inhabitants), an old town to the south-west of the latter, has become known through a code of laws collected in the twelfth century, and for a long time in force throughout the surrounding districts. Loir-et-Chkr is named after two rivers, which intersect its northern and southern portions, separated by the valley of the Loire. In the north are the corn-fields of Beauce, but the verdant hills lining the southern bank of the Loire soon merge into the di-eary plains of Sologne. About one-tenth of the area is covered with forests, an equal area consists of heaths, and there exists but little manufacturing industry. Mer (3,467 inhabitants), on the Loire, has a few vineyards. At Siietres may be seen " sacred " stones and the remains of an ancient city ; Mcnars boasts an old castle; and /S/". i)e«/.s has mineral springs similar to those of Spa. Blois (18,188 inhabitants) is beautifully situated upon hills overlooking the Loire. Historically it abounds in interest. It was here the Estates of France met between 1576 and 1588, the Duke of Guise was assassinated, and Catherine de Medicis breathed her last. The fine old castle in which these events took place has been carefully restored. Amongst the famous children of Blois was Denys Papin, the physician, LIBRARY OF THE UNIVERSITVoflLUNOIS, LOIR-ET-CUER. 535 •whom intolerance drove out of the counfiy. The vicinity of Blois abounds in old parks and castles. The old palace of Chamhord, erected by Francis I., one of the finest specimens of the Renaissance, is one of the most remarkable amongst them. The castle of Bcaiireganl, near Bcuvroii, is noted for its portrait gallery. The castle of Cliaiimont, below Blois, surpasses all the above on account of its picturesque site. Homoraiifin (7,436 inhabitants), the principal town of the Solognc, had impor- tant manufactories formerly, but is of little note now. On the Cher are Se/hs (3,259 inhabitants) ; Sf. Aigitan (^2,5%1 inhabitants), with mills and tan-yards ; Fig. 175. — CuABTUES. ScUe 1 : 40,000. . 1 line. Thizie, noted for its red wines ; and Montrichanl (2,881 inhabitants), with a fine castle. The houses of this to^m arc constructed with a stone known as " toph of Saumur," which is procured from the quarries of Ihuvre, near the Cher. Vendome (7,80G inhabitants), on the Loir, is the only town of note in the north of the department. Up to the time of the Reformation it boasted of tan-yards, ■woollen and glove manufactories, but its industry is nearly gone. Its fine Gothic tower and huge castle are quite out of proportion to the number of its inhabitants. Monioire (2,65-4 inhabitants), lower down on the Loir, has an old castle, and the vicinity of both these towns abounds in Roman and prehistoric remains, including a subterranean town, in part still inhabited 236 TBANCE. EuRE-ET-LoiR, named after its two principal rivers, includes the greater part of Beauce, and is almost void of natural beauties. The western districts of Dunois, Drouais, Thymcrais, and Perche offer more varied scenery. The department is one of the granaries of France, and ftimous for a fine breed of horses known as Percherons. Chateauduii (6,061 inhabitants), on the Loir, is the old capital of Dunois, and boasts of an ancient castle. The other old places of note on that river are Bonncval (2,373 inhabitants) and Chycs (1,759 inhabitants). Norjent-k-Rotrou (6,569 inhabitants), on the Huisne, has an old castle built by the Counts of Perche, and manufactures textile fabrics. The villagers in the neighbourhood engage extensively in baby-farming, and the mortality amongst their little charges is extraordinarily large. Chart res (20,067 inhabitants), on the Eure, the old city of the Carnutes, and the capital of the department, has a magnificent cathedral, the two steeples of which are visible for miles aroimd, and several other interesting churches. The ancient fortifications have been converted into public walks, and only one of its fortified gates now remains. Descending the Eure, we pass Maintcnon, with an old castle. Drcux (7,087 inhabitants), in a side valley of the Eure, is an old seat of royalty. It contains the mausoleum of the Orleans family. In the vast forest extending to the north of it lies the castle of Anet, which Philibert Delorme built for Diana of Poitiers. Indke-et-Loire includes nearly the whole of the old province of Touraine. It consists of several well-marked districts, viz. the sterile tertiary plateau of " Gatinc," to the north of the Loire ; the rich alluvial tract of Varenne, between Loire and Cher ; the elevated tract of La Champcigne, between the Cher and the delightful valley of the Indre ; the sterile plateau of Ste. Maure, beyond the valley ; and the cretaceous district of Veron, which extends along the Loire, between it and the Lower Vienne. On the Loire rise several magnificent castles, amongst which are those of Amhoise (4,475 inhabitants), a favourite residence of the kings during the sixteenth century; of Poce; and of CIos-Luci, within the walls of which died Leonardo da Vinci in 1519. Another castle equally famous rises upon an island of the Cher, at Chcnonceaux, one of the finest examples of the Renaissance, where Farmer- General Dupin gathered around him the most famous representatives of the litera- ture of the eighteenth century. Tours (48,325 inhabitants) occupies a site on the narrow tongue of land lying between the Loire and the Cher. This fine town transmits to us the name of the old tribe of the Turones. Its Roman remains are restricted to a few remnants of the old walls and to the foundations of an amphitheatre. The Middle Ages are represented by a cathedral, the towers of St. Martin's Church, and the ruins of a palace buUt by Louis XI. Amongst modern structures the fine bridge over the Loire, which connects Tours with its suburb of St. Symphorien (2,169 inhabitants), is the most remarkable. A statue of Descartes has been erected upon it. Tours is one of the most pleasant towns of France, and its library, museum, and scientific IKD BE- ET- LOIRE. 287 societies iiffoid iutellectuul resources, but its commerce and industry ure fur lets than might be expected from its favourable geographical position. In the time of Louis XI. it bad a population of 80,000 souls, but its pri spcrity was destroyed 1)y the revocation of the Edict of Nantes. Tiiere arc railway works, silk-mills, woollen factories, tan-yards, and manufactories of glazed china. Candied prunes are amongst the delicacies for which " Fat " Tours is celebrated. Vourraij (1,3!H inhabitants), to the cast of Tours, produces a superior wino. Mettraij (l,87o inhabitants), to the north, has a reformalory founded in 1809. Cliaieaurenault (3,487 inhabitants) is the largest town in that part of the depart- ment which lies to the north of the Loire. Its tan-yards and leather manufactures are of considerable importance. Descending the Loire, we pass several fine castles, including those of Lui/nes, Vereiz, Ciuq-Mars (St. Medard), and Langeais, the latter one of the finest examples of the militury architecture of the fifteenth century. Bourgueil (1,711 inhabitants), Fig. 176.— TouKS. ^ lule I : i:CO,(«.» SSlUcs. on the north of the Loire, has vineyards, but the red wines grown there do not keep. Lochts (3,689 inhabitants) is the principal town in the valley of the Indre. In addition to a huge castle, now used as a prison, it boasts of several mcdioeval buildings, including two royal castles. Moiitlazon and Azay-lc-Rkh'au (1,335 inhabitants), lower down on that river, are likewise noted on accoimt of their old castles. Chinon (4,536 inhabitants), on the Vienne, is one of the historical towns of France. From the time of Clovis to that of the religious wars it was one of the most coveted fortresses. The Norman Kings of England frequently resided here, and Charles VII. of France here assembled the Estates of his kingdom. Fearful scenes have taken place within its walls, and a spot is still pointed out where one hundred and fifty Jews were burnt for poisoning the wells. Rabelais was born in the neighbourhood. Ascending the Yieinie, we reach L'lale liouc/iani, with VOL. II. K 238 PEANOE. cement works, and La Haye, tlio birthplace of Descartes. At Grand Pressignij, near the latter, M. Leveille, in 1863, discovered a rich store of flint implements. Ste. Maurc (1,684 inhabitants) lies on the steiile plateau to the north of the Vienne. RichcUeu (2,328 inhabitants), in a side valley of that river, was the birth- place of the famous cardinal of that name. Of the magnificent palace which ho built himself there exist now only a few insignificant ruins. Maixe-et-Loire, named after the two rivers which join below Angers, includes the most important portion of the old province of Anjou. Crystalline rocks predominate in the east, sedimentary ones in the west, and these two zones conse- Fig. 177. — Angeks. Scale 1 : 120,000. 1 'hiae. quently differ in their physiognomy, vegetation, sj'stems of husbandry, and the material used in building houses. In the east forests of some extent still exist, but upon the whole the department is carefully cultivated, and wine, corn, fruit, and cattle form important articles of export. We begin travelling down the valley of the Loire. The first town we reach is Saunnir (13,463 inhabitants), with a fine old castle, numerous church steeples, and excellent quays along the river. The town is the seat of the great cavalry school of the French army, almost monopolizes the manufacture of chaplets, and carries on much trade in agricultural produce. The vicinity abounds in antiquities. The SAETHE. 239 cromlech of Bagneiir, witliin a mile of the town, is the finest of all Anjou. At Dout-lii-Foiitaiiie (3,194 iuhubitaiits), farther to the south-east, are several other cromlechs ; but far more famous than these are the remains of a magnificent abbey at Fontevrault (2,651 inhabitants), now used as a house of detention. The villages below Saumur, such as Tri-res, Cunault, Qcnues, La Menitri; and 57. Jfaiir, arc remarkable on account of their ruins of ecclesiastical or other old buildings. Lis Poiiti-de-Cc (1,876 inhabitants), on an island, is strategically important, as the passage of the Loire can easily be efibcted here. The Authion (see Fig. 1G6) joins it below that town, the principal places in its fertile valley being Loikjuv (1,876 inhabitants) and Beaufoi-t-vit-VdlUv (2,680 inhabitants), both centres of the linen industrj'. The best hemp of France is grown there. A few miles below Ponts-de-Cc, at La Pointe, the river Maine joins from the north. Still travelling down the Loire, we pass Chalonncs (2,449 inhabitants) and its coal mines ; the village of Champtocc (762 inhabitants), where Jfarshal Gilles de Rctz, the legendary Bluebeard, had his castle ; and the jncturcsque little town of St. Florcnt-k-Vicil (958 inhabitants), mth David's mausoleum of the Vendean partisan, Bonehamps. Retracing our steps to the mouth of the Maine, we ascend that river for 5 miles, and reach Autjcrs (53,366 inhabitants), the capital of the department, named after the Gallic tribe of the Andecaves, and next to Nantes the most important town in the basin of the Lower Loire. Boulevards enclose the old city, built around a magnificent cathedral, and suburbs stretch out bej-ond thcra in every direction. The castle built by Louis IX. occupies the summit of a bold rock, and there are many other mediaeval buildings which impart u character to the town. There arc scientific societies and colleges, a school of art industry, and museums, amongst which that containing a collection of the works of the sculptor, David of Angers, is perhaps the most interesting. Commerce and industry flourish. There are foundries and linen and sail-cloth manufactories. The nurseries and market gardens in the neighbourhood arc famous throughout France, and the vineyards of Si. Barthilemij, Rochefort, St. Georges, and Serrant enjoy a high reputation. The slate quarries {ardomerex), to the east of the town, are the most important in France, yielding about 200,000,000 slates annually. Segre (2,212 inhabitants) and Baugi (3,318 inhabitants) are the only towns of anj' importance in the north of the department. Cholet (12,335 inhabitants), in the south-west, on a tributary of the Sevre, suffered much during the Vendean war, but recovered rapidly from its disasters. It is now one of the centres of the linen and woollen industry of France, besides which it carries on a brisk trade in cattle. The surrounding villages are dependent, in a large measure, upon the manufactories of Cholet, as are also Beaupnau (2,579 inhabitants), on the Evrc, and Chemillv (3,073 inhabitants). At Thoiiarci, on the Layon, are Roman ruins ; whilst Brksac, on the Aubance, boasts of a sumptuous castle built in the seventeenth century. Sartjie includes portions of the old provinces of Maine, Anjou, and Pcrchc. The Sarthc, which flows west through a hilly district, and the Loir, the valley of which is bounded by low chalk cliffs, draiii the department into the Loire. P. 2 240 FEANCE. Jurassic limestones, chalk, and tertiary formations predominate. Agriculture is the principal occupation, the land being cultivated for the most part by farmers. Its geese, pullets, and capons are famous throughout France. Fig. 178. — The Slate Quakkies neaii Angers. Le Mans (45,709 inhabitants) occupies an elevated site at the confluence of the Huisne with the Sarthe. It is a prosperous town. Roman towers and a magnifi- cent cathedral attest its antiquitj^ but its numerous factories prove that it is 8ARTUE. 2il abreast of modem times. Hardwaro, agricultural implements, linens, and other textile fabrics are manufactured. Ftcsuay-le-Vicomie (3,010 inhabitants), on the Upper Sartho, at the foot of a tottering fortress, manufactures linens, whilst SnUt' (5,334 inhabitants), on the Lower Sarthe, has marble quarries, manufactories of farinaceous preparations, and cattle fairs. Within a couple of miles of it is the famous abbey of Soksmes, founded in the thirteenth century. SiUc-k'-Gtiillaume (2,995 inhabitants) and Louv, two small towns to the west of the Sarthe, engage in the manufacture of linen, an industry likewise carried on Kg. 179.— Lb Man8. Scale 1:60,000. :"'10 Wof Pirun . 1 llilc. in the picturesque town of Mamera (5,147 inhabitants), and at Bonnitahk (3,185 inhabitants), to the east of that river. La Ferti-Bernard (2,634 inhabitants) is the principal town in the beautiful valley of the Huisne. At Diiiieau, near it, may be seen a remarkable cromlech. La Fkche (7,468 inhabitants), on the Loir, is the seat of a military school occupying the old Jesuit college in which Descartes was educated. Higher up on that river are Le Liide (2,720 inhabitants), with a fine modern mansion ; Chulvau- du-Loir (2,527 inhabitants), inhabited by clog-makers, quarrymen, and tanners ; 212 FEANCE. and Charfre, wliere there are several subterranean liabitations. North of the Loir are Ecommoy (1,841 inhabitants), Maijet (1,631 inhabitants), and 8t. Calais (3,000 inhabitants). Mayenne lies almost wholly within the basin of the river whose name it bears, and which, lower down, is known as Maine. Geologically it forms a part of Brittany. There are slate quarries, coal mines, and lime-kilns. The linen industry is of importance, but more so the cultivation of the soil and the breeding of cattle. Mayenne (8,826 inhabitants) is the chief town in the north of the department. The manufacture of linen occupies several thousand workmen in the town and the villages near it, and there are also cotton-mills, flour-mills, and lime-kilns. Ern^e (3,866 inhabitants) and Chailland (518 inhabitants), both on the river Ern(5e, which enters the Mayenne from the west, are likewise engaged in the linen industry. Juhlains, a village to the south-east of Mayenne, is the old capital of the Aulerci- Diablintes, and, in addition to a magnificent castellum, possesses other Roman ruins of the highest interest. Laval (25,110 inhabitants) is a delightful city on both banks of the Mayenne, surrounded by shady walks and fine gardens. Ambroise Pare, the " father of French surgeons," was a native of the place, and a monument has been erected in his honour. Several thousand workmen are engaged in the manufacture of fancy tickino-, and there are also marble works and lime-kilns. Coal is worked at Gcrmanehieres, to the west of Laval ; whilst the rocks of Coevrons, above the fine old city of Evron (3,433 inhabitants), yield porphyry, granite, kaolin, and man- ganese. Ste. Suzanne, a village near Evron, still possesses its mediajval castle and walls. Chateau-Gonticr (7,218 inhabitants) on the Lower Mayenne, is a great agricul- tural mart, and its ferruginous springs attract a certain number of visitors. Craon (3,874 inhabitants), to the west of it, was the birthplace of Volney. It is famous for its pigs and its breed of horses. Coal mines and slate quarries are near it. Loire-Inferieure is intersected by the Lower Loire and its estuary. Historically and geologically it belongs to Brittanj', but the peasantry have long ago discarded the use of the Breton tongue, and commercial interests have aKenated the country from Brittany. The department is rich in horses and cattle, agriculture and gardening are carried on with much success, while industry and commerce flourish. Nantes (116,093 inhabitants), one of the great commercial towns of France, dates back to a time far anterior to that of the Romans, and bears the name of the Grallic tribe of the Namnetes. Its position, at a point where the rivers Erdre and Sevro join the Loire, is exceedingly favourable for commerce, especially as sea- going vessels can reach its fine quays with every tide. Its most remarkable buildings are a castle on the river bank, a Gothic cathedral, and modern palatial edifice, beneath the roof of which have been brought together the library, museum, and art collections of the town. The public park is one of the finest. Historically the name of the town is connected with the Edict of Nantes, promul- gated by Henri IV. in 1598, but revoked by Louis XIV. in 1685. As a maritime LIBRARV OF THE UNIVERSITY of ULINOIS. LOra PMNF^EIEURE. 243 port the town is losing ground since the introduction of larger vessels, for only those drawing less than 10 feet of water can safely venture up the river. At the same time it must not be forgotten that the commerce of St. Nazaire, at the mouth of the river, is carried on almost exclusively by Xantcs firms. In former times Nantes supplied the French West Indies with slaves, taking sugar in return, and up to the present time its intercourse with these colonies is very active. It is the great colonial dejjot of the valley of the Loire, and its sugar refineries only vield to those of Paris and Marseilles. Iron foundries, lead and brass work.s, oil-mills, Fig. 180.— Nantes. ficale 1 : 56,000. J- WW or Par« -y ; JsKfewjw^^-H^^jsf ■ IMUe. soap works, machine shops, a tobacco manufactory, ship-yards, and other industrial establishments give employment to thousands of workmen. Other thousands work in the granite quarries above the suburb of Chatitenaij (8,490 inhabitants). The preservation of food annuallj' increases in importance. The valle3-s of the Erdre and Sevre abound in fine old castles and modern country mansions, the latter more especially around Cllsson (2,241 inhabitants). Ancenis (4,668 inhabitants) is the only town on the Loire above Nantes. Descending the river, we pass Lidre (2,229 inhabitants) and the island of Indret, 244 FRANCE. with an old castle and a Government manufactory for marine engines ; Coueron (1,063 inhabitants) and its lead works; and reach Sarenni/ (1,703 inhabitants), a small town built on a bluff to the north, affording a magnificent prospect over the estuary of the Loire. Paimkeiif (2,473 inhabitants) lies opposite, but its harbour is hardly ever now visited by merchantmen since docka have been excavated at Sf. Nazaire (14,761 inhabitants), at the mouth of the river, and 30 rjiles below Fig. 181.— St. Nazaike. Scale 1 : 30.000. I>° [ 31"Wf.f P arij 2"|inVofGr. J Mile. Nantes. This town haa sprung up rapidly since 1856 around a Breton village, and packet steamers connect it with the West Indies and other parts of the world. In reality, however, it is merely an outport of Nantes, to which most of the mer- chandise is forwarded immediately after it has been landed. Its environs consist of barren heaths, and the town is very much in want of good drinking water.* * Value of imports (1875) at St. Nazaire, £13,240,000 ; at Nantes, £2,800,000 ; of eitports at St. Nazaire, £2,680,000, at Nantes £3,200,000. LOIEE-INFEBIEmE. 245 The district to the west of St. Nazaire, with its primitive inhabitants, its ever- changing coast, and its salt swamps, yielding about 30,000 tons of salt a year, is one of the most interesting in France. Its principal towns arc Croixic (1,081 inhabitants), much frequented by seaside visitors, and Giicraiu/e (2,415 inhabitants), still surrounded by turreted walls. On the wide bay to the south of tho Loire, in the district of Rctz, are Bounjucuf (817 inhabitants) and Toriiic, a rising seaside resort, with numerous pretty villas. Clu'iteaubriaut (4,082 inhabitants) is the only place of importance in the north of the department, its old walls and gabled houses offering a curious contrast to its modern court of justice and manufactories. Agricultural progress, too, changes the face of the country, and lai-ge tracts of heath in the ^•icinity of tho agricultural school of Grandjouan have been converted into productive land. CHAPTER VIII. BRITTANY (BRETAGNE). General Aspects. IITTANY and Cotentin, the two peninsulas of Western France, are geologically of the same origin, and, together with Poitou and Cornwall, arc the principal remaining portion of a huge granitic island, which also included Poitou and Cornwall, and was separated from the continent by an arm of the sea extending to the Vosges and the plateau of Central France. An irruption of the Atlantic severed the French portion of this ancient island from that lying beyond the Channel. The ocean incessantly lashes the broken coast of these peninsulas, but their granitic rocks are better able to resist its onslaughts than is the calcareous soil of Normandy and Saintonge. The climate and physical aspects of these two peninsulas are the same, but their political history has been very different. The Bay of St. Michel completely separates Brittany from Cotentin ; and the latter being too small of extent to lead an independent life, and moreover easy of access, very soon cast in its lot with that of the population of Northern France. Brittany, on the other hand, offered a stubborn resistance to every attempt at assimilation. Thanks to its remoteness — far away from the great high-roads of nations — it was able to maintain its old customs and its Celtic tongue. The stubborn resistance offered by the Bretons to foreign encroachments was maintained for centuries. The English, though masters of Anjou and of Normandy, never succeeded in firmly establishing themselves in Brittany ; and long after that province had become French it maintained its ancient customs, and down to the present day it is distinguished for many pecu- liarities. Rocks, tortuous valleys, heaths, and forests separate Brittany from the rest of France, and the readiest access to it is afforded by the sea. Its many fine harbours facilitated the creation of a mercantile marine, and the frequent wars between England and France afforded an opportunity to the Bretons for exhibiting their prowess at sea. The rivalry between them and the " Bretons " on the other side of the channel fed their local patriotism, whUst frequent intercourse with GEXERAL ASPECTS. 247 other maritirao districts of France created amongst thern a Freuch national feelinjr. In its general features, Brittany consists of two 'Lands of granite, gradually approaching each other in the west, the triangular space between them being occupied by ancient sedimentary formations. The crystalline, fern-clad heights to the west of the Lower Loire, known as the Sillou (" furrow ") of Brittany, may be described as the edge of a plateau rather than a chain oi hills. The Yilaiue has excavated itself a passage through the granitic heights, which farther west form the range known as the Landes of Lanvaux (G7-1 feet). The granites finally give place to schists, which form the Black Mountains of Brittany, thus culled alter the forests which formerly covered them. They culminate in the bold Menez-Hom (1,083 feet), on the peninsula of Crozon. The northern granitic range of Brittany is far more complicated in its structure Fig. 182.— The Landes of Lanvavx. SciUc 1 : 050,000. S'V-ofParLsl • t\* ^gil ^3 ^m ^ iijjrj^ T?^ i^'^ ^ ffiS S m ^ y u Aim/3 ^P3 WT ^^^fe W^^ ■ ^^^^^vi U'ilUcs. than that of the south. From the plain intersected by the canal of the Ille the country gradually rises to the heights of Le Mene (1,110 feet) ; but beyond these extends a vast ledge of granite, until we reach the fine range of Arr^e and its sandstone peak of St. Michel (1,284 feet), the most prominent hill of Brittany. The vale enclosed between these granitic heights is traversed by several rivers, communication between which has been established by means of a canal, which connects the Lower Loire with Brest, but has now been superseded by railways. Brittany generally gives an impression of monotonous grandeur ; and Bi-izeux, a native poet, addresses it as the " land of granite and of oaks." But the country is not without landscapes more pleasing to the eye — heaths and fields, shadj' lanes, tranquil rivulets, half-hidden lakelets, and old walls covered with ivy. On tho seashore other sights greet the eye, and nothing can be more impressive than the billows of the Atlantic rushing upon the cliffs of Finistere. With a lowering sky the physiognomy of the country is sombre in the extreme, but the sun imparts to 248 FEANCE. it an aspect of quiet cheerfulness impossible to describe. The Bretons themselves yield completely to these impressions, and home sickness is frequent amongst them when abroad. The Coast. AxciEXT Armorica, the " Land of the Sea," fully merits its Celtic appellation, for to the sea it is indebted for its climate and for most of its resources, and the sea has shaped the temper of its inhabitants. Off the western promontories of Brit- tany the gulf-stream encounters the secondary ocean current, which sweeps the Fig. 183. — MoRBiH.w. SciM : ilO.fOO. ■ snsi T'-vis^-^w--,: -s\-.4 . 5 Miles. shores of the Bay of Biscay. The tides are violent and irregular, and the sea is perpetually in motion down to its very bottom. A powerful under-current running along the northern coast sweeps the granitic sea-bottom, piling up the sand and mud in the east. Some of the rocks forming these are but ill adapted to resist the action of the sea, and enormous blocks of rock have tumbled down from the cliffs. In the west, where sedimentary strata intervene between the two bands of granitic rock.s, the encroachments of the sea have been most considerable. The roadsteads of Brest and Douamenez penetrate deeply into the land, and almost resemble Norwegian fiords, half obliterated by alluvium brought down by the rivers which enter them. To the west of the estuarj of the Yilaine this contest between the THE COAST. 249 elements has given birth to a hind-lockccl bay known as the Morbilian, or "little sea." Islands are scattered over it, some of them inhabited, and all subject to continual changes. M. E. Desjardins is of opinion that this inland bay is ol' com- Fij;. 184.— TiiR Pemnsila of Qiiiieuos. ScoJo 1 : 100,000. IMUc. paratively recent creation. A subsidence of the land has certainly taken place there, for cromlechs have been discovered which do not even uncover at low water. The numerous islands at the mouth of this bay indicate the diiection of 250 FEANCE. the old coast, and farther off a still more ancient coast-line may be traced in the islands lying between the Points of Croisic and of Quiberou. These islands, as ■well as the elongated peninsula of Quiberon, certainly mark the extent of Brittany in some bygone age. As to the peninsula mentioned, a causeway and sands sub- merged by each flood alone attach it to the mainland. The island of Groix and the small archipelago of Glenan mark the extent of the old coast to the west of Quiberon. Tradition tells us that the nine islets of Glenan are the fragments of a larger island. As to the large island of Belle-Ile, or Guerveur, farther off the shore, it is, with the island of Yen and the sunk rock of Rochebonnc, the only remaining witness of a coast-line even more ancient than those noticed above. Doubling the bold headbid of Penmarch, or the "horse's head," we enter the Fig. 185. — TiiK Headland of CoitNOUAiLLU. Scale 1 : 400,000. ■W.u'1'.-.i Tevpiiitf^f' - y lid' /■"■'"■ "">:*,^^* .'f^- .■Wottr desolate Bay of Audierne. Not a tree grows upon the heights which surround it, and no traces of cultivation greet the eye. The headland of Cornouaille (Cornwall), to the north of that bay, juts far out into the sea. Standing upon its summit, no less than 262 feet above the sea, we are not beyond the reach of the spray, and the ground is felt to shake beneath our feet. The waves dash into the Enfer (hell) of Plogoff, at its foot, creating a sound like thunder, and at the neighbouring Bay of Trepasses the superstitious mariner fancies he hears the voices of the drowned rising above the howling storm and the roar of the waves. To our ancestors this uproar sounded like the voice of a god, whom nine Druid virgins sought to pro- pitiate by leading a life of devotion upon the weather-beaten island of Sein. If tradition can be believed, many a town has been swallowed up by the waves in that part of the country. The Bay of Douarnenez is said to mark the site of the THE COAST. 251 ancient city of Is ; and a causeway of Roman construction, leading to some place now submerged, may still be traced near the Bay of Trepasses. The island of Ouessiint occupies a position analogous to th;it of Soin, with reference to the headland of Lt'on. This clili-bound island is cultivateJ, but not a tree, not a shrub grows upon it. Mariners dro:id to approach it, for rocks abound, the tides and winds are most irregular, and dense fogs prevail. But though the passages separating Ouessant and the neighbouring islets arc full of danger, they give access to the magnificent road of Brest, where four hundred vessels find u secure shelter. Several small islands and rocks on the north coast of Brittany enable us to trace the old line of coast. The dreaded granitic headland, known as '■ Swords of Treguier," ne;ir Brehat, has oflercd a powerful resistance to the waves, but the coast farther cast has been encroached upon in many parts. In the Bay of St. Brieuc alone no less than 120 square miles of land have been swallowed up since the fifth century. Traces of ten Gallo-Roman buildings have been discovered at various spots on the beach, and the old walls on the Cape of Erquy, which bounds the bay on the east, are supposed to be the remains of the town of Rcginea mentioned on Peutinger's Table. The island of Cezembre, at the mouth of the Bay of St. Malo, formed a portion of the mainland in the twelfth century, and even more recently. Submerged forests and bogs are met with at different points of this coast, and the recovery of the trees buried for centuries beneath the sands of the beach occupies many of the poorer inhabitants of St. Malo. The remains of buildings discovered in the Baj' of St. Brieuc prove, however, that the encroach- ment of the sea is not exclusively due to its erosive action ; a subsidence of the land has evidently contributed to that result. If tradition and old chronicles are to be believed, the encroachments of the sea have been formidable indeed. The archipelago of Chausey is stated in the " Lives of the Saints " to have formed part of the mainland in the beginning of the eighth century, the area now covered by the sea being then occupied by a vast forest known as Scisciaaim nemiis. Thus much is certain — that a forest formerly covered what is now the beach of the Baj' of St. Michel. The names of villages which stood in that forest have been handed down to us, and at low water traces of them may sometimes be seen. !Nowhere else in the world, the estuary of the Severn and the Bay of Fundy alone excepted, does the tide attain so extraordinary a height as in the Bays of St. Malo and St. Michel, where it rises 40, and even 50 feet. In the course of six hours it invades the beach of the latter bay, con- verting the rock of St. Michel, with its picturesque castle, into an island, ilan, however, has imdertaken not only to put a stop to the further encroachments of the sea, but also to recover some of the land already swallowed up by it. The interesting hill of Dol, with its numerous remains of prehistoric animals, formerly stood in the midst of the sea, but 3,500 acres surrounding it have been converted into productive land. Embankments 30 feet in height, and constructed since the eleventh century, now extend for a distance of 30 miles along the southern shore of the Bay of St. Michel, and the recovery of the sandy beach lying beyond 252 FEANCE. tiieni is not considered a hopeless enterprise. The greatest obstacle to this recon- quest is not offered by the sea, but by the rivers which flow into the bay, and for which an outlet must be provided. Elsewhere on the coast of Brittany man has had to guard against an invasion of moving sand-hills. The dunes of St. Pol-de-Leon are the most formidable, but having been planted with trees, they no longer cause anxiety. The sand com- posing these and other dunes in Brittany is unusually rich in carbonate of lime. Fragments of shells and seaweed enter largely into their composition, and the fraes, or calcareous sand, carried thither by the winds actually constitutes an element of wealth, being most useful as manure. Seaweeds are collected all along the coast, to be applied to the fields ; and in the bogs of Cancale and St. Michel the peasants annually take up 500,000 tons of Fig. 18G.— The Bay of St. Michel. Scale 1 : 500,000. ' WlofCr • 5 Miles. mud mixed with fragments of shells, which they spread over their fields. These fertilising agents are all the more appreciated as the crystalline and palccozoic rocks of Brittany contain hardly any lime at all. The fishing grounds of Brittany are amongst the most productive of France. The peasants of Quimper and Chateaulin formerly almost lived upon salmon, and farm-labourers objected to their being required to eat it more than thrice a week. Thousands of men are engaged in the coast fisheries, yielding herrings, sardines, mackerel, lobsters, and oysters : and Breton fishermen, inured to the hardshijjs of a seafaring life, annually visit the fishing grounds of Newfoundland and Iceland. Many amongst them work in the fields during winter, or collect sea- weed, but early in spring engage themselves as sailors on board the vessels proceeding to the Arctic regions. The four departments of Brittany supply the mercantile marine of France with one-fifth of its sailors. i; ' .„ LIBRARY OF THE UNIVERSITY of ILLINOIS. INHABITANTS. 268 INHABITANTS. The iubabitants of Brittany differ from (hose of the rest of France in laiigua^o, manners, and social condition. Kg. 187. — BuLTON Peasants. 4ymifi /I ill) lu Armorica, a remote region but little visited, ancient customs maintained themselves longer than in the more accessible parts of France, and the Druids enjoyed most power. Tlic modern Bretons arc no doubt, to ;i largo extent, the VOL. II. S 254 PEANCE. descendants of these ancient Armoricans, but kindred Celtic tribes, driven fi'om Great Britain through the invasion of the Anglo-Saxons, settled amongst them. These new arrivals founded the towns of St. Brieuc, St. Malo, and others. Being superior in intelligence to the aboriginal population, they soon gained a prepon- derance, and Armorica became Brittany, or Little Britain. The descendants of these immigrants still differ from other Bretons. They are tall, fair, and blue- eyed, these features being most prominent on the islands of Batz and Ouessant. The Bretons living to the south of the northern coast range are less tall, brown- complexioned, and have round heads ; but they, too, have dark blue eyes. Some of the inhabitants of the islands and of remote districts are said to be of a different Fig. 18S. — AiTuoxiMATE Extent op tub Bketon Tongue. fcSC 1^ Auri§ny Guernsey ^s'. '^ fi Gi-an\-itti •^* V ^*^ .■ l''W•.of Ci- origin. As a rule the Bretons bear a strildng resemblance to the Limousins and other inhabitants of the plateau of Central France. They have even been likened to the Xabyls of Algeria. Dr. Bodichon, himself a Breton, says that " the Breton of pure blood has a thick skull, a palish yellow skin, a brown complexion, black or brown eyes, a squat build, and black hair. He, like the Kabyl, is stubborn and indefiitigable, and his voice has the same intonation." The Celtic, or Breizad, spoken by the Bretons, is akin to Welsh. There arc four dialects, those of Treguier, Leon, Cornouaille, and Vannes ; and considerable jealousies exist between those who speak them, as is proved by imcomplimentary expressions like these : " A thief like a Leonard ! " " a traitor like a Tregorrois ! " 255 INHABITANTS. .< ablockhcad likoa Vanuetais ! " and " a brute like a Coruouailluls ! " "l"!- J>t-- ture of Brittany is poor, and cannot compare in antiquity or wealth with that ot Fi". 189.— Women- of Cascalb. •'-■::ji^;-^^UTS Irelmd or Wales. Only one weekly paper is published in Breton. Frencb is ;^:i.. Brest and tboLns generally, and ^ _^-;^^^:^2l^X tbe peasants, n>ost of whom can converse now vvUh the .entieme 256 FRANCE. formerly tLey hated so mucli. Still the boundary between the French-speaking Bretons, or " GuUots," in the east, and the Bretons projDer, has changed but little since the twelfth century. An examination of a map almost enables us to draw the lino dividing the two languages. On the one side we meet witli French names, or with Breton ones accommodated to French tongues ; on the other, with pure Breton names only, such as begin with abcr (month), cone (port, conch- shell), car, caiir, or /■<'/• (fortress, manor-house), coed, or coet (wood), Ian (conse- crated ground), loc (place, hermitage), leu (court of justice), mene (hill), inor (sea), penn (head), p/e, pk'ii, ov phir (people, tribe), ros (coast), &c. The manners of the Bretons, though peculiar in many respects, do not essen- tially differ from what may be met with in other remote localities of France. Brit- tany, iu fact, presents us with a fair likeness of mediasval France. As Michelet says, " The Bretons have only been estranged from us because they have adhered most faithfully to what we were originally ; they are not much French, but ver}' much Gaul." Old pagan customs still survive, and the peninsula of Pontusval, in Leonais, has been known as ar 2)(ifffiiiiz, or the " laud of the pagans," down to the present time. But there are many other parts of the province whei'e fountains and large trees remain objects of veneration, and the mistletoe has lost none of its pristine virtue. The ancient sanctuaries have been converted into chapels, but the old divinities survive under other names. Our Lady of Hatred, the patroness of a chapel near Treguier, is the Christian representation of a ferocious Celtic deity, whom women invoke to destroy a detested husband, and to whom children pray for the death of aged parents. St. Ives the Truthful, on the other hand, is appealed to as the defender of orphans and widows, and to redress all wrongs. Dolmens, or cromlechs, are revered as the tombstones of powerful men, and raised stones, which no peasant passes by without crossing himself, abound through- out the country. The peasants near Auray, when suffering from rheumatism, lie down on an altar, invoking the aid of St. Etienne. Elsewhere they rub the forehead with "sacred" stones when suflering from headache. Young people still dance around the dolmens, and married couples furtively touch one of these stones in order that their posterity may prosper. The great grave-hill near Carnac, 140 feet in height, is visited by sailors' wives to pray for their husbands. In 1658 the Breton clergj' solemnly declared that the devil alone could profit from food offerings placed upon these dolmens : since that time many of them have become objects of superstitious fear instead of veneration. Topography. MoRBiHAN is richer in ancient stone monuments than any other department ol Brittany, and its towns are more original in their aspect. Breeding cattle is of great importance. Heaths occupy a vast area even now, and most of the peasants keep bees. Eye, buckwheat, fish, and shell-fish constitute the principal articles of food. 3I0RBIIIAN. 267 The eastern portion of the department lies within the basin of the Vihiino and its tributary, the Oust. Eoclic-Beruard is a small port near the mouth of Uio Fig. 100. — LoniENT Asn Port-Lovis. .«calo I : 150,000. 4 ■.■f^, "f r^ ^/4 '^^/ J' JT'W.of Cr Vilaine, here spanned by a bold suspension bridge, which offers no obstacle to sailing-vessels proceeding up the river to Redon. Ploirmel (2,790 inhabitants) 258 FRANCE. is the principal town in the valley of the Oust, with remains of ancient walls and a church of the sixteenth century. Jossclin (2,522 inhabitants), higher up on the Oust, is commanded by a fine castle. A jDj-ramid, half-way between these towns, marks the site of the " Battle of the Thirty," fought in 1531, between the champions of Beaumanoir and Bamborough. Bolian, with ruins of a castle, has given its name to one of the most powerful families of France. Vanves (15,716 inhabitants), the capital of the department, on a creek of the Bay of Morbihan, resembles a large village rather than a town, but boasts of a museum rich in local antiquities. Auray (4,335 inhabitants), on another creek of the bay named, is famous on account of its oyster beds. The sardine fisheries occupy many of the inhabitants, and annually, at the commencement of the fishing season, a nautical procession is formed, headed by the priests, who solemnly bless the sea. A chapel near the town is much visited by pilgrims. In the neighbour- hood was fought the battle which terminated the Breton war of succession (1364). Port-Navalo and Loemarialcer are two villages at the mouth of the Bay of Morbihan. Near the former rises the artificial hill of Tumiac, 66 feet in height, and the latter boasts of a remarkable dolmen (see Fig. 8). Other dolmens of note are met inland, near the villages of Elccn (756 inhabitants) and Grand CJntmp (668 inha- bitants), as well as on the peninsula of Ruis, remarkable, moreover, for its mild climate. Around Sarzeau (840 inhabitants), the birthplace of Lesage, laurel-trees, camellias, myrtle-trees, and pomegranate-trees grow in the open air. The western portion of the department is drained by the river Blavet, rendered navigable as far as Fontivy (6,402 inhabitants), formerly known as Napoleon- ville, and consisting of a Breton quarter, with quaint houses, and the military blocks adjoining it. Vessels of 200 tons ascend the Blavet as far as Hoinrlont (4,844 inhabitants), miles above Loricnt (31,000 inhabitants), the largest town of the department, and its busiest port. The harbour of Lorient is accessible to vessels of the largest size ; and in the beginning of the eighteenth century, whilst the French East India Company existed, its commerce exceeded that of every other port of France. The company failed in consequence of the progress made by the English in India, and its ships, dockyards, and arsenal became the property of the State. It is still one of the five great military ports of France. The inha- bitants are much interested in the sardine fishery. Porf-Loids (3,262 inhabitants), at the mouth of the Blavet, is a dependency of Lorient. Its citadel has frequently served as a prison of state, as has also that of Le Palais (2,823 inhabitants), the capital of BeUe-Ile-en-Mer. FixiSTERE, or " Land's End," is the westernmost department of France. To its moist and mild climate it is indebted for its fertility, and jjlants grow luxu- riantly wherever there is soil to root in. The coast district, known as the " Golden Belt," is careftilly ciiltivated by small proprietors, but many of the large estates in the interior consist of barren heaths. Agriculture and the breeding of cattle and horses constitute the wealth of Finistere. There are also quarries of granite and slates, but the argentiferous lead mines are no longer worked. The fisheries are of considerable importance. FIXISTEEE. 259 Qiiimperlt; a pretty town of 4,080 inhabitants, is the first place met with on crossing from Morbihan into FinisttTc. Its port is accessible only to small coast- ins vessels. Then follows the village of ronf-Aieii, with nuiucrous windmills. Fig. 191.— COSCARSEAU. Scale 1 : 33.000. f "i I" i . J"....., IjMflcs. Concarneau (4,614 inhabitants), on the wide Bay of Fouesnant or Forest, is one of the great fishing towns of Brittany. Its maritime fauna is exceedingly rich, and an aquarium has been established to enable scientific men to study it. Qiiimper (13,879 inhabitants), the capital of Cornouaille, has a tidal harbour, 260 FRANCE. and boasts of a highly venerated cathedral, dedicated to St. Corentin. An agricultural college and a drainage and irrigation school have been established there. Quimper was the birthplace of Kerguelen, the navigator, and of Laennec, the physician. The surrounding country abounds in natural curiosities, and the manners of the inhabitants are very primitive. Bricc (482 inhabitants), a village to the north, is noted for its " double nags," which amble naturally. Pont I'Abb^ (3,827 inhabitants) is one of the most old-fashioned towns of Brittany, and at the village of Pcnmarch w£ meet with the ruins of a considerable town. Andlcrne (1,627 inhabitants) is likewise a decayed city, but Douanicncz (8,087 inhabitants) has become one of the principal quarters of the sardine fishery, which employs 800 boats and several thousand men. The wide Bay of Douarneuez is bounded in Fiff. 192.— Brest. the north by the peninsiJa of Crozon (824 inhabitants), beyond which a narrow gullet leads into the magnificent roadstead of Brest. Brest (66,828 inhabitants) is the most populous town on the Atlantic seaboard between Havre and N'antes, and next to Toulon the greatest naval arsenal of France. Its aspect, however, is very difierent from that of the delightful city of Provence. It is almost sinister, and from afar only uniform ramparts and cannon are visible. The estuary of the Penfeld, hardly more than 300 feet wide, forms the port of the town. On its right rises a castle of the thirteenth centuiy, very much older than the modern fortifications built by Yauban. The shabby buildings on the left contain marine stores. Passing beneath a swing-bridge, the estuary winds for more than a mile between stores, workshops, and ship-yards. Huge basins have been excavated in the solid rock, and a breakwater nearly a mile in length has recently been constructed. Steamers connect Brest with New York, but the commerce of the town is not of much importance. c6tES-DU-X0RD. 261 The vicinity of Brest and of its industrial suburb of Lambdzellec (2,243 inhabit- ants) abounds in remarkable sites. Ascending the Elorn, wo have Plougastcl-Daonlaa, with its orchards and market gardens, on the right, and reach Landcrneau (G,fl65 inhabitants), with a largo linon-mill, and St. JUarfi/rr, famous on account of its horse fairs. The river Aulno, which likewise enters the road of Lrest, leads past Le Faou and. Port-Lauiiai/ to Chuteanlin (2,211 inhabitiints), near which are slate quarries. On the Aven, a tributary of the Aulne, stands Car/iaix (2,296 inha- bitants), the Eoman Yorganium, where seven roads meet. Passing through the narrow gullet which connects the road of Brest with the open Atlantic, wo notice Camaret, an old outport, on the left, and the small creek of Miiiou, the terminus of an Atlantic cable, on the right. Doubling Point St. Matthicu, surmounted by the ruins of a church, wc pass in succession Coiiquct, a favourite bathing-place ; Aber-Ilduf, where there are granite quarries; Aber-BcnoH ; awA Abcr-Wiach. Lesneven (2,437 inhabitants), near which is the church of Folgoet, much frequented by pilgrims, lies some distance inland. Morlaix (13,019 inhabitants), on the Dosscn, has a tidal harbour, and vessels of several hundred tons arc able to anchor close to the stores and manufactories which line both banks of the river. The most remarkable building of the town is a rail- way viaduct, which, at a height of 190 feet, passes over the river and the houses of the town. Moreau was born at Morlaix in 17G3, and the traveller Lojean is a native of Plouegat-Gucrrand, near Lanmeur, to the north-east of the town. Descending the river, we pass the castle of Taureau, on an island at its mouth, built in the sixteenth century as a defence against the English, but now used as a prison. St. Pol (3,503 inhabitants), the old capital of Leonais, has two magnificent churches, but has otherwise lost all importance. The environs, protected by embankments, are exceedingly fertile. Roscoff (1,282 inhabitants), the old harbour of L^onais, is known on account of a fig-free, which has grown to extraordinary proportions. The vegetables grown around it are exported to Paris, London, and Rotterdam. The sea abounds in fish, and a zoological station, similar to that at Concameau, has been established. C6tes-du-Xord, " north coast," is for the greater part carefully cultivated by a multitude of .small proprietors. Agriculture and cattle-breeding are the leading occupations. A manufacturing industry can hardly bo said to exist, and there are no great commercial ports. Loiideac (2,091 inhabitants) is the principal town in the southern portion of the department, which drains into the rivers Blavet and Vilaine, and is covered to a large extent with furze. Corhnj, a village to the north-west of it, is noted for its horses, said to be the descendants of Arabs introduced during the Crusades. Lannion (G,llo inhabitants), in the delightful valley of the Guer, close to the frontier of Finistere, has a small port. There are several curious old buildings. The river Jaudy enters the sea farther west. The tide ascends it as far as the famous old city of Triyuier (3,G11 inhabitants), with a cathedral of the fourteenth century. Doubling the dreaded headland known as the "Swords" (Epees) of Treguier, we arrive at the mouth of the river Trieux and the small port of 262 FEANCE. Lezardricux (516 inhabitants). The tide ascends as far as Portrieux (2,192 inha- bitants). Higher up on the river is Guiiigamp (7,895 inhabitants), with an old citadel. Returning to the coast, we pass the island of Brehat, inhabited by a superior race of men, whom consanguineous marriages have not injuriously affected, and the small fishing ports of Paimhol (1,576 inhabitants), Brehec, St. Quay (984 inha- Fig. 193.— MoRLAix. Scale 1 : 200,000. S Fathoms lo Fathoms s^ Faihome ij Fathoms ^^^^____ 2 Miles. bitants), and Bink (1,110 inhabitants) ; and entering the river Gouet, ascend with the tide to the tidal harbour of St. Brieuc, (13,683 inhabitants), the capital of the department. The town is not remarkable for its buildings ; but its inhabitants, known as Briochins, engage in the manufacture of textile fabrics, and carry on a considerable trade with agricultural produce. Hundreds of men find employment in the granite quarries in its neighbourhood. St. Quinfin (3,218 inhabitants), on cOtes-du-nobd. 203 the I'ppcr Goiict, is noted for its liiicu industry, which was much more important formerly. At Pledran, a small village 6 miles to the south-oast of St. Brieuc, may be seen the curious ancient camp of I'eran, with vitrified walls. Lamballe (4,"2-18 inhabitants), the old capital of the duchy of rciithievre, lies on the road to Dimn (7,978 inhabitants), tho easternmost town of the department, Fig, 194. — St. Malo and St. PEnvAX. Swilc 1 : 80,000. 4°|t5'Wof P«ri« .•|5'Wof C7 picturesquely situated on the banks of the river Ranee, which lower down flows past St. Malo. An old castle, now used as a prison, crowns a hill near the town ; a magnificent viaduct spans the river ; and the heart of Dugucsclin is preserved in the Gothic parish church. A granite pillar, 10 miles to the south-west of the town, marks the site of the castle of La Mottc-Broons, in which Duguesclin was born (1321). Dinan has tan-yards and sail-cloth factories. Its mild climate has attracted many English residents. 264 FEANCE. Ille-et-Vilaixe. — The greater portion of this department is drained by the river Vilaine and its tributary, the lUe, and only an inconsiderable part of it borders upon the British Channel. Agriculture and cattle-breeding are the prin- cipal occupations; bee-hives (160,000) are more numerous than in any other department in France ; and at St. Malo and elsewhere on the coast fishing and navigation occupy many of the inhabitants. Si. Mah (10,061 inhabitants), at the mouth of the Ranee, is the great seaport of the department, separated from its more ancient sister city of St. Scrvan (9,912 inhabitants) by extensive wet docks. The tides sometimes rise 50 feet, and the Fisr. 195. — View of St. Malo. sea alternately advances up to the quays and retires for a considerable distance, completely changing the aspect of the two towns. The inhabitants of St. Malo, or Malouins, have at all times enjoyed a reputation as bold seamen, engaging in com- merce or piracy as opportunities offered themselves. Four expeditions were fitted out in England to burn the town, but they failed. The Malouins became so wealthy that they were able to lend 30,000,000 francs to Louis XIV. They are enterprising and persevering, and somewhat haughty. Lamennais and Chateau- briand were both natives of the town, and are amongst its most distinguished representatives. The commerce of the two towns is no longer what it used to be, in spite of fine docks and railways. About eighty vessels are engaged in the New- ILLE-ET-VILADTE. 2G5 foundland fisheries, and provisious in largo quantities are exported to the Channel Islands and England. The town attracts numerous seaside visitors. Caiicak (3,269 inhabitants), on the western shore of the Bay of St. Michel, has famous oyster beds. They yielded 120,000,000 in 1802, but only 15,500,000 in 1875. At Lc VirUr, on the same bay, oyster- breeding is carried on successfully. Doi (3,517 inhabitants), a famous old town with a fine Gothic church, lies a short distance inland. Xear it stands the famous menhir of ChamiJ-Dolent, surmounted by a cross. Coiiihoiinj (1,491 inhabitants), with a castle in which Chateaubriand spent several years of his youth, lies to the south ; Fouglns (I0,39ti inluibituuts), on the Upper Couesnon, in the south-east. The town retains its old castle, but the mediaeval fortifications have been razed to make room for suburbs. Shoemakiug, weaving, and the quarrying of granite occupy thousands of men in the town and its vicinity. At St. Auhin-du-Cormwr (1,15U inhabitants), in this neighbourhood, was fought the battle which resulted in Brittany becoming a French province. Crossing the water-shed separating the rivers flowing into the channel from those taking a southerly course, we reach Reiuics (53,598 inhabitants), the capital of the department, at the confluence of the lUc with the Yilaine. Four railways and eleven highways converge upon the town, and a canal connects the navigable lUe with the river Eance, which enters the sea at St. Male. Its coimncrcial advantages are consequently very great. The aspect of the town, with its houses built of greyish granite and deserted streets, is nevertheless very dreary. The gate of Mordelaise is the most interesting monument of the Middle Ages, but a fine university building, with valuable scientific and art collections, constitutes the glory of the place. Rich meadow lands surround the town, and the butter known as Pi'cvalaye is named after a castle in the neighbourhood. VUr6 (8,475 inhabitants) is a picturesque old town on the Upper Vilaine. Madame de Sevigne resided for a considerable time at the castle of liochcrs, to the south-east of it. Descending the Vilaine below Rennes, and passing through its gorges, we reach Rcdoii (4,955 inhabitants), at the mouth of the Oust, and on the canal which connects Nantes with Brest. Other places of interest in the depart- ment are Montfort (1,507 inhabitants), on the Men, a tributary of the Vilaine, with an old castle ; Pdiwponf, in the famous forest of Broceliaude, one of the reputed haunts of Merlin the enchanter ; Janze (1,03G inhabitants), to the south- cast of Kenues ; and La Guerche (2,612 inhabitants). CHAPTER IX. THE CHANNEL ISLANDS. HOUGH a political dependency of England, these islands geographi- cally belong to French Normandy. Their soil, climate, produc- tions, and inhabitants are the same, and in their customs and political institutions they are even more Norman than Normandy itself. Magistrates there still raise the " hue and cry " {chdncnr de haro), as was formerly done by the people when wronged by the great, and the legislative body is still known as coliui'. If we would study the institutions of feudid Normandy wo cannot do better than go to the Channel Islands. Ever since they sided with John Lackland against Philip Augustus, in the thirteenth centurj^, these islands have almost uninterruptedly enjoyed the blessings of peace, for their neutrality was guaranteed. England very wisely lefc them in the enjoyment of their local institutions, and can boast of no subjects more faithful than these islanders. The islets, rocks, and banks off Granville have remained in the possession of France, but only a few of the larger islets of the archipelago of Chausey are inha- bited throughout the year. A few acres there are cultivated, but fishing is the jirincipal occupation, and the sea yields a rich harvest of fish, shrimps, and sea- weed, but there are no oysters. Quarrying also is carried on extensively, and the streets of Paris are for the most part paved with Chausey granite. The storm- beaten rocks of Minquiers and the Grelets, farther out, are only occasionally visited by fishermen from Granville or the Channel Islands. Jkksey* — that is, the island of Jcrs, or Cccsar : historians have identified it with the Cassarea of the Antonine Itinerary — is the largest of the group. In shape it is a parallelogram, its length being nearly twice its breadth. The cliffs along its northern shores have offered more resistance to the onslaughts of the Atlantic, and from their summits (350 feet) the island slopes down to the south, nearly all its rivulets flowing into the Bay of St, Aubin. On ascending their shady valleys up to where they rise, we find ourselves upon the summit of the cliffs, with a grand outlook over the ocean. * Jersey has an area of 45 square niiles, and 56,627 inliabitants ; Guernsey and the smaller islands have an area of 28 square miles, witli a population of 33,968 souls. THE CHANNEL ISLANDS. 207 The southern and westeru coasts of the island exhibit many traces ot' the erosive action of the ocean. Ledges of rock and sand-banks, which in former times were dry land, stretch for a mile or two from what is now the hi-^'h-wuter line ; Fig. 196. — The Ciiaxnll I:.lam>s. Sculo 1 : ?00,000. S'lWofParu '' 'f f^p'tteJiiBiifi- I.U.. M<- \ lAU)l'.R5fK\ :,;)tL GrERN'SKy 1^ .K*r«JioTi S I'KHM.t .... 10 KLdu^ttlM ^7 fadwm* 10 MUca. and the cliffs vof Corbiere have been gnawed into curious pinnacles and pillars, and pierced by caverns. The heights surrounding the beach of St. Ouen, in the west, are covered witli shrubs which bend to the storm. Dunes exist in taut purtiou of 268 FEANOE. the island, and they have occasionally overwhelmed cultivated fields, as a punish- ment, local tradition tells us, for the massacre of shipwrecked mariners. Except in the north and west, where the brine-laden air destroys the vegeta- tion, the island is naturally fertile, and being blessed by a mild climate, it pro- duces fruits and vegetables of excellent quality. Its cows ai'C highly valued, and cattle imported from France are invariably slaughtered for butchers' meat. There are a few dolmens recalling prehistoric ages. Locally they are known as poquclaijcs, a name recalling that of the ^'oii/picaiis, or dwarfs, of Ai-morica. Skeletons and coarse cincreal vases have been found at the foot of some of these ancient stone monuments. Norman-French is still the oflScial lan- ffuasc of the island, and Wace, the author of the famous " Roman de Ecu," was a native of " Jersui." Within the last fifty years a large number of English have established themselves upon the island, attracted by its mild climate and the cheapness of the necessaries and luxuries of life. These wealthy immigrants have gradually changed the physiognomy of the inhabitants and of their houses; and, when passing through the streets of St. Helier, we may almost llincy being in an English town. During last century the Jerseyites were attached to England only Ijolitically, but at the present day we must look upon them as members of the great English family, in spite of the vicinity of France and the many Frenchmen domiciled upon the island. The castle of MontorgncU, on the eastern coast of the island, was its old capital, the fishing village of Gorey nestling at its foot. St. Uclier (16,715 inha- bitants), the modern capital, stands on the vast Bay of St. Aubin, on the south shore of the island, and is quite English in its aspect. Two forts defend its harbour, from which the sea retires during low water. Large vessels anchor in the road- stead of St. Aubin, but an artificial harbour, covering no less than 380 acres, has been in course of construction since 187-1. St. Auhiii, which was the more impor- tant place formerly, is hardly more now than a suburb of St. Holier, with which it is connected by rail. Sekk, whose granite cliffs rise boldly in the channel which separates Jersey from Guernsey, consists of two portions, joined together by a narrow and precipi- tous neck of land. Its cliffs rise to a height of IGO feet, but access to its fertile and smiling plateau is facilitated by means of a tunnel. Eabelais, in " Panta- gruel," calls it the island of pirates, thieves, brigands, murderers, and assassins, but its present inhabitants are peaceable enough. Guernsey, the Sarnia of the Romans, and probably the Groens-ey, or green island, of its Scandinavian conquerors, is deserving of its ancient name. Though less carefully cultivated than Jcrsej-, green meadows, elms growing in the hedges, and apple orchards impart to it the aspect of a wooded country. The general slope is towards the north-east, the boldest promontories rising at the western extremity. Less frequently visited than Jersey, the inhabitants have remained more fliithful to their ancient customs. Small, sunburnt, with black eyes, and thick brown hair, they strike one as being true representatives of tlie Breton race. THE CHANJfEL ISLANDS. 269 Many Celtic expressions are used by them, and until quite recently they looked with superstitious awe upon the dolmens, cromlechs, and menhirs scattered over their island. They are old rivals of their neighbours on the larger island, and, when these latter sided with the Parliament during the Commonwealth they stuck firmly to the King. St. Peter's Fori (16,150 inhabitants) occupies a sheltered situation on the east coast. Its harbour is accessible at all times. Granite, quarried in the vicinity, is the principal article exported, and there are large stores of wine. Aldernev (Aurigny) is separated from the coast of France by the strait of Raz Blanchard, only 10 miles wide, but much dreaded by mariners. Steep cliffs rise on the south, and the island slopes down towards the north, where there are numerous creeks and small baj-s. The most considerable of these, that of Braye, was to be converted into a huge harbour of refuge, similar to that on the coast of England opposite, but the works have recently been stopped, in spite of the vast sums already expended on them. The formidable rocks known as the Casqucts, to the west of Alderuey, are rendered conspicuous by lighthouses. The political institutions of the Channel Islands are still feudal in their character. The seigneurs are vassals of the Queen, the "sovereign lord of the land," and annually do homage to her at a ceremonious " assize of heritage." Their privileges are still considerable. The Legislative States of Jersey consist of thirty-eight members, viz. the governor and the bailiff of the Royal Court, both appointed by the Crown ; the twelve judges, or jurats, of the Eoyal Court, elected for life by the ratepayers ; the twelve rectors of the f)arishes, appointed to their livings by the ratepayers ; and the twelve constables, elected every three years, one for each parish, by the inhabitants. The riconte, or high sheriff, and the two iteiioiiciaieiirs, or under-sheriffs, occupy seats in the Assembly as its officers. No taxes can be levied without the consent of the States. The revenue of the island amounts to £22,000, and there is a debt of £160,000. In Guernsey there are " States of Deliberation," composed of the bailiff of the Royal Court, who is president ; the procureur, the ten rectors of the parishes, the twelve jurats or judges of the Roj'al Court, and fifteen delegates elected by the rate- payers. The bailiff and procureur are nominated by the Crown ; the jurats are chosen by " States of Election." VOL. II. CHAPTER XI. THE VALLEY OF THE SEINE. The River Seine. EOLOGICALLY this is a well-defined portion of France. It covers three-fourths of an ancient gulf of the sea, Paris being in its centre, and the coasts of former ages can still be traced in many places. Calcareous rocks, overlying the schistose plateau of the Ardennes on the one hand, and the granitic mountains of Morvan on the other, bound the basin in the east ; rocks belonging to the same formation separate Beauce and Lower Normandy from the palasozoic rocks of Brittany in the west ; and only in the south does this geological basin extend beyond that of the Seine and embrace a portion of that of the Loire. Historically this ancient country of the Sequanians has at all times proved itself the natural centre of France, towards which converge the roads from Belgium and Germany, from Southern France and the Atlantic. Add to this a favourable climate, and we need not wonder at the Seine holding a rank amongst rivers quite out of proportion to its volume. The Seine, so called, rises on the north slope of the Cote-d'Or, but its real head-stream must be looked for in the granitic and porphyritic district of Morvan. This district forms the northern buttress of the plateau of Central France. Though . nowhere exceeding 2,960 feet in height, its aspect is sometimes Alpine, and its valleys fertilised by the debris carried down by the torrents, are verdant with vegetation. Swamps (ouches) have been converted into fields, and yield harvest after harvest ; but the forests, to which these mountains owe their Celtic name of Morvan {i.e. "black mountains"), have to a great extent been destroyed. Pic- turesque clifils, perched upon which are the towns of Vezelay, Avallon, and Semur, terminate the district of Morvan in the north. The bare chalky hills beyond these, as far as the plain, are attractive only in summer, when the apple-trees are in blossom. The aspect of the comitry is more varied in the north-east, where the hills of Cote-d'Or, the jjlateau of Langres, and the Faucilles ("sickle mountains"), form the water-shed as far as the Vosges. Some of the valleys in that part of Burgundy GENERAL ASPECTS. 271 Cotentin are bare, and the country owes all its attractions to the vicinity of tho ocean. The plains to the east of BoCage, irrigated by tho Orno, the Dives, and the Touques, are a pastoral country. Bessin, to tlio east of tho Vire, comprises many marshes now under cultivation. Tho vast meadows around Isigny might remind us of Holland, if it were not for tho rows of willows, poplars, and trees which intersect them, and the low embankments covered with hawthorn and brambles. The plains of the Orne and of Calvados are admirably suited for the breeding of horses and the fattening of cattle. The iinest grass, however, is reserved for the Fig. 197. — Tub Foeest op A.ndainb. Scale I : 330,000. El !o'. Wiif r^ 5 Milea. choicer breeds of cattle and for milch cows. The cheese and butter made enjoy a high reputation. None of the rivers, not even the Vire or the Orne, are nangable farther than the head of the tide. Subterranean river channels are frequent, as in other lime- stone regions. Several " sinks," or hetuirs, occur in the bed of the Aure, and only in winter is the volume of the river sufficient to flow on the surface a feeble stream. The Lower Aure is fed from subterranean channels, but it, too, is partly swallowed up by sinks, and at its mouth forms a delta, one arm of which reaches the sea through an underground channel. The granitic cliffs of Cotentin resemble those of Brittany : exposed to the attacks of conflicting tides, they have been destroyed in many places. The wide t2 272 FRANCE. Bay of St. Michel, to the south of Granville, has thus been formed. Elsewhere the deep bays, or flieurs (a corruption of the Scandinavian word fjord), have been silted up. The promontories forming the extremities of the peninsula do not mark its ancient limits, for Alderuey and other islands were formerly attached to it. The conflicting tides give rise to phenomena resembling the maelstrom. The Raz Blanchard, between Cap de la Hague and Alderney, sometimes rushes along like a mighty river at the rate of 10 miles an hour. The current known as La Fig. 198. — Meadows of Normandy. D^route, farther south, though less swift, has nevertheless proved the destruction of many a mariner. The aspect of the limestone cliffs of Calvados is very different from that of the granitic rocks. These soft rocks have been gnawed away more regularly by the waves, and their debris now forms broad beaches, surmounted here and there by rocks, anciently portions of the mainland, and still offering some resistance to the waves. Topography. La Manche includes the peninsula of Cotentin, together with adjoining portions of Normandy. Though bounded on three sides by the sen, the maritime commerce T.A M.VNCHE. 278 of this department is not of much importunco ; industry is even less so ; iind the population depends almost exclusively upon H<»ricul(ure for its sustenance. Tho soil is not very fertile naturally, but tho small proj)rietor8 who share it have done much to improve it. Tho moist and warm climate is favourahlo to the growth of herbs and grasses, and tho breeding of horses and cattle is carried on with much success, more especially in the east. Some parts of tho department resemble huge orchards, and about ^8,t"-^ l°i37'\V.otCr. Fut, 5 Fa4?U>7rM . 1 MUe. to 1802, who thus intercepted all communications between Havre and Cherbourg. Valognes (4,910 inhabitants) lies in the centre of the peninsula of Cotentin, and at the mouth of the Douve. In the midst of marshes converted into fertile meadows stands Carentan {2,n'2 inhabitants), which exports dairy produce to England. St. L6 (9,519 inhabitants), the capital of the department, occupies a delightful site in the valley of the Vire, and carries on some textile industry. Returning to the western coast, the first place we arrive at is Coutances (Constantia, 8,008 inhabitants), an old episcopal city which has given its name to the entire peninsula. Its cathedral is a fine structure of the fourteenth century. Regneville, the port of Coutances, has oyster beds. Higher up on the Sienne is Vilkdieu-les-Poeles (3,437 inhabitants), a town of tinkers and frying-pan makers, as is implied by its name. OUNE. 275 Grancille (12,372 inhabitants) has an excellent harbour and docks, and carries on commerce with the Channel Islands and England. The inhabitants arc sup- posed by some to be of Iberian descent, and such a thing as slander is said to be unknown amongst them — a very curious circumstance for a provincial town. Arranches (7,754 inhabitants), the old town of the Abrincates, occupies an admirable situation at the mouth of the See. It boasts a fine catheallc-ni-lli- I'.TM-viUe" {>'.' Honoi Tt ■^ . ■• MilM. of muny fine buildings, most of tbcm constructed of tbe famous stone quarried in the ncigbbourbood. The Byzantine cburcb of St. Pierre, at tbo foot of tbe old castle, bas a fine Gothic spire. The abbey of St. ^Itienne, in which William tbo Conqueror was buried, is distinguished by its simple grandeur, and bas a nave of 278 FRANCE. the eleventh century. Many of the other ecclesiastical and private buildings are remarkable on account of the architecture. The " sapient " city may boast of numerous educational establishments, and its library and museums are amongst the wealthiest in France. An active commerce is carried on, and the docks admit vessels drawing 16 feet of water. Ouistreham, at the mouth of the Orne, Fig. 203.— Trouville. Scale 1 : 50,000. 1 Mile. was the great port of the country in Anglo-Norman times, but is now a simple village, much frequented as a seaside resort, as are also other villages near it, amongst which Courseiillcs, with a small port and oyster beds, is the most important. In a side valley of the Ujjper Orne is Conde-sur-Noireau (6,835 inhabitants), with cotton-mills. The river Dives, on entering the department, is joined on the left by a small CALVADO& 279 tributary, commanded by the curious old city of FaUtise (8,180 inbubitanta), in whose castle was bora AVilliam the rinujucror. Tboro are cotton-mills and horso fairs, called after tlio suburb of Guibruy. At Dins, now a poor village at the mouth of the river, the Conqueror embarked the army of 2oi>,000 men with which he invaded England. Licarot, in a side valley of the Dives, is noted for its cheese. Lisieux (18,396 iuhabitiints) is the most important town on tlie Touques. Its fat meadows nourish cattle for the Paris market, and cloth, leather, and cotton stuffs are amongst its principid manufacturing products. A Gothic cathedral is its most remarkable building. Crhrcoiir, noted for its fowls, is near. Poiil- fL'reque (2,373 inhabitants) exports cheese and vegetables. Trouville (5,161 inhabitants), at the mouth of the river, is one of the most fashionable seaside resorts of France, annually frequented by 20,000 bathers ; but the town also carries on some commerce. The castle of Bouurrillf, at the neighbouring village of Touques, was a favourite residence of "William the Conqueror. Houfleur (9,037 inhabitants), at the mouth of the Seine, opposite Havre, rises amphithcatrically from the water-side. It was an important place formerly, before it had been eclipsed by its parrenu rival on the opposite bank of the river, and its mariners roamed over every sea. Its port has been silted up, but it still exports vast quantities of vegetables, fruits, poultry, and eggs, more especially to London. Fishing and ship-building are also carried on, and the gardens produce excellent melons. CHAPTER X. LOWER NORMANDY AND COTENTIN. General Aspects. HOUGH small in extent, this section of France has made its influence felt in the history of the country. From ancient times it has served &a the intermediary of commerce and ideas between France and Great Britain, and from its shores departed, in the eleventh centurj', the Norman conquerors of England. The inhabitants differ in physique from those of other parts of France, for the Norman conquerors maintained their ground longer there than elsewhere. Bayeux was ceded to them in A.D. 923, or twenty-five years later than Rouen, but they came to the former in larger numbers, besides which the Saxon Baiocasses or Sesnes of Bayeux, speaking a kindred dialect, had jDreceded them. The local dialect contains many words of Teuton origin, such as j(iV 0°|I.O'U' , 1 MUe. whether the supply of water is more or less ample, and it happens frequently that the tutelary statue erected by the city of Paris is not reflected in its crystal waters. The stream only becomes considerable about 15 miles farther north, where it is reinforced by two beautiful springs rising on the plateau to the west. At Chatillon, 30 miles below the " source," another douix, or spring, unites with the river, which lower down is joined by the Ource and the Laignes. The whitish Aube, rising in the chalks of Champagne ; the Voulzie, running through a delightful valley ; the Loing, the sparkling Essonne, and other tributaries flowing on regularly throughout the j'ear, difier essentially from the torrents TUE RIVER SEINE. 288 which join the Upiier Yonne. No less than 7.5 per cent, of the surface of the basin of the Seine consists of permeable rocks, and this, together with the character of the tributaries mentioned above, accounts for the Seine bemg that river of France whose volume undergoes the fewest changes during the year. Of course there are exceptions; and quite recently, in the spring of 1876, the Seine Fig. 206. — The Soubcb op the Selse. Scale 1 ; 80,000. 24E.«rP«rl. J S'. Ctrnwiii -^ In Frnillr ra''.-i'. • '• ■'":'■ ,1- ft --'■ ' '( :' J 1 V 'if:. Blis!h V-/C- Sec l!^>\ ^V ( ) ' • ' - i^^'; V ^"E-oif-r MUc. overflowed its banks and caused much destruction. On the 17th of March no less than •08,'273 cubic feet of water passed every second beneath the bridges of Paris, being fifty times more than when the river is at its lowest. But the difference, after all, is little compared with what may be witnessed in connection willi tlie Loire and the rivers of the south. M. Belgrand has shown, however, that during 284 FRANCE. a geological epoch coinciding with the stone age, the Seine, too, had its floods, its volume sometimes exceeding 1,000,000 cubic feet a second. The Marne, which joins the principal river at the very gates of Paris, is of greater length than the Seine, but its volume is less, and nowhere within its basin does the annual rainfall exceed 24 inches. Between Epernay and Meaux the annual precipitation only amounts to 16 inches, and most of the rain is sucked up by the soil. This small amount of rain, however, is not attended by sterility, for that portion of the Champagne known as " lousy," on account of its Fig. 207. — The Basin op Vitey-le-Fkanjois. Scale 1 : 320,000. z^lSo'E. of Pains !,» So- E of Or . 5 Miles. barren rocks, its short herbage, poor fields, and poverty, lies to tlie east of this " rainless " region. In spite of the greater precipitation, it contains tracts fitly to be described as " steppes." Upon one of these the camp of Chalons has been established. The zone of chalk is widest in that part of France, and the cultivators of the soil have to sustain a severe struggle. Only where marl occurs naturally or is applied to the chalky soil can fine crops be raised, and such localities form oases in the desert. The Marne, now discharging 2,G50 cubic feet a second, was a far more considerable river in prehistoric times. All the rivers rising in the THE RIYEE SEINE. 285 Jurassic heights and converging upon Paris have denudetl a considerublo portion of the area which thoy drain. In this manner a wide phiin of erosion, enveloped by the cretaceous rocks of Champagne, has been formed. "Within it lie the towns of Auxcrre, Bar-sur-Seine, Bar-sur-Aube, Vitry, Bar-lc-Duc, and Sto. Menehould. M. Elie de Beaumont has likened this plain to the ditch of an exterior lino of the fortifications of Paris, the hills of Brie forming the rampart. In tho formation of this plain the Marne has had the greatest share. Tho basin of Vitry-lo- Francois, within which the two head branches of tho river join, affords one of tho finest examples of the action of water as a geological agent. Over an area of 200 square miles the cretaceous rocks nave been carried away, and alluvial soil conveyed down from the hills has been deposited instead. On approaching Paris, the Marnc meanders in numerous curves, taking its course through a valley the delights of which have been the themes of poets and painters, and which has been encroached upon by the villas and summer houses of the citizens of Paris. The Ourcq, one of the affluents of the Marne, has partly been diverted to feed a canal which supplies Paris with water, and is at tho same time navigable. The last curve of the Marnc is of recent origin. Formerly the Marne bifurcated Fig. 208. — Section of the Paris Basin. HorizoDtal Scale 1 : 6,000,000. Vertical Scale 1 : 100,000. Vpsges _^ormiii(iy Hu,qx>: Horizontal Sr^^ l:it>'ito^£>fi. below Meaux, the northern arm flowing through the depression in which runs the canal of Ourcq, whilst the southern joined the vast lake which then covered the basin of Paris, and above which rose the islands of Slontmartre, Passy, Stains, and Ormesson. Nor had the three curves which the Seine describes below Paris any existence, their future directions being merely indicated by the promontories of Vanves, Mont Valerien, and St. Gei-main. The Oise, which joins the Seine above Poissy, is commercially an important river, for it rises near the coal-fields of Belgium, and traverses a region distin- guished for its industry. Locks render it navigable throughout, and canals join it to the Marne, the Mouse, the Scheldt, and the Somme, one of them, that of St. Quentin, passing through several tunnels. The valleys of the Seine and tho Oise meet at right angles, embracing between them the huge quadrant of a circle, tho centre of which is at Paris, whilst the periphery is formed by the Jurassic zone extending from Burgundy to tho Ardennes. Tho geological formation of tho basin of Paris may here be studied most advantageously, the degrading action of the water having been least. Geologists have likened the successive beds of this basin to a number of basins placed one within the other. Where impervious VOL. 11. u 286 FEANCE. layers of clay prevent the passage of water, the latter collects underground, and thus the rain which falls on the chalky plateaux of Champagne finds its way to the surface through wells bored at Paris. The artesian springs at Grenelle rise from a depth of 1,640 feet. Beneath the Seine which flows on the surface there are other Seines far underground. Beneath the Lake of Eughien, which occupies a cup-shaped cavity in the marl, there are other lakes, which may be tapped, when their water rushes up to the surface. About one-half of the rain falling within the basin of the Seine finds its way into the river, the other half feeding subterranean reservoirs. No large tributaries join below the Oise, but the Seine nevertheless increases in volume, for numerous springs rise in its bed. Below the confluence with the Eure the influence of the tide makes itself felt, and the river is of imposing width. The ancient gulf through Fi". 209. — The Estuary op the Seine. 2-15- rw.ofrjrii 4 Miles. AUuvud Lanit TecovereA, froni t}ic Sea,. CdelaHeVv, '4 L'Ecln/l --l-fH',. LE ti^VRE X^ TRocvai O'l&'E-of Grgcnw which it flows is for the most part bounded by sloping hills, but a few old chalk cliffs, formerly bathed by the sea, may still be seen. Below Rouen the Seine forms curves similar to those near Paris. Beyond Quillebceiif it is confined within embankments. The phenomenon of the bore {mascard) may be witnessed above that town as far as Caudebec. A tidal wave, 10 feet in height, then rushes up the river at the rate of more than half a mile a minute, and the conflict between it and the river is most imposing. The bay of the Seine has been much changed in consequence of engineering works. The mouth of the river is now 10 miles below Quilleboeuf, opposite the Cap du Hode. The embankments are flooded at high water, and behind them the sea deposits the mud held in suspension. When these deposits have attained the height of the embankment the latter is increased in altitude, and the land thus protected may be cultivated. The estuary of the Rille, which joins that of the UPPER NORMANDY. 287 Seine on the south, is eflfeetiiuUy treated in the siinio niiinner. Like niiiny other rivers traversing ciileareous formations, the Rillc, or Risle, flows partly through underground channels. TJPPEII NoUMAMJV. The plateaux of Upper Normandy, which extend from the northern bank of the Seine to the English Channel, where they terminate in Capes do la Tlevc any ^MlpTevSk i Aubervihe 2 Miles. The maritime slope of this plateau is intersected by numerous vaUeys or river- less dales. The parallelism of the rivers is remarkable : the B^thime, the Yeres, the Breslo, and the Somme all flow in the same direction, dividing the country into regular parallelograms. The roads either run along the valleys or at right angles across the intervening plateaux. Most of the towns have been built lengthways along the roads, running towards the north-west. They have hardly any side streets ; and one village, that of Aliermont, near Dieppe, forms a single street nearly 10 miles in length. The right slope of most of the valleys of Upper Normandy is steeper than that on the left. M. de Lamblardie ascribes this curious feature to the greater rapidily with which evaporation takes place on the slopes exposed to the sun. The slopes THE COAST. 289 facing northward arc more humid, and the disintegration of (he rocks would consequently go on at a more rapid rate. The rotation of the earth, however, is sufficient to account for this phenomenon. The Coast. The undisturbed action of geological agencies in this part of Franco is exhibited by the formation of the coast, no less than by that of the plateau. The shore between Ilavre and Dieppe forms a convex curve, and is continued thence to Fi?. 212.— Cape de la IlfevB. I3oulognc and Cape Gris-Xcz by a concave one. The contour of this coast-line is most graceful, and yet few localities exist where the sea has wrought greater havoc. Between Havre and Auet, a village to the south of the Somme, bold chalk cliffs line the coast, sometimes rising to a height of 300 feet, and only interrupted at intervals by breaks through which the inland waters make tlicir way to the sea. Sometimes, when the storm rages, masses of rock wcigliiiig thousands of tons are detached, and gradually worn down into sand. The rain-water which filters through the fissures of the rocks is even a grcatet 290 FEANCE. ao-eut of destruction than the sea. The lower portion of the cliffs generally consists of ferruginous sand, through which percolates the water of many springs. Cavities are thus formed, the superimposed mass of rock settles down, and at the next onslaught of the waves tumbles down upon the beach. The sea here con- tinually encroaches upon the land. In the beginning of the twelfth century the church of Ste. Adresse stood 4,600 feet from the present coast, at a spot now occupied by the bank of £clat. The sea has consequently advanced at a rate of about 8 feet annually. This rapid progress is due in a large measure to the coast current, which carries away the debris of the cliffs. For a time the fragments of rock which tumble dovm. from the top of the cliffs form a protective barrier ; but by degrees the chalk dissolves, and is carried to a distance, whilst the enclosed pebbles, unable to contend against the waves, are distributed along the beach, and even aid in the work of destruction. The ports, moreover, are being silted up by pebbles and mud carried down by the rivers, and require the protection of piers. At the Cape of Antifer the ocean current bifurcates, the principal branch run- ning east along the coast of the countrj' of Caux (calx, lime), whilst a lateral arm turns south, in the direction of Havre. The port of that town is thus threatened from various directions. The ocean current transports thither its pebbles ; the debris carried down by the Seine gradually silts up the estuary of the river ; and the rivers of Calvados convey thither the sands and pebbles of Lower Normandy. The efforts of the engineers to avert the fate threatening the port, and which has already overtaken Honfleur, on the left bank, are incessant. Fortxmately the conflicting ocean currents which meet at Havre possess attendant advantages, for they produce three tidal waves, arriving in succession, and the period of high water, instead of being limited to eleven minutes, extends over three hours. Vessels are thus afforded ample time to enter the docks. Topography. YoNNE. — This department is named after the principal tributary of the Upper Seine. It includes portions of the ancient provinces of Burgundy, Orleanais, and Champagne, and the great high-road from Paris to Lyons runs through it. Agriculture supports most of the inhabitants, and wine, cider, and beer are amongst its products. Auxerre (15,656 inhabitants), the capital, occupies the slope of a hill on the left bank of the river Yonne. It boasts of a magnificent cathedral, the finest in all Burgundy, and carries on a considerable trade in wine, the best being grown near Chahlis (2,185 inhabitants), to the west. Fontenaij, noted for a great battle fought in 841, lies to the south-west. Avallon (5,337 inhabitants), built on a rock overlooking the valley of the Cousin, has a few mediajval buildings, and carries on some trade ; but in the ej^es of the antiquarian it is eclipsed by the ancient capital of the district, Vezelay, on the Cure, now in ruins, but in the twelfth century a famous place of commerce and HAUTE-MARNK. 291 piljjrimage. It was hero that Kichard Ca-ur do Lion met the King of France in 1190, when preparing to start upon the third crusade. St. Florentin (2,256 inhabitants), Toniierre (4,991 inhabitants), and Ancy-le- Franc are the principal phices on the Armanf on. Tonnerre, lying on the railway from Paris to Lyons, carries on some trade in wine. L(i Roche, at the confluence of the .i\j'man(;on with the Yonnc, is a busy railway centre. Following the river, we pass Joignij (5,975 inhabitants) and its vineyards, and Vilkneiife-sur-Yonne (3,606 inhabitants), and reach Sens (12,251 inhabitants), the old capital of the Senones. Its cathedral is a most remarkable edifice, with windows painted by Jean Cousin. A chapter-house and the episcojjal palace, equally remarkable, adjoin it. AvBE is cut in two by the river Seine, which divides it from south-east to north-west, and is named after a tributary of that river. The surface is for the most part hilly, and moderately wooded, and in the north the do2)artment merges in the monotonous plain of Champagne. The soil is generally sterile. Troycs (41,275 inhabitants), the ancient capital of Champagne, the ancient Augustobona, on the river Seine, is altogether without natural defences, and thus fell an easy prey to every foreign invader. The town, however, took advantage of its central position, and in times of peace its commerce and industry flourished. The revocation of the Edict of Nantes nearly ruined it. It is now a great centre of the hosiery industry, and the nurseries in the neighbourhood enjoy a wide reputation. Amongst its edifices the first place must bo accorded to a magnificent cathedral, one of the finest in France. An ancient abbej' now serves as a library and museum. The old ramparts have been converted into delightful walks. Higher up on the Seine is Bar-siir-Sciiie (2,512 inhabitants), the insigni- ficant capital of an anondissement. Near it, in the valley of the Laigne, are the three Riceijs (2,755 inhabitants). Descending the Seine, we reach Romilly (4,925 inhabitants) and Nogeui-mr-Seine (3,335 inhabitants). Near the latter stood the abbey of I*araclet, the retreat of Abelard. The river Aube, on entering the department, flows beneath the stately abbey of Clairvaux, now converted into a con^•ict prison. At Bar-sur-Aube (4,495 inhabitants) the Aube leaves the hilly district and enters the chalky plain of Champagne, flowing past Brknne (1,860 inhabitants), where Napoleon first studied military science, and Arck-sur-Aube (2,817 inhabitants), the birtliplace of Danton. nAVTK-M.\RNE is divided by the plateau of Langres into two distinct sections, of which the southern is drained into the Saone, whilst the northern, embracing the districts of Bassigny, Tallage, and Perthois, is traversed by the Upper Marne, the Upper Meuse, and the Upper Aube, these three rivers rising within the department. More than a fourth of the surface is wooded. Iron ore abounds. Bourbotmc-ks-Bains (3,705 inhabitants), famous on account of its .springs, is the only town in the southern section of the department. Langres (9,488 inhabitants) occupies a commanding position on the Upper Mame, and is strongly fortified. It is the old capital of the Lingones, has a grand 292 PEANCB. old gate constructed by the Bomans, and a fine Gothic cathedral. Diderot was a native of Langres. The knives named after the city are manufactured in the neighbouring town of Ifogenf-le-Hoi (3,430 inhabitants). Chaumont-en-Bassigny (8,791 inhabitants), on a high limestone terrace at the junction of the Suize with the Marne, is a quiet country town. A magnificent aqueduct of fifty arches sup- plies the town with water. Below Chaumont we enter the " black country," in the centre of which is JoinviUe-en-YaUagc (3,723 inhabitants). Lower still is the Fig. 213. — The Entitions op Lanobes. Scale 1 : 120,000. ':Wq,.^^j§^^»^ \^ ^^>^^=:^axiSj$^ ^r t> ^ ;0..^i . 2 Miles. valley of Osne, famous for its iron foundries. St. Dizier (9,453 inhabitants) is one of the great iron marts of France. Vassij (2,799 inhabitants), in the valley of the Blaise, was an important town formerly, but has never recovered from the massacre of its Protestant inhabitants in 1562. Iron mills and foundries are in the vicinity, and higher up in the same valley lies the castle of Cirey, where Voltaire resided for several years. Makne, named after its principal river, consists of several well-marked geo- graphical regions. The Bocage, Perthois, and Argonne, in the south-east and east, belong to the lower cretaceous formation, and are partly wooded ; Champagne proper, in the centre, consists of chalk and marls ; whilst the district of Remois and the hills of Epemay and Sezanne are of tertiary origin. The population around the industrial city of Reims is dense, but in the monotonous plains it is sparse. MAENE. 293 Vitnj-k-F)-an^o!s (7,590 inhabitanls), on the Murne, is the terminus of the canal which joins that river to the Rhine. The town has been destroyed repeatedly, and was last rebuilt by Francois I. Chalons-sur-Marne (20,215 Fig. 2M. — CUALONS AXD ITS CaMP. 8cale 1 ; 160,000. f>"lE.otG 2 Miles. inhabitants), the capital of the department, has several fine churches, but the most remarkable edifice of the town in the old sanctuary of Notre-Dame dc I'Epine, about 6 miles to the north-east of it. The indu.strial art school is ono 294 FEANCE. of the most flourishing in France, and a vast trade is done in champagne. The old fortifications have been converted into public walks. Near a site now known as Attila's Camp was fought the battle of the Catalauuian Fields, which broke the power of the Huns. The " camp of Chalons " is no longer occupied. Epermy (15,414 inhabitants), one of the two great centres of the commerce in champagne, lies on the Marne, embosomed in vineyards. The wine from which veritable champagne is manufactured is grown on the hills bounding the river, and in a district extending from Sillery, near Reims, to Avizc (2,113 inhabitants) and Vertus (2,371 inhabitants), in the south. Ay (4,007 inhabitants), close to !l6pernay, is most famous for its cms. In 1873 more than 22,000,000 bottles Fig. 215. — The Bifukcation of the Grand Mokin at Sezanne. Scale 1 : 320,000. ) Miles. of champagne were manufactured in the department, and the profit derived from its sale has furnished the means for erecting the luxurious chateaux dotted over the country. Several of the towns in the hills to the south of ^pernay have become known through the military events of 1814 ; as, for instance. La Fere- C//a7>ijK' noise, Sezanne (4,690 inhabitants), and Montmirall (2,077 inhabitants). Sezanne, moreover, is interesting on account of the bifurcation of the river Grand Morin, which rises to the north of the town, a phenomenon similar to that in connection with the Cassiquiare in South America. Reims (80,098 inhabitants), the ancient capital of the Remi, does not enjoy the advantage of lying on a navigable river, but a canal connects it with the Marne MABNE. 295 aud the Aisne, and five railways converge upon it. It is one of the great historical cities of France. Clovis was baptized there, and the Kings of France, ever since Fig. 216. — ItsiMS AND £rERNAY. Scale 1 : iS»,O00. I- kO>: ..I' l-.ir • .■.■■■■ y'^i.'^.-^^^^'^i^ ''i'"'^'.^, 7.v\\v:^ lO-aOE nfV.ri. ^ T'amorfjiii *;OJVTAI,/»f,i:l ' citfM- |2°4O'E.ol0r . 2 Miles it is named. Brie, between the Seine and the Marne, consists of an eocene plateau, almost arid in its character, whilst the district of Gatinais, to the south of the Seine, consisting of miocene sandstones, being better supplied with water, is more fertile. A few largo forests remain, but the greater portion of the department is divided amongst a multitude of small landowners, busily employed in supplying the neighbouring city of Paris with corn, vegetables, and cheese. There are many quarries and clay pits, and the manufacture of paper is of con- siderable importance. Melun (11,215 inhabitants), the capital, ia the first large town on the Seine 298 FRANCE. Fig. 219.— Paris and the Gheat Highways France. above Paris, of which it is almost a rural suburb. The most remarkable building of the town is a huge prison. Near it is the chateau of Vaux-Praslin, with a collection of paintings, and a park laid out by Le Notre. Fontainehleau (11,545 inhabitants), at a distance of a couple of miles from the Seine, and in the midst of a vast forest, is one of the favourite pleasure resorts of the Parisians. The palace is associated in our memory with the revocation of the Edict of Nantes, the assassination of Monaldeschi, the captivity of Pius VII., and the abdication of Napoleon. Sandstone is quarried ; sand for the manufacture of glass is dug ; and the neighbouring village of Thomery is noted for its delicious white grapes. Morct, at the mouth of the Loing, carries on a brisk trade, but is inferior in that respect to Montereau-fauU-Yonnc (6,847 inhabitants), higher up the Seine, at the mouth of the Youne, which has also a huge china manu- factory, employing more than six hundred workmen. Provins (7,176 inhabitants), the old capital of Brie, lies in the delight- ful valley of the Voulzie, which joins the Seine from the north, and is com- manded by a citadel dating back to the thirteenth century. Near Ncinoiivs (3,857 inhabitants), on the Yonne, is Bi(jnon, the birthplace of Mirabeau. Brie-en-Comte (2,685 inhabitants), on the Yerres, a tributary of the Seine, is altogether dependent upon Paris, which its inhabitants supply with building stones, lime, vegetables, roses, and cheese. Meaux (11,739 inhabitants) is the most important town on the llarne, its houses clustering around an unfinished Gothic cathedral. The treaty putting an end to the war against the Albigenses was concluded here. Meaux, like most other towns of the department, is engaged in supplying • Paris with provisions. Lagny (4,247 inhabitants) and Chelles (2,351 inhabit- ants), both on the Marne below Meaux, are dependent upon Paris. The chateau of Ferrieres, to the south of the former, is one of the most sumptuous in France. La Ferte-soiis-Joiiarre (3,657 inhabitants), above Meaux, is the centre of the most fertile district of the department. The millstones procured from its quarries are exported as far as America. Jouarre (1,747 inhabitants), near it, has the ruins of a famous convent. Coulommiers (4,239 inhabitant^^) and La Fertd- Gaucher (1,849 inhabitants) are the only places of note in the valley of the Grand Morin. The former exports cheese, and near the latter are several paper-mills. LISRARY OF THE UNIVERSITV of ILLINOIS, I III I I I I Ill I'll lill rt(lll iiiiiaiiifciBiiiiaiiiiiBiiiiiiMii;;; l_ 1 .=-_-.^ ,:■'-. 1 , , , ^_j'^-- ' ^.- . PARI>!. 299 Pakis and the Department of the Seine are almost identical, for the latter in reality only consists of that great city and a portion of its environs. Paris, more than any other city of the world, has been alternately cursed or raised to the skies by poets and prose-writers ; and, whilst Barbier scornfully speaks of it as an " infernal vat," Victor Hugo chants its glories as those of the " mother of cities." Paris may not be the moral superior of other capitals of the civilised world, Kg. 220. — The Growth of Paris. Scale 1 : 125,000. \ ||b.Chap<:lt*/ V- '- X- Hfllfx Jl«iiluion(uot-') "faotbrpn 1 , 50' \>!l(\i rhftc<'iilonl Monlroutff ^«C!J(' ~~ •••m*... Bmavu* t-f f^ipfur y^ugiijt^ J^/I. Sncrutte tyi /-V.f. , Jnrrv^jrc ujii//r l^ur^ Iff ITff3 t/yW *^'- ^■j^ /S/^^ . 2 Mile . but it cannot be denied that at various epochs it proved itself the most active focus of human thought. Next to Athens, Rome, and Florence, no other city is so frequently in our thoughts as Paris. No other city has done more to transmit to us the lights of other days. As an intermediary between the Latin races and the rest of Europe, it fulfils functions of the utmost consequence, and is in some sort the arbiter between tho civilised nations of the earth. In certain respects Paris is the capital of the world. Tlie strangers who flock to it in thousands 300 FRANCE. proclaim it to be so. No other city of the world offers equal attractions to persons of the most varied tastes. Paris consists of a hundred distinct cities welded into one, and yet, as a whole, it is full of individuality. London, in com- parison with it, is wanting altogether in cohesion. In London the various classes of society exist side by side ; in Paris, by imperceptible gradations, one class merges into the other. Curiously enough, the great geographical advantages enjoyed by Paris have frequently been overlooked. M. Saint-Marc Girardin says that " the site occupied by Paris was not intended by nature to become the site of a great city." But M. Elie de Beaumont and Dufrenoy, in the commentary accompanying their map of Fig. 221. — The Comparattve Growth of London and Pakis in Popilation. 1 1 1 1 1 1 1 1 1 1 t 1 1 1 r 1 r / 1 f 1» Rm^'—* i<. ho ji-oo iSoo J 600 1/00 1 800 r8/s 5 France, point out that features of the soil and subsoil facilitated its growth. Common sense, not guided even by the lights of science, is able to appreciate the advantages offered by the geographical position of Paris. Old Lutetia was built upon a group of islands, near the confluence of two navigable rivers. The elevated hill of Montmartre served its inhabitants as a watch-tower, whence they were able to espy the ajjproach of an enemy. Paris not only lies on the great national highway which joins the Atlantic to the Mediterranean, but likewise on the route connecting Spain and Aquitaine with Northern Europe. It is the natural centre of the valley of the Seine and of the districts bordering upon it. Strategically its position is a strong one, and the semi- LIBRARY OF THE UNIVERSITY of ILLINOIS. GEOLOGICAL IVIAP OF Tf k'* , ■? • a % v» • AcWi ^''7'-^^°%. -*.' -t .-t,nt"^i iiifi\.J^ /Z,.^^ liw I'll. fe ^^ve/s; VillcDktivt \ ■ t: a'eaax. / t^ '^y , (Valeaufopl V;iun "4 ,/1^^ ::z-. 110 "Drawnly A.Yuilleniin Chalk TERTIAKY .S^m rff "^^^'^/^ ■% Adf .•BmSk, i^\ wf .v^^i IKuAnr o^ .^j? "^**^^!^^J 7^u»P«^m|^ ^ T ^*H^ J V'^--^^S ja^^S^^S^ " ^ j^^B*'" ^^^ f I ^^J ^^^^a^S^J?? a^e-t^ ^~-- mj Fer^^ budding % faUfrtpoted — — ^^^^^^— 5 Miles. of Vincennes and Boulogne outside of them. In the latter are the racecourse of Longchamp and a garden of acclimatation. Farther away from the town, but still easy of access, are the parks and forests of St. Cloud, Versailles, St. Germain, Montmorency, Chantilly, Compiegne, and Fontainebleau. Three great cemeteries — those of Montmartre, Mont Parnasse, and Pere-Lachaise — lie within the walls, but the future necropolis of Paris occupies the sterile plateau of Mery, beyond the river Oise. The enceinte of Paris has a circumference of 22 mQes, and its approaches are defended by two circles of detached forts, forming a vast entrenched camp of 350 square miles. SEINE-ET-OISE. 807 Amongst the many other towns and villages of the department of the Seine three are several which are mere suburbs of the great city. Of these the most important is Viiuriines (18,'27;i inhabitants), joined to Paris by Sf. Mamie (7,499 inhabitants). The castle of Vincenncs is historically interesting. The manufactur- ing town of St. Denis (29,500 inhabitants), to the north of Paris, is best known through its abbey church, the old burial-plioe of the Kings of France. The following are the prineip;il places in the arrondissement of St. ])enis : — Pan/in (13,646 inhabitants) and Atilpnillicrs (14,340 inhabitants), two manufacturing towns; Boittlj/ (1,402 inhabitants), famous for its forest; Lc Bourgct, which recalls a French defeat ; St. Oticn (11,250 inhabitants), with a castle built by Louis X^'III. and a huge railroad depot; Clichy-la-Gurciuie (17,354 inhabitants), Zt>crt//o/A-P(VVY< (22,733 inhabitants), Asnilres (5,692 inhabitants), and Colomhes (2,691 inhabitants), with numerous villas ; Neuilli/ (20,781 inhabitants) and Coiirberoie (11,811 inhabit- ants), two suburbs of Paris separated by the Seine ; Piiteau.r (11,387 inhabitants), a town of dye works and factories ; Siiresiies (5,097 inhabitants), at the foot of Mont Talerien ; Xanterre (3,890 inhabitants), noted for its holy well of Ste. Genevieve, its cakes and rosieres ; and Boulogne (21,556 inhabitants), beyond the wood of the same name. Sceaux (^2,460 inhabitants) is the capital of the arrondissement, to which belong the towns and villages to the south and east of Paris, the most important amongst which is Vincennes. The others are : — Montrcuil (13,607 inhabitants), famous for its orchards ; Charciitoii (8,744 inhabitants), with a lunatic asylum ; Maisons-Alfort (7,115 inhabitants), with its veterinary college; Nogent-sur-Marne (7,481 inhabit- ants), where the river is spanned by a viaduct 2,600 feet in length ; Icry (15,247 inhabitants), with huge factories; Vitnj (3,718 inhabitants), abounding in nursery gardens ; Choi-si/-le-livi (5,829 inhabitants), with the tomb of Rouget de I'lsle ; GetitiUy (10,378 inhabitants) ; Arcueil (5,299 inhabitants), with its two aqueducts; Montrouge (6,371 inhabitants), Vanves (8,812 inhabitants), Issy (7,356 inhabitants), and Clamart (3,333 inhabitants), near wooded heights, supplying building stones ; and Foiitcnay-uur-Roscs (2,804 inhabitants), which supplies the markets of Paris with flowers and fruits. Seine-et-Oise, the centre, which is occupied by the department of the Seine, is in the main a dependency of Paris, and, except in the vicinity of the latter, it is very tliinly populated. Its paper-mills and beet-root sugar manufactories are of some importance. Versailles (49,552 inhabitants) is now the most sumptuous suburb of Paris, but when Louis XIV. selected its site for the construction of his vast palace, he had no idea that the two would ever be attached to each other bj' a chain of suburban villages. The recent selection of Versailles as the seat of Government has done much to accelerate this junction. The palace, which formerly was the residence of the King and his court, now accommodates the Senate and the Chamber of Deputies, and an almost interminable suite of its rooms is occupied by paintings designetl to perpetuate the glories of France. Like its dependent mansions, the Great and Little Trianon, it has served as a pattern to nearly every sovereign throughout Europe, 808 FBANCE. but not one amongst them has succeeded in building an edifice or creating a park at all comparable with it. Versailles is associated generally with the old monarchy, but some of the revolutionary events also have taken place there. It was the birth- Fig. 228. — St. Germain-en -La ye. Scale 1 : 110.000. r -^ i S* GERJVM3. I tHi t '■" ""m I M 1 ^^ >,^1*>i.>^p»^^. ^ ^„^, ^ ""iBte.^ 2 Miles. place of Hoche, Houdon, Berthier, and others. Louis XV., Louis XVI., and Louis XVIII. were born in the palace. Many of the neighbouring towns and villages enjoy some reputation. Senrs (6,512 inhabitants) is famous for its porcelain ; St. Cloud (4,7G7 inhabitants) has a fine park and numerous villas ; St. Cyr (2,870 inhabitants) is the seat of a LI8RAKY vOF THE UNlVERSlTVoflUlNOIS, SEINE-ET-OISE. 809 niilitary college ; at Grigiion is an agricultural school ; Vilk-d' Array, Bouijiral {'i,\'2\ inhabitants), Loiiceciennes (1,1)40 inhabitants), and JJarlij are favourite summer resorts ; Rhi'U (7,980 inhabitants), at the toot of Mont Valerien, is an imix)rtant suburb of Paris, in which Richelieu had his chateau. Near it, below the hills of Marly, is the pumping station which supplies N'ersailles and its water works with the waters of the Seine. St. Germain (U),978 inhabitants) occupies the summit of a hill, and from the terrace of its chateau may be enjoyed one of the finest views in the vicinity of Paris. James Stuart resided in this castle, Louis XIV. was born in it, and it now contains one of the most precious historical museums in the world. The pine forest of Ledia stretches north of the town ; 21ai.soii.s-Lajfi/fc (2,824 inhabitants) has a famous castle built by Mansart ; and Poksy (4,G77 inhabitants), an old town, is often mentioned in history. Louis IX. was bom there, and the curious bridge over the Seine was built by him. Arijeiifcuil (7,i)34 inhabitants), another old town, is more especially noted for its early vegetables, its gypsum quarries, and its inferior wines. The arrondissement of Corheil, above Paris, is far less populous than that of Versailles. Its capital (0,187 inhabitants), at the confluence of the Seine and Essonne, has corn-mills, a j)rinting office, and other industrial establishments, and at Essonne (3,669 inhabitants), above it, are the most important paper-mills of the department. Mediaeval buildings abound in the vicinity, the most famous amongst them being the castle of Moiitlhery (^"2,005 inhabitants), on the banks of the Orge. Etampes (7,399 inhabitants), on the Juine, in the rich corn district of the Beauce, has several curious old churches, one of them with a leaning tower. It was the birthplace of GeoS'roy St. Ililairo. RamhouilM (4,294 inhabitants) lies in a wooded country within the basin of the Eure. Francis I. was born there, and the old royal castle is deserving of notice. The first merino sheep introduced into France were taken to the farm attached to it. Most of the other towns of the arrondissement have old castles. At Dotirdan (2,719 inhabitants), on the Orge, is the donjon of Philip Augustus; Iloudan (1,976 inhabitants) has a picturesque old tower ; Montfort-F Amauryhon&Xs of an old citadel, imposing even in its ruined condition ; and near Chevreuse, in the delightful vaUey of the Yvette, we come upon the chateau of Danipierre, rich in art treasures. The abbey of Port-Royal-des-Champs was razed to the ground in 1710, as a place accursed, for AntoLnc Arnauld and other Jansenistes had composed their works within its walls. Descending the Seine, we pass the email town of Mantes-la-JoUe (5,649 inha- bitants), at the mouth of the Vaucouleurs, its pretty church being reflected in the water of the river. In its \"icinity are the castle of Rosny, where Sully was born, and the sumptuous mansion of Roche-Guyon, with an old feudal castlo partly carved out of the rock. To the north of these, on the Epte, stands the ^•illage of at. Clair, with an old Norman castle. The arrondissement of Pontoise lies to the north of Paris. Enghien is much frequented for the sake of its sulphur springs, its lake, and its shaded walks. 310 FEAXCE. Monimoreney, which almost adjoins it, is famous for its cherry gardens. Chateaux and country seats abound in the neighbourhood, the most famous being that of St. Leu-Tarerny, with the tombs of the last Conde and of Louis Bonaparte. Ponioite (6,301 inhabitants), on the Oise, is one of the great provision marts of Paris. The Estates met here in 1-561, and Louis XIY. sought a refuge in the town during the troubles of the Fronde. On the opposite bank of the river is St. Ouen- fAumone (1,638 inhabitants', with the ruins of an old abbey ; and farther east is Mery-sur-Ouie, with the new Parisian necropolis. AisxK lies almost completely within the basin of the Seine, being traversed by Tig. 229.— Laos. ScJe 1 : SO.OCO. K '^'^\ ■ J.- rmj^^ HjOf aUHe. the rivers Mame and Oise, and is named after the Aisne, a tributary of the latter. The rivers Somme, Escaut (Scheldt), and Sambre rise within its limits, and in the north-east it borders upon Belgium. Anciently the department formed part of the provinces of De-de- France and Picardy. The naked plateau of Brie in the south, the wooded hills of Tardenob, the vicinity of Soissons, Talois, and the chalky cotmtrv around Laon belonged to the former, whilst Vermandois and the hill country of Thierache depended upon Picardy. Agriculture is in an advanced state. Hemp, flax, beet-roots, and rape seed are extensively cultivated, and the number of AISXE. 811 sheep IS very large. The ghiss works are amongst the most important in Europe, and there are also sugar refiucries, cotton and woollen factories, and other industrial establishments. ChutcaK-Tliicrnj (5,713 inhabitants), on the Marne, is commanded by the ruins of a fine old castle. It was the birthplace of La Fontaine. La Fl-rc-cn-Tardenois (2,068 inhabitants), on the Ourcq, has become known through the large number of prehistoric remains discovered in the grave-hills in its vicinity. Afc Port-aux- Perches the Ourcq becomes navigable, and a railroad connects the place with Fig. 230.— St. Quentln. Scale 1 : 80,000. CISE.nlPans Haifa Mile. Villers-Cotterets (3,116 inhabitants), the birthplace of Alexandre Dumas, where Francis I. published, in 1539, an edict which made the use of French compulsory in all public documents. Ferie-Milon, a village lower down on the Ourcq, was the birthplace of Eacine. Soissons (10,754 inhabitants), the ancient Noviodunum, on the Aisne, no longer ranks as one of the foremost cities of France, but the Middle Ages have left it a fine Gothic cathedral and several other ecclesiastical buildings, and its gardens have lost none of their freshness. 312 FEANCE. Laoii (12,036 intabitants), the capital of the department, rivals Soissons in antiquity and population. Being on the high-road which connects Paris with the Meuse, the town has been besieged many times. It boasts of a Gothic cathedral, and of a museum rich in antiquities, many of them having been discovered in the old underground villages of the neighbourhood. Artichokes and cabbages are amongst the most important articles exported to Paris. Hirson (4,285 inhabitants), on the Upper Oise, as well as Venins (2,889 inha- Fig. 231. — CoMPifeoNE. Scale 1 : 180,000. . 2 Miles. bitants) and other towns of Thierache, engage much in basket-making. St. Michel- Rochefort (3,231 inhabitants), near the former, has forges and cotton-mills. Guise (6,242 inhabitants), lower down on the Oise, the native place of Camille Desmoulins and the seignorial seat of an illustrious family, has huge china and stove works, as well as other factories. Descending the river, we pass La Fere (4,896 inhabitants) and Tergnier (3,079 inhabitants), and reach Chauntj (8,982 inhabitants), with its cotton and woollen niiUs, tan-yards, and other factories. A short railway conveys us thence to St. Gobain (1,957 inhabitants), famous on account of its glass works AISNR. 813 ever since (lie thirteenth centuiy. The country around is wooded. Prt'moiitrif is a small village to the oast, with a fiiinous old abbey, converted into a lunatic asylum. Coiicy, another village, boasts of one of the finest feudal castles of tho Fig. 232.— CUA.NTILLV. Scale 1 ; 130,000. 2 Macs. Middle Ages. Another castle stood at Quierzi/, on the Oise : it originally belonged to the lords of Heristal. .SV. Qtientin (37,0S0 inhabitant.^), on the Somme, is the capital of the depart- ment, a canal, much frequented by coal barges, connecting it with the Scheldt and the Oise. There are numerous cotton and woollen mills, machine shops, beet-root sugar refineries, and other industrial establishments. Among the public buildings a 314 FRANCE. Gothic town- hall and a collegiate church of the twelfth century are most deserving of notice. Fresiwy-k-Gmnd (3,849 inhabitants) and Bohain (5,975 inhabitants) are smaller towns in the neighbourhood, carrying on the same branches of industry. OiSE, like Aisne, has been formed out of portions of Ile-de-France and Picardy. The river Oise bisects it, the chalk region of Beauvaisis occupies the centre, whilst more recent tertiary formations predominate in the north. There still remain a few pine forests, but nearly the whole of the surface is cultivated. Industry is highly developed. In china, earthenware, and fire-proof bricks the department occupies the foremost rank ; its iron mills and foundries are of great importance ; and there are also cotton and woollen mills and sugar refineries. Noyon (5,785 inhabitants), Noviomagus of the Romans, is the first town on the Oise, and one of the most ancient of France. Charlemagne was crowned in it ; it was the birthplace of Calvin ; and its cathedral is one of the finest in France. The old abbey of Oiirncamp, below Noyon, has been converted into a factory of cotton velvets. Compiegne (12,923 inhabitants), below the mouth of the Aisne, is best known in connection with its forest, ever since the days of Clovis the hunting ground of the Kings of France. The existing chateau was built in the eighteenth century, and contains a valuable collection of Cambodian antiquities. Picnrfonds, at the eastern skirt of the forest, has mineral baths and a castle constructed by a Duke of Orleans. Still descending the Oise, we pass the old towns of Verberie and Pont Sfe. Ma-rcnce (2,225 inhabitants), and reach Creil (5,438 inhabitants), one of the great railway junctions of France, and, together with the adjoining town of Montataire (4,864 inhabitants), the seat of iron works, machine shops, and china manufactories. Of the places to the east of the Oise, Scnlifi (6,537 inhabitants), in the delight- ful valley of the Nonette, is the most important. The ruins of a Merovingian palace and an old cathedral point to better days. Ermenonville, with its tomb of J. J. Rousseau, is higher up in the valley, and ChantUhj (3,476 inhabitants), the French Ne^vmarket, is lower down. Much lace is made in the vicinity. Crepy (2,646 inhabitants), close to the eastern frontier, is the old capital of Valois. Clermont (6,101 inhabitants), the capital of the centre arrondissement, has a large prison and a lunatic asylum. The town has some manufactories of hosiery, and so have a few other places near it, as Liancourt, St. Just-en- Chaussee (2,395 inhabitants), and Bretcidl (3,034 inhabitants). Beaiimis (16,591 inhabitants), the largest town on the Th^rain, a famous old city, with an unfinished cathedral, a town-hall, and other curious buildings, has been known from the most remote times for its cloth, tapestry, earthenware, and fireproof bricks. Cloth and buttons are also manufactured in the towns below Beauvais, amongst which are Noailles, Mouy (3,118 inhabitants), and Bury (1,172 inhabitants), as also at Meni (3,517 inhabitants), to the south-east of it. EuRE is named after a river which enters the Seine within the limits of the department. Norman Vexin lies to the east. The plain of St. Andre occupies the south, the fertile plain of Neubourg adjoining it in the north. The EURE. 315 lowlands on the estuary of the Seine are known as Koumois. The fertile meadow lauds of Lieuvin aro in the west, beyond the Rille. Euro depends mainly upon agriculture and cattle-breeding, but there are also copper, brass, and zinc works, sugar refineries, cotton and woollen mills. Vtnioii (0,384 inhabitants), Claillon (:J,rJ6 inhabitants), and Lvx AmMya (3,'257 inhabitants) are the only towns of note on the banks of the Seine. The first of these has quarries, vineyards (the last met with on the Seine), and u huge Government cloth factory. Gaillon exports much fruit to Paris and England, but is best known on account of the ruins of a fine castle, built in 10 10 by Georges d'Amboise, the cardinal. Les Audelys consists of two towns, one on the river, Fig. 233.— Les Asdelts. Scale 1 : 50,000. 1 ilile. the other a short distance inland. The latter has manufactories ; the former is essentially a place of commerce, and the river there is commanded by Chateau Gaillard, erected by Richard Coeur de Lion. Blanchard, the first aeronaut who crossed the Channel, was a native of the town, and IS'icolas Poussin was born in a neighbouring village. The river Epte enters the Seine from the right, flowing through a delightful valley, the principal town within which is Gi.ms (3,090 inhabitants), with a famous old castle. Lower down the Seine is joined by the Andelle, which sup- plies motive power to numerous mills. The first town reached on ascending the Eure is Louviers (10,097 inhabitants), a busy manufacturing place, producing cheap cloth and other woollen stuffs. 316 FEANCE. Evreux (11,453 inhabitants), on the Iton, a tributary of the Eure, the capital of the department, is noted for its cutlery and hardware. At Breteuil, higher up on the same river, are iron works and rolling-mills. The valley of the Avre, another tributary of the Eure, is the seat of a considerable industry. Its principal town ia Verneuil (3,267 inhabitants). Ivnj-la-BaiaUle, on the Eure itself, is noteworthy for the defeat inflicted upon the League by Henri IV. (1590). The river Rille traverses the western portion of the department. Ragles, on its upper course, has manufactures of copper, brass, nails, and needles ; whilst Fig. 234. — EouEN and its ENrinON's. Scale 1 : 320,000. r 15 W of Paris ri S'E of Or 5 Miles. Bcrnay (6,087 inhabitants), in the side valley of the Charentonne, is noted for its cottons, woollens, ribbons, and linen. Its horse fairs are famous throughout Normandy, and in the vicinity are several castles of note, amongst which that of Broglie is the most remarkable. Still descending the river, we pass Brionne (3,229 inhabitants), a manufacturing town, and reach Pont Audemer (5,557 inha- bitants), at the head of the tide, and the only seaport of the department, Quille- hceuf, on the estuary of the Seine, being merely a pilot station. Seine-Inferieure (Lower Seine) includes nearly the whole of the chalky plateau of Caux. The hilly district of Bray lies in the south-east. The depart- LIBRARY OF THE UNIVERSITY of ILLINOIS, SEIXE-INFfiBlETJEE. 817 ment ranks high for its agriculture, its industry, and its commerce. Rouen and Elbeuf are great seats of the cotton and woollen industries, wliilst Ilavro only yields to Marseilles in the extent of its commerce. Elbeuf (38,34;i inhabitants, including its suburbs) is the first town of the department on the Seine. Its woollen manufactories annually consume £2,000,000 \rorth of raw material, and, in addition to them, there are print works, machine shops, and other industrial cstablisbmeuts. There are no remarkable buildings, two churches with stained windows excepted, but the environs of the town are picturesque, the Seine being bounded by steep cliffs and extensive forests. Descending the river, we pass Oiswl (3,405 inhabitants), St. Etiennc-de-Rouvray (2,788 inhabitants), Sotteville (11,278 inhabitants), and the chemical works of St. Paul, above which rise the bold cliffs of Bon Secours, surmounted by an old church, and find ourselves within sight of Rouen. Rouen (104,863 inhabitants), the old capitol of the Veliocasses, the Rotomagus Fig. 235.— Le IIavke. Scale 1 : 100,000. \'u(Pori6 10' If Cosselin Caueriainrill]^ of the Romans, is most favourably situated near the mouth of a great navigable highway, which places it in communication with the sea as well as with the interior of the country. The city Wes within a basin surrounded by steep hills, but two valleys facilitate communication with the plateau. Rouen is famous for its fine Gothic buildings. The cathedral is richly decorated, has beautifully stained windows, and is rich in ancient tombs, including that of Richard Cocur de Lion. Its spire rises to a height of 494 feet. The church of St. Ouen almost surpasses the cathedral in magnificence, whilst the church of St. Maclou is valued for its sculptured portal, one of the best works of the Renaissance, attributed to Jean Goujon. The courts of justice are one of the most finished examples of the Gothic architecture of the end of the fifteenth century. There are other buildings which almost convert Rouen into an architectural museum, such as the clock- tower of the old town-hall, the tower of Joan of Arc, and the Hotel Bourgtheroulde. A valuable gallery of paintings and a library of 100,000 volumes are contained in VOL. II. V 818 FEANCE. the town-hall, and the number of scientific societies and superior schools is con- siderable. Corneille, Boieldieu, Fontenelle, and La Salle, the discoverer of the mouths of the Mississippi, were born in the town, and statues have been erected in memory of most of them, as well as in honoiu- of Joan of Arc, who perished here at the stake. Vessels drawing 16 feet of water can reach the quays, and Eouen carries on a lucrative commerce in spite of the competition of Havre, which guards the mouth of the river. As one of the great centres of cotton industry it is now without a rival in France. Its manufactures mainly produce simple and durable stuffs, and Fiff. 236. — The Cliffb of I^tretat. in years of prosperity over a million spindles are at work at Rouen and the neigh- bouring towns of Pvtit-Quevilly (5,719 inhabitants), Darnefal (5,018 inhabitants), Devi lie (4,183 inhabitants), and others, and the cotton stuffs produced attain a value of nearly £4,000,000. Following the windings of the river, the traveller skirts the cliffs of Canteleu and the Forest of Roumare, passes the small port of Duclair, and encompasses the peninsula of Jumieges, with its fine old abbey. It was here the Normans landed on their first arrival in France. Caudeiec-en-Caux (1,951 inhabitants), with its tall tower, the port of the old manufacturing town of Yretot (7,636 inhabitants), whose seigneurs enjoyed the title of king, is left behind us. Lillebonne (4,570 SEINE-INFfiRIEURE. 819 inhabitants), the old capital of Caux, near the mouth of the river Bolbec, boasts of a few Roman ruins, but Bolbec (0,778 inhabitants), higher up in the valley, is now the leading town of the country. It is clean and well built, and its inhabit- ants are engaged in the manufacture of cottons. We pass Harjlcitr (1,908 inhabitants), a decayed port, and the castle of Tancar- ville, built on a commanding clifY near the mouth of the Seine, and reach Jfarre (85,407 inhabitants), the great port of "Western France. This town is of modem date, for it was founded by Francis I., as a successor to older towns higher up the river whoso ports had become silted up. Havre has not only taken care to keep its navigable channels open, but has also constructed docks, and to the enterprise of its citizens it is indebted for the supremacy it holds as a maritime city. It is essentially a seat of commerce, and the only buildings of note are its town-hall and its museum — the latter with statues of Bernardiu de St. Pierre and Casimir Fig. 237.— F£cAMP. Scale I : 40,000. . Half u Mile. Delavigne, the most famous children of the town. The docks and quays are on a vast scale. Le Havre principally imports cotton, coffee, copper, timber, wool, skins, corn, and coals. It exports silks, woollen stuffs, cottons, and " articles de Paris," and England is its chief customer. Lines of steamers connect it with Xorthern Europe, the Mediterranean, and America. The town no longer engages in the cod and whale fisheries, but the conveyance of German emigrants to America has recently proved a source of profit. There are ship-yards, machine shops, rope-walks, sugar refineries, a tobacco manufactory, and a few cotton-mills, besides which the town is much frequented by seaside visitors, a fine beach for bathing extending as far as Ste. Adresse and the lighthouses of La Ileve.* • In 1875 vessels of l,377,15t) tons burden entered in the foreign trade, and 140^760 tons in tlio coasting trade. Tlie exports and importii were valued at £67,200,000. Y 2 D20 FRANCE. 3£ontivilliers (3,554 inhatitants) is the only place of any importance close to Havre. Along the coast, towns and villages occupy the mouth of each valley. Just beyond the bold cliffs of Antifer we reach Etretat (1,976 inhabitants), a delightful seaside village, " discovered " by the landscape painter Isabey. Then follow Tport, a small village of fishermen, and Ficamp (12,074 inhabitants), which extends for several miles up a narrow valley, and has many cotton-mills. Its port Fig. 238.— Dieppe. Scale 1 : 17,000. rlS'E.af Or Quarter of a Mile. is accessible at all states of the tide to vessels drawing no more than 13 feet of water, and over a hundred vessels, employed in the Newfoundland, mackerel, and herring fisheries, belong to it. Passing St. Valery-en-Caux (4,090 inhabitants) and a few small villages, w-e reach Dieppe (19,471 inhabitants), one of the great towns of the department, and, next to Havre and Rouen, its busiest seajjort. During the Middle Ages the mariners of Dieppe were amongst the boldest rovers of the sea, and the town, SEINE-INFilRIEURE. 821 enriched by commerce, became very powerful. But civil wars and the silting up of. the port, which no longer deserved its Norman name of Diop (" detp "), destroyed its prosperity. Recently the town has somewhat recovered. Docks have been constructed ; steamers ply daily between the town and Newbaven ; the fishery is of importance ; and the carving of ivory, the manufacture of tobacco, and the entcrtuiument of seaside visitors prove sources of wealth. The fishermen in the suburb of Lc Pollet arc supposed to be of foreign, perhaps Venetian, origin. A statue has been erected to Duquesne, the naval hero who defeated De Iluyter. An old castle commands the town, and a few miles inland may be seen the ruins of that of Arqxi'x. Treport, at the mouth of the Bresle, is a seaport of some importance. Higher up on the same river is Eit (4,1G9 inhabitants), an old Gallo-Roman city, with a castle built by Henri de Guise, and frequently inhabited by Louis Philippe. Amongst noteworthy places in the eastern portion of the department are Aumak (Albemarle, '2,052 inhabitants), on the Upper Bresle ; Ncufclidtd (3,586 inhabitants), famous for its cheese, on the Bethune ; Forycs-ks-Eaux, with ferruginous springs ; and Gournay (3,056 inhabitants), on the Epte, a tributary of the Seine, which exports much butter. CHAPTER XII. NORTHERN FRANCE. Basins op the Somme axd the Scheldt ; Picardy, Artois, and Flanpers. HE north-western corner of France, between the Channel and the German Ocean, is by no means of wide extent, but it is neverthe.- less one of the most important districts of the country. Nations, difibring in language and customs, have repeatedly struggled for its possession; and the narrow strait, or jms (stride), which there separates France from the British Islands, has become one of the most frequented highways in Europe. Geologically this region is interesting on account of the cretaceous and oolitic heights of Boulogne, which rise like an island in the midst of the tertiary plains of Artois and Flanders. These heights were joined at some former epoch to the Wealden of Kent, from which they are separated now by the Strait of Dover, or Pas de Calais. They abound in ores and coal, and have added much to the wealth of the country. The heights of Boulogne divide the rivers of Northern France into two groups. Those on the southern slope, such as the Somme, the Authie, and the Canche, like those of Caux, take their parallel course to the ocean, whilst the rivers descending from the eastern slopes have more sinuous courses, and partly find their way into the Scheldt. The Somme is the most considerable river of the country. It rises near St. Quentin, flows at first in the same direction as the Oise, from which it is sepa- rated by a narrow belt of country, hardly more than 6 miles across. Near Ham it turns to the north, and having been reinforced by the Avre above Amiens, it enters a deep and rectilinear channel cut into a low plateau. The valley of the Somme distinctly exhibits traces of ancient floods. The river formerly filled up the whole of the valley, carrying down with it immense quantities of sand and gravel. It was in one of these heaps of gravel that Boucher de Perthes discovered, in 1838, the stone implements which have revolutionised anthi'opological science. Much of the valley of the Somme consists now of bogs, and more turf is dug here than in all the remainder of France. BASINS OF TUE SOM:Mt; AN'D TKE SCHELDT. 828 The tide ascends tho river as fur as Abbeville, and, by constructing embank- ments, the estuary of the river has been reduced to 27 square miles, and nmch of the laud formerly invaded by tho sea converted into pastures. The army of Fig. 239. — The Uills op Boulogne. Scale 1 : 350.000. 5 Miles. Edward ITI. crossed this estuary by the ford of Blanquctaque two days before the battle of Crecy (1346). Crotoy, near the mouth of the river, was used as a harbour up to the beginning of this century, but the engineers have " regulated " the river, and excavated a navigable canal which leads past St. Valery. The bay, 824 FEANCE. unfortunately, is silting up, in spite of all their efforts, and sea-going vessels are able to reach St. Valery only on ten or twelve days every month. The coast in this neighbourhood has certainly undergone many changes during historical times. The swamp or lagoon of the Hable, to the south of the Somme, is clearly an old mouth of that river, the neck of land which now separates it from the sea having anciently been a bar closing its mouth. The whole of the shore region, from the bay of the Somme to that of the Canche, and inland as far as the hills of Artois, is of recent formation. Rue, formerly a seaport, now lies 6 miles inland, and the old port of St. Quentin (Grand-Gouffre) is dry land. Fig. 240. — The Estuary op the Somme. Scale 1 : 300,000. l"'30'E.ofrH- DepiA Icjs tfum Z *z F'alhcnt^ ilL iota wni^r DtfitA 2^1 -S FatAcina over S raiAoms 4 Miles. The peasants of Picardy, in imitation of their neighbours, the Flemings, have won much land from the sea. They have constructed dykes and drainage works, and planted the dunes with reeds. Cape Gris-Nez, which separates the German Ocean from the British Channel, occupies an important position with reference to the geological changes going on along the coast. On either side of the cape the ocean currents deposit large quantities of silt, and the land gains upon the sea, whilst farther away from it, along the coast of Caux and in Holland, the sea encroaches upon the land. An upheaval or subsidence of the land has something to do with these changes. To B.VSINS OF THE SOMME A\D TnE RCUELDT. 826 tlie west and south ot" a line pussinff tlirou<;li Niouport the land slowly rises, whilst in the cast it subsides. At the same time it should be remembered that the land may subside without the sea encroaching upon it, as long as the alluvium deposited by ocean currents along the coast is of considerable amount. Such happens to be the case along the coast of Dunkirk. M. Gaspard has discovered there a layer of turf containing prehistoric remains at a depth of 10 feet beneath the marine sands. The land consequently must have subsided there since tho formation of these ancient turf beds. The researches of M. Day at Sangatte and Wissiint, near Cape Gris-Nez, prove that a similar subsidence has taken place to the west of Calais. He has discovered there a submerged forest, with bones of the aurochs and fresh-water shells, which clearly demonstrate this fact. At an epoch Fiir. 211. — The Ancient Gtlf op Flaxders. Scale I : 700.000. f SO 11 ■ .\l li(.K. still more remote an upheaval appears to have taken place, for beneath the dunes traces of old sea beaches have been discovered far beyond the reach of the actual tides. Ilowevcr this may be, during the last thousand years the long-shore men of Artois and French Flanders have enjoyed a period of conquest in their struggle with the sea. In the time of the Romans the lowlands lying to the north-east of the hills of Artois along the Belgian frontier were covered by the sea. As lately as the ninth and tenth centuries the sea extended as far as St. Omer. Even now the alluvial fields around that town are beneath the level reached by the spring tides, and a few deep ponds, fringed with willows, still mark the greatest depressions of this ancient gulf. The promontories which rose on the western shore of this 326 FEANCE. gulf still retain the names they received from Norman mariners, such as Mark Ness, Boker Ness, and Long Ness, and here and there may be recognised ancient islands rising above the general level of the polders which environ them. In the Middle Ages the towns of Calais, Gravelines, Dunkirk, Nieuport, and Ostend occupied a line of dunes, which separated this ancient Gulf of Flanders from the open sea. The alluvium brought down by the Aa and its tributaries gradually converted the lagoon sheltered by these dunes into a swamp ; and a swamp it would have remained to the present day had it not been for the labour of man. Fig. 2-l'2. — The Moeees of Dunkikk. Scale 1 ; 200,000. — .. S I^itthcTn L.inC' ^^^—^^^— 2 Miles. As early as the seventh century the first embankments were thrown up around the islands of the ancient gulf. The islands became attached to the mainland, canals were added to canals, until they intersected the whole of the country. These drainage works, which rival those accomplished by the Hollanders and Frieslanders, are locally known as wateringues. In time of war the sluices were frequently opened to inundate the country surrounding the fortresses along the coast of Flanders, and it requires years of labour to repair the injury thus done. Sometimes, when the rains are exception- ally heavy, the lowlands to the north of St. Omer are covered with water to a BASINS OF THE SOMMi: AND THE SaiELDT, 827 depth of 3 feet, ^^^len this huppens the wutcr has to be drawn off at the porta, and this produces so swift a current in the canals as to interrupt navigation for three or four months at a time. On the other hand, in years of drought the small canals, or tratenjands, dry up, or become converted into fever-breeding, stagnant pools. This likewise leads to an interruption of navigation, for tlio sluices must be kept closed along the rivers, in order to store up water for refilling the canals. "Wells sunk near the coast have been observed to rise and fall with the tides. The Aa is the principal river of this region, and its channel is altogether an artificial creation. Since the middle of the eighteenth century the river enters the sea at Gravelines, but before that time its mouth was 3 miles to the east of that town, and earlier still, up to 1170, it was a couple of miles to the west of it. The old port of Mardyck was a creation of man, as is that of Dunkirk. The labour involved in converting the whole of this region into productive land has been immense, and would never have been accomplished had not the proprietors of the wateringues been permitted to baud together for the common management of their estates. In 1793 the dykes were cut, as a measure of defence, and all that portion of the arrondissement of Dunkirk lying below the level of the sea was Fig. 243. — Section of the Stiuit of Dover between Dunkihk axd Bboasstaibs. Scale 1 : 650,000. . 10 llilca. inundated. The "Moiires" became lagoons, but the inhabitants, not being impeded by official interference, very soon succeeded in recovering the ground they had lost. In works of this kind care must be taken to prevent the mingling of fresh and brackish water, which inevitably results in murderous fevers. The shelving beach of sand which bounds the whole of this coast has undergone but few changes since 1776. At the mouths of the harbours it has certainly increased in width towards the west, for the sediment brought down by the rivers is carried in that direction by the ebb. Nor do the sand-banks lying parallel with the coast appear to have changed much in the course of a century. They are numerous, and form a veritable labyrinth, all the more dangerous to the navigator, as the course to be taken varies according to tide and wind. These banks are undoubtedly due to the set of the currents, which is generally towards the German Ocean. In the Strait of Dover the tide sets towards the east, and westerly winds predominate. The matter held in suspension is thus carried towards the north, and deposited for the most part along the coast of Flanders. The depth of the sea has decreased 3 to 6 feet since the commencement of this century, but well- sheltered roadsteads extend along both the English and the French coasts. That of the Downs, on the English coast, is protected by the Goodwin Sands ; that of 328 FRANCE. Dunkirk, on the French coast, lies within a chain of sand-banks fringing the coast of Flanders. The centre of the Strait of Dover, between Gris-Nez and the South Foreland, Fig. 244. — The Strait of Dover and the Proposed Tunnel. Scale 1 : 1,000,000. I'lW-'^'"'" DufUh, asK. . 10 Miles. Governments took up the question, and since 1875 some progress has been made in the great work. The tunnel will pass through the impermeable lower chalk, at a depth of 4 1 4 feet below the level of the sea. Except its seaboard, the densely populated region now under review has no well-defined natural boundaries. From the line of water-parting separating the Somme, the Scheldt, and the Oise, the country slopes insensibly almost in every direction. We can cross the frontier from Belgium into France without noticing it, and the only obstacles met with by an invading army consist of rivers and canals, with fringes of large trees, which sometimes impart some beauty to this 830 FRANCE. monotonous country. A triple line of fortresses defends the frontiers of France, and the inhabitants of this ethnological border-land have at all times been remark- able for their warlike spirit. The Nervians, who opposed Ccesar, and the Flemings of the Middle Ages, were renowned for their bravery. The Picardians, who live to the south of the Flemings, are equally brave, and in some measure they combine the solid qualities of the north with the quickness of the south. Nowhere does the political boundary agree with the ethnological one. Near the coast, the Flemings, or flamingants, occupy both sides of the boundary, whilst farther east French is spoken in Belgium as well as in France. The Flemish language has lost ground since Artois, Picardy, and a portion of Flanders have become a part of France. It was spoken formerly as far as the gates of Abbeville and Amiens. In the seventeenth century its use was common to the north of a line drawn from Boulogne to St. Omer. The country between Lille, Valenciennes, and Cambrai Fig. 247. — The Coal Basin of Northern Fii.\NCE. Scale 1 : 700,000. ^->.>-> > * > \ 10 Miles. did not adopt the French language till the middle of last century. Even In those districts where Flemish is spoken, the towns are bilingual, and Fi-ench is rapidly gaining ground. Only about 150,000 persons actually speak Flemish still. The population in Northern France is very dense, but the resources of the country are considerable. The soil, in many instances of very inferior quality, is most carefully tilled, and Montesquieu's remark, that the fecundity of a country depends less upon the natural fertility of the soil than upon the civil liberty enjoyed by its inhabitants, is fully borne out by what may be seen in the vicinity of Lille. The soil there is naturally sterile, but the inhabitants having formerly been exempted from the payment of indirect taxes and statute labour, were able to devote the whole of their resources to the improvement of the land. The agriculture of Picardy and Flanders ranks high, and excepting in the densely populated depart- ment of the Nord, the produce not only suffices for local wants, but also supplies BASINS OF THE SOMME AND THE SHELDT. 881 considerable quantities for exportation to other parts of Fronce and to England. Calais, Boulogne, and Gravclines export much agricultural produce, the peasants themselves frequently freighting the sliips with eggs, fowls, und cheese, and main- tiiining regular agencies in London, Rotterdam, and Antwerp. For centuries the country has been pre-eminent for its manufactures, and the Fig. 218.— r£B0XNK-8CR-S0MMB. almost inexhaustible beds of coal will secure it that pre-eminence for centuries to come. Coal was first discovered in 1717 at Fresnes, close to Valenciennes, and since then an exact geological exploration of the entire basin has been made. TorOCKAI'HY. SoMME is named after the river wliich traVerscs the entire department, and enters the Channel below Abbeville. Tho soil is carefully cultivated by peasant 832 FRANCE. proprietors ; the breeding of horses, cattle, and sheep is carried on in the west ; and nowhere else are the poultry-yards so carefully attended to. There is no coal, but much turf is cut (1,420,000 tons in 1873). The manufactures include woollen and cotton stuff, linen, hosiery, and beet sugar. The Somme, on entering the department, flows past Ham (3,122 inhabitants), known for its castle, frequently used as a prison of state. It then flows north, in the direction of Peronne (4,210 inhabitants), one of the most famous fortresses of France. At the village of Tcrtnj, close by, Pepin of Heristal won the battle ^yhich secured to him the dominion over Austra'^ia (087). At the old abbatial Fig. 249. — Amiens. Scale 1 : 80,000 1 MUe. town of Corbie (3,977 inhabitants) the Somme is joined by the river Ancre, on which stands the small manufacturing town oi Albert (4,414 inhabitants). The district of Santerre lies to the south of the Somme, its capital being Montdidier (4,266 inhabitants), a dismantled fortress. This town, as well as the others in the same district, such as Roye (3,810 inhabitants), Hosieres (2,437 inhabitants), and Villers-Bretonncux (5,356 inhabitants), engages in the manu- facture of hosiery. The tenure of the land is stiU the same as in the Middle Ages, and no farm can be sold without the consent of the tenant. Amiens (61,606 inhabitants), at the confluence of the Arve with the Somme, the ancient capital of the Ambiani and the Roman Samarobriva, is a town of con- SOMME. 888 eiderable importance. Its cathednil is oue of the most sumptuous edifices of the thirteenth ceuturv, and by the side of it all other buildin-^s of the town shrink into Pier. 250. — The Catuedkal op Amiens. insignificance. There are a mu.semn, a library, and a botanical garden. The old walls have been converted into public walks, but the citadel is still maintained in VOL. II. Z 832 FEANCE. proprietors ; the breeding of horses, cattle, and sheep is carried on in the west ; and nowhere else are the poultry-yards so carefully attended to. There is no coal, but much turf is cut (1,420,000 tons in 1873). The manufactures include woollen and cotton stuff, linen, hosiery, and beet sugar. The Somme, on entering the department, flows past Ham (3,123 inhabitants), known for its castle, frequently used as a prison of state. It then flows north, in the direction of Peronne (4,210 inhabitants), one of the most famous fortresses of France. At the village of Tertnj, close by, Pepin of Heristal won the battle which secured to him the dominion over Australia (G87). At the old abbatial Fig. 249.— Amiens. Scale 1 : 80,000 1 MUe. town of Corbie (3,977 inhabitants) the Somme is joined by the river Ancre, on which stands the small manufacturing town oi Albert (4,414 inhabitants). The district of Santerre lies to the south of the Somme, its capital being MontcUdier (4,266 inhabitants), a dismantled fortress. This town, as well as the others in the same district, such as Eoye (3,810 inhabitants), liosieres (2,437 inhabitants), and Villers-Bretoiineiix (o,356 inhabitants), engages in the manu- facture of hosiery. The tenure of the land is still the same as in the Middle Ages, and no farm can be sold without the consent of the tenant. Amiens (61,606 inhabitants), at the confluence of the Arve with the Somme, the ancient capital of the Ambiani and the Roman Samarobriva, is a town of con- SOMME. 888 sideralile importance. Its cathedral is oue of the most sumptuous edifices of the thirtet-uth ceuturv, and by the side of it uU other buildiuf's of the town shrink into Fiff. 250.— The Catiiedbal or Amiens. insignificance. There are a museum, a library, and a botanical garden. The old walls have been converted into public walks, but the citadel is still maintained in VOL. II. /. 334 FEANCE. an efficient condition. The manufactures include linens, woollens, cottons, silks, and velvets, and there are iron foundries, machine shops, and chemical works. The market gardens around the town are most productive, and supply even England with vegetables. The Somme, below Amiens, has been converted into a navigable river. Passing Picquigny and Lonrjpre, in the midst of turf pits, we reach Abherillc (19,328 inhabitants), a great commercial port during the Middle Ages, but now, owing to the silting up of the estuary of the Somme, of little note. There are a fine Gothic church and the anthropological museum of M. Boucher de Perthes. The manu- facturing industry produces carpets, linen, iron castings ; and there are rope-walks and boat-3'ards. A viaduct, 4,484 feet in length, crosses the estuary of the Somme, and connects St. Vakri/sur-Somme (3,406 inhabitants) with the railway system of France. "William the Conqueror put in at St. Valery before he crossed over to England, but the harbour is hardly accessible now. Fishing-boats generally start from Crotoij, opposite, or from the village of Caijeux (2,480 inhabitants), on the open sea. The villages of the district of Vimeu, which extends to the south as far as Treport, are much frequented for sea-bathing. The river Maye, which enters the sea to the north of the Somme, flows through the forest of Cricij, where the windmill which sheltered Edward I. during the famous battle is still pointed out. Lower down on that river is Rue, a small town. The river Authie bounds the department on the north. On it is Doullcns (3,886 inhabitants), with an old citadel converted into a convict prison for women. Pas-de-Calais is named after the strait which separates France from England, and is known to us as the Strait of Dover. The department includes the greater portion of the old province of Artois, and, excepting the hilly tract near Boulogne, it consists of monotonous plains of great fertility, traversed by tributaries of the Scheldt, and by the Aa, the Authie, and the Canche, which flow into the Channel. The agricultural produce more than suffices for local consumption, and calves, sheep, poultry, eggs, corn, and vegetables are exported. The discovery of coal (annual yield 3,000,000 tons) has led to the establishment of numerous fiictories ; and there are iron works, sugar refineries, cotton, wooUen, and paper mills, copper works, and machine shops. The fisheries, likewise, are very productive. There are no towns on the river Authie, but Bcrcli-sur-Mer (4,107 inhabitants), behind the dunes to the north of the estuary of that river, is a place of some importance, with a sea-bathing establishment for 500 scrofulous children, main- tained by the city of Paris. The valley of the Canche is densely peopled. Frecent (3,792 inhabitants), near the source of that river, has iron works. Hcsdin (3,083 inhabitants) was fortified formerly ; and Azincotirt, where the French were defeated in 1415, is a few miles to the north of it. ;Si/. Pol (3,872 inhabitants) lies in a side valley of Canche. Still descending the latter, we pass Montretiil (3,474 inhabitants), an old member of the Hanseatic League, and reach Etaples (2,948 inhabitants), near the mouth of the river, the small port of which is occasionally visited by coasting vessels. PAS-DE-CALAIS. 885 Tionlogne (40,075 inhabitants), at the mouth of tho Liane, the most populous town of the department, occupies a position with reference to En{»land which tho Roman emperors appreciated liij^lily. But of the many huildinfja erected bj' them hardly anj' vestiges remain now. For centuries tho town formed an apple of discord between France and England. It is one of tho great maritime ports of France, communicating daily with Folkstono b\' steamers. More than 100,000 travellers here cross the Channel every year. The fislieries are of great importance. The existing harbour no longer answering tho requirements of commerce, the foundations of a new one were laid in July, 1878. The aspect of Boulogne is more picturesque than that of most commercial to^vns. The old Fi(f. 251. — lioviOGSB. Scale 1 : 64,000. i)^i:."\v...(j. 1 . . 1. ..I 1. town occupies the summit of a hill, and is inhabited by the wealthier citizens, whilst the lower town, apart from its sunqituous bathing establishment and a few hotels, cannot boast of remarkable buildings. Some of the roads in the suburbs are quite English in their aspect, which need not surprise us, as nearly one-tenth of the population is of English birth. These English settlers have contributed much towards the industrial development of the town. The manufactures include steel pens, hardware, and linen, and there are saw-mills and marble and cement works. Le Porhl (3,!):?8 inhabitants), a village to the south-west, is iiihaJuted by fi.shermen, (»nd af Sniinr ('I,l!)l inli.ibitanls) is (he ukkIcI farm of Ilaut-Tingry. 336 FRANCE. On tlie road from Boulogne to Calais we pass a column erected to celebrate Napoleon's proposed invasion of England; Marquise (3,923 inhabitants), with iron works and marble quarries ; Ambleteuse, where James I. disembarked in 1688 ; and AudresseUes, where an English company proposed to construct a large port. Calais (34,922 inhabitants), the rival of Boulogne, consists of a fortified town and of the industrial suburb of St. Pierre-les-Calais. The town for more than two centuries (1346 — 15-38) was held by the English, but the bulk of the inha- bitants are Flemish, and the public buildings remind us of Flanders. St. Pierre Fig. 252. — Calais. Scale 1 : 30,000. iiiilf ii Jiue. manufactures more especially cotton and silk tulle, a branch of industry introduced in 1819 by English capitalists, and still partly directed by English workmen. There are likewise linen-mills, steam saw-mills, and other establishments. The exports to England consist mainly of Parisian articles, horses, vegetables, eggs, poultry, and a variety of manufactures. The harbour of the town is quite inade- quate, and contrasts very unfavourably with that of Dover, on the opposite side of the Channel, which is here annually crossed by more than 200,000 travellers. Guines (3,644 inhabitants), 5 miles to the south of Calais, has bleaching grounds, NOED. 837 and a pyramid near it marks the spot where Blunchard and Jeffcrics alightwl on January 7th, 1785, after having crossed the Channel in a balloon. On going from Guinos to ^^^(//rs (1,10-} inhaliifants), wo pass, near Balingliara, the Field of tlie Cloth of Gold, where ITenry A'lll. and Francis I. met in lo'JO. St. Omer (•21,404 inhabitants), on the river Aa, has a mcdianal church, the ruins of an abbey, and manufactures tulle, muslin, common cloth, and pipes of every kind. Arques (3,701 inhabitants) is almost a suburb of St. Omcr. Tlitrou- aniic, on the Lys, is a poor village now, but it was an important town until Charles V. destroyed it in 1554. Near it, at Enguinegatte (Guingatto), was fought the famous Battle of the Spurs (1513). At Aire (5,058 inhabitants) the Lys becomes navigable. All the towns in the neighbourhood are centres of industry. Bellinne (9,315 inhabitants) has sugar refineries ; Lons (9,383 inha- bitants), Netu (4,219 inhabitants), and Ilenin-Lietard (5,491 inhabitants), have coal mines ; whilst Lilkr-t (4,701 inhabitants) is famous for its boots. The first artesian well was bored near it, and its yield has never dimini.shed. Arras (26,764 inhabitants), the old cajiital of Artois, on the Scarpe, a tributary of the Scheldt, does not yield to Calais or Boulogne in historical interest. It was famous during the dominion of the Romans for its industry, bu.t the tapestry which once was produced there is found now only in museums. The most noteworthj* building is a town-hall of the sixteenth century, with a fine belfry. The abbey of St. Waast, a structure of the eighteenth century, has been converted into a museum. The manufactures include beet sugar, soap, earthenware, and lace. The town is strongly fortified, and its fortifications occupj^ more space than do its houses. It was the birthplace of Hobespierre. Bajxiiime (3,190 inhabitants), to the south of Arras, is a small fortress of little note. NoRD (" north ") is the name of the most northern department of France, and includes portions of the ancient provinces of Cambresis and Ilainaut. The river Lys bisects it where it is narrowest. The south is hilly and partly wooded. The centre, intersected by tributaries of the Scheldt, consists of an undulating plain, whilst the maritime portion presents itself as a dead flat, above which rise a ictv isolated hillocks. Agriculture, industry, and commerce flourish. Cereals, beet- root, oil-j-ielding plants, flax, tobacco, hops, and vegetables are cultivated. The coal mines yield 3,500,000 tons a year. Industry is highly developed. The textile industries of Valenciennes and Cambrai employ 2,807,600 spindles, 25,810 power-looms, and 85,848 hand-looms. In 1873 were produced 200,000 tons of beet sugar ; 353,600 tons of cast iron, steel, and hardware ; 32,000 tons of zinc ; 81,750 tons of earthenware and glass ; 22,500 tons of soap ; and 36,600 tons of soda. The population has more than doubled since the beginning of the century. Arrntici (4,636 inhabitants), the capital of the eastern arrondissement, a portion of the old province of Hainaut, is only a small town, with picturesque fortifications ; but Fourmies (8,151 inhabitants), to the south of it, has grown into a considerable town, where the first glass works of Xorthern Franco wore established in 1599. LnudrecicK (3,693 inhabitants) and Jliinliriic/e (5,110 inhabitants) are the principal towns on the Sambrc. They are both fortified. At Maubeuge and the neigh- 338 PEANCE. bouring town of Hantinont (5,180 inhabitants) are numerous iron foundries and rifle factories. The villages of Malplaquet and Wattignies, both famous in the annals of battles, are near. Foignics and Jenmont (2,190 inhabitants) are customs stations on the Belgian frontier. Barai, the ancient Bavacum, capital of the Nervians, to the west, was an important Roman station formerly, but is now merely a village. Camhrai (10,969 inhabitants), like Bavai, has suflPered much during every war, but has always risen from its ruins, and fought stoutly, too, for its municipal liberties. Several treaties were signed in the old capital of Cambresis. The Fig. 253. — Valenciennes. spile 1 : 50.000. 1".^2E uf Gr 1 Mik- principal buildings are a town-hall and a cathedral. A monument has been erected in honour of Baptiste, the inventor of a species of cambric known as batiste. The principal articles manufactured are cambrics, tulles, and cotton lace. Caudrij (4,548 inhabitants), Quievy (3,467 inhabitants), and C (dean- Cam- brisk (9,444 inhabitants), the famous treaty town, in the south-east, manufacture linen, cotton, and woollen stuffs. Solcsmcs (5,723 inhabitants), in the east, has sugar refineries. Descending the Scheldt, we pass Iicinj (3,890 inhabitants), the fortress oi Bouchain, Lourches (3,590 inhabitants), and Denain (11,849), the latter with coal mines, iron works, and rolling-miUs. NORD. 839 Valenciennes (2'2,686 inhabitants) is a first-ruto fortress, but the manufacture of lace, which rendered the place famous during the Middle Ages, has almost ceased to exist, cambrics and lawn being nuuuifuctured instead. The neighbourhood of the town abounds in coal mines, iron works and sugar refineries. At Aiiziii ((!,!)20 inhabitants), close to the gates of the town, more than 2,000,000 tons are raised yearly by a single company, employing 10,000 workmen, to whom they pay annually £400,000 in wages. I.arge workmen's cities have sprung up in the vicinitv of these coal-pits, which extend IVoni Denain to the fortitied town of Conde-sur-Emiut (3,282 inhabitants), on the Belgian frontier. Even at St. Amand- Fig. 254.— LiLLB. Scale I : 70,000. 0»4i, P.. of l'apl^ 3*S E.of Gp les-Eaiu (7,243 inhabitants), a fashionable watering-place on the Scarpe, the sky is obscured by the smoke rising from hundreds of chinmeys. Douai (23,348 inhabitants), until recent times one of the most important features of France, is the scat of a university, of courts of justice, and of military establishments, including an arsenal and a gun foundry ; but it also engages in the manufactures common to the country, and, like the neighbouring towns of Aniche (4,686 inhabitants), Orc/iiis (3,318 inhabitants), and Marchicnnes (2,048 inhabitants), it has its cotton-mills, sugar refineries, distilleries, and machine shops. The old Flemish Parliament House is used now as a Court of Appeal. 342 FRANCE. Kg. 257. — Gravelines. Scale 1 : 50,000. Tourcoing (33,013 iuhabitants), engage almost exclusively in all branches of the woollen industry, and are the rivals of Bradford, in Yorkshire, which excels them in quantity and strength, but must yield to them in beauty of design. The suburbs of these two towns, Wattrelos (4,102 inhabitants), Croix (2,586 inha- bitants), and others, likewise engage in the woollen industry. Roubaix alone consumes daily 100 tons of wool. The towns have nothing to show beyond their factories, and the environs are wanting altogether in the picturesque. The Lys, into which numerous factories discharge their refuse, flows 5 miles to the north- west. Two villages on the small river Marcq, one of its tributaries, are noteworthy on account of the battles fought near them. These are Boiivines, where Philip Augustus defeated the Emperor of Germany (1214), and Slons-en-Pevele, where Philip the Fair took revenge for the defeat sustained at Courtray. AYhen we cross the Lys we enter the Flemish-speaking portion of the department. Ilnzehronck (6,363 inha- bitants) and Bailleul (8,180 inhabit- ants) are both manufacturing towns. the latter being the centre of the trade in the so-called Valenciennes lace. Cassel (3,224 inhabitants), on an isolated hill, from which may be en- joyed a most extensive prospect, is a famous old cadelhun. Other towns of some importance are Steenwerk (4,309 inhabitants) and Steenroorde (4,018 inhabitants). The arrondissement of Dunkirk has but few manufactures, but carries on a considerable commerce by sea. Bergues (5,368 inhabitants) is an old fortress, defending the approaches to Dunkirk. Its famous belfry and the two towers of an abbey are visible from the high sea. Bourhoiirg (2,448 inhabitants) is the principal mart for Flemish cart-horses. Crravelines (4,184 inhabitants), a small fortress, has impor- tant fisheries, and exports eggs, apples, and vegetables to England. Fort PhUippe was built in 1812, to prevent the smuggling carried on by English vessels employed by Rothschild ; and the town which sprang up near it was known as the town of smoggleitrs, or schmoHeler. Dunkirk (Dunkerque, 35,012 inhabitants) is a Flemish town, its belfry rising high above the houses which surround it. The town has sustained more sieges than anj' other in the neighbourhood. Its most glorious epoch dates back to the time of Louis XIV., when its mariners, led on by Jean Bart, often held their own 1 Mile. NORD. 848 agninet whole fleets, liut the laiglish ut lust obtained the upper huml, and it was destroyed in accordance with the treaty of Utrecht (1713). It has been Fig. 258.— DiNKiKK. Scale 1 : ^OOa HuUu MUe. restored since, and even enlarged. There are now three wet docks, capable of receiving vessels of 1,000 tons burden, and a fourth dock, of larger dimensions and greater depth, is being constructed. The roadstead of Dunkirk is one of 344 FEANCE. the safest in the Channel, quite equal to that of the "Downs," on the coast opposite. The commerce of the town flourishes, and is increasing, and saw-mills, cotton-mills, oil refineries, and other manufacturing establishments have been founded. The mariners of the town engage in the Newfoundland fisheries. Close to the walls of Dunkirk was fought the battle of the Dunes (1558), when Turenne beat Conde and his Spaniards. At Hondschoote (1,870 inhabitants), a neighbouring village, the Austrians were defeated in 1793. CHAPTER XIII. THE VOSGES. Basins op the Mei'se asd tub Moselle. General Aspects. ORTH-EASTERN France, within its present limits, may almost be looked upon as a continuation of the basin of Paris. There, too, as in Champagne, we meet with old beaches from which the sea has gradually retired, and many of the rivers, in their upper course, exhibit a remarkable parallelism with the Seine. The two great rivers of the country, however, the Meuse and the Moselle, flow to the Rhine. The system of the Vosges extends, under various names, from the Upper Saone to the great bend of the Rhine near Mayence. The nucleus of this mountain system consists of a triangular citadel of crystalline rocks, and if the sea were to rise 1,500 feet, this mountain mass would be converted into an island. Amongst the sedimentary rocks which form the inferior slopes sandstone predominates. It is generally tinged red by oxide of iron, frequently forms bold cliffs, or is split up into huge blocks resembling fantastically shaped castles. The Yosges bear a striking resemblance to the Black Forest, on the opposite bank of the Rhine. The geological formation of both chains is the same ; in each we meet with magnificent pine forests, above which rise dome-shaped summits clothed with tender grasses and a carpet of flowers. Both chains rise steeply from the wide valley of the Rhine, but slope down gradually towards the interior of the countrv. The low range of the Faucilles and the plateau of Langres connect the Vosges with the mountain system of Central France. The Faucilles are wooded, intersected by numerous ri\Tilets, and easy of access. They are of Jurassic age, whilst the plateau of Langres is covered with chalk. In the south, a deep depres- sion, known as the " gap of Belfort," separates the Vosges from the Jura. This gap, through which run a road, a railway, and a canal, has at all times played an important part in history. Immediately to the north of it rise some of the highest summits, or balhiis, of the Vosges, including the Ballon d'Alsace (4,100 feet). For 75 miles the present boundary between France and Germany follows the crest of the Vosges; but to the north of the Grand Donon 346 FRANCE. (3,313 feet), a huge mass of sandstone, witli a gigantic stone ring upon its summit, the victorious Germans have adjudged themselves both slopes. In the Vosges, as in many other mountain chains, the culminating summits rise at some distance from the crest. The most elevated mountain of the entire chain, the Ballon, or " Belchen," of Sulz (4,677 feet), rises about 8 miles to the Fig. 259. — Glacieks of the Vosges. Scale 1 ; 360,000. I wo E or rim . 2 Jlilea. east, being almost cut off from the main range by the delightful valley of St. Amand. Standing upon this mountain, our eye ranges as far as the snowy summits of the Bernese Oberland. Eleven fine roads run across this southern portion of the Vosges, the most fiimous amongst them being that known as the " Schlucht " {i.e. gorge), which connects Gerardmer with Munstci'. The contrasts between the French and the Alsatian slopes of the Vosges are GENERAL ASPECTS. 847 not confined merely to a diftbrence in the gradient, but extend likewise to climate and vegetation. The rains are lieavior on the western slope than on the eastern. At Strasburg and Culmar the annual rainfall does not exceed 27 inches, whilst at Mirecourt and Vesoul it amounts to 50 inches. The cause of this is evident. The westerlj' winds, on reaching the Vosges, part with most of their moisture. In Lorraine the sky is often clouded ; and whilst the vino flourishes in Alsaf ia up fo a height of 1,300 feet, its cultivation is impossible along the western slope of the mountains, owing to the rigours of the climate. To the same cause must bo traced the great extent of the glaciers, which in Fig. 2C0. — The Laxeb of G£rabdmer and Lokoemer. Scale 1 : I2&,000. '*??F§^- 'Jp :^.. ■:.;^' 'i^ -,.i t. - V^B^L. ■o'&.ot Cr Mae. a former age covered the western slope of the mountains, and descended into the ocean, which then reached to their foot. One of these glaciers occupied the valleys of the Upper Moselle, and that of the Moselotte, and extended beyond Gemiremont as far as Eloyes. A gigantic dyke, nearly 200 feet in height, and partly destroyed by the floods of the Moselle, still marks the site of the terminal moraine. In area this glacier far exceeded that of Aletsch, now the most considerable in Europe, and M. Ilogard thinks that at one epoch it spread like- wise into the valley of the Meuse, where erratic blocks of Vosgesian origin abound. Old moraines, rock-scratchings, and other evidences of glacial action abound. 348 FRANCE. The country around Giromaguy, to the north of Belfort, is strewn with huge blocks, as if a battle of giants had been fought there. In the west, towards Luxeuil, the streams of ice have worn away the surface of the hiUs, and small lakes or meres abound, one of them discharging one stream into the Moselle, and another into the Saone. Small lakes, some of them reflecting dark pines, and others embedded in verdant meadows, are also met with in the upper valleys of the Moselle and its tributaries. Most of them owe their existence to moraines, which dam up the rivers. Some of the best known of these lakes are near the Pass of the Schlucht. The small Lake of Retournemer occupies a cup-shaped cavity, whilst the larger Longemer occujDies the valley lower down, giving rise to the Vologne, which, not far from the lake, rushes headlong over a ledge of granite, and then swallows up the emissary of the lake of G^rardmer (2,180 feet). This latter is the largest lake in the Vosges. It is shut in, on the west, by a moraine 230 to 260 feet in height, has a depth of 246 feet, and overflows towards the east. The surrounding country, with its sombre forests and emerald meadows, is one of the most charming to be found in the Vosges, and in comparing the beauties of nature with those of the works of man the inhabitants of the country may well say, " What would Lorraine be without Gerardmer and a bit of Nancy ? " That portion of the Vosges which was formerly covered with glaciers is most plentifully irrigated. The Moselle, the Moselotte, the Vologne, and the Meurthe have all forced themselves a passage through ancient moraines. The Hohneck (4,460 feet), at the head of the ancient glacier of Gerardmer, forms the centre of dispersion of the riVers of the Vosges. Most of these rivers flow into the Alsatian 111, or into the Moselle, both of which are tributary to the Rhine. The Meuse, too, flows now into the Rhine, but at some former epoch it appears to have been a separate river, and it actually retains its name down to the sea. It first describes a large curve, almost parallel with the Moselle or Little Meuse. Its course, as is the case with many rivers flowing through a limestone region, is partly underground. In summer the river is almost entirely swallowed up near the village of Bazoilles, and reappears 2 miles below, at Noncourt. Having been joined by the Chiers, the Meuse winds along the schistose rocks of the Ardennes. Below Charleville it pierces the plateau, forming a sticcession of picturesque gorges, equally attractive to the artist and the geologist. The river meanders 600 or 1,000 feet below the level of the plateau, sometimes hemmed in by steep cliffs, at others bounded by tree-clad slaty slopes, presenting a charming contrast to the reddish or variegated cliffs. The valley offers but scanty accommodation for towns and villages, and one of the former, Montherm^, is so much shut in that the rays of the sun only reach it during part of the day. Where the Meuse crosses the French frontier it discharges 27 tons of water a second during summer, and twenty or twenty-five times that quantity when in flood. The plateaux which bound the valley of the Meuse are covered with woods, pastures, bogs, or naked rocks, and cultivable little valleys are few and far LIBRARY OF THE UNlVERSiTV of ILLINOIS. OENERAL ASPECTS. 840 between. The schistose heights of the Fugues, or Fanges, to the east of the river, are most melancholy of aspett aiul very thinly populated. Their name has reference to the pools of stagnant black water which abound there. Formerly the " sombre and formidable " Forest of the Ardennes occupied the whole of the country between the Scheldt and the Rhine. Wild boars and other beasts were numerous then, and the forest was much dreaded. Most of it has been destroyed, towns and villages now occupy the valleys, and the stubborn soil is made to yield harvests. The Ardennes and the Tosges luivc played no inconsiderable part in tho Pig. 261.— Meandeiunos of the Melse. S&do 1 : ICO.fOO. 2°20V ..iP. ■ 5 Milea. hi>tor_v of France. The Ardennes more especially have at all times proved a formidable obstacle t) invading armies, not so much on account of their width and their deep valleys, but because of their being very thinly populated. The roads open to an invader either lead through the valley of the Moselle, to the east of the Ardennes, or through the valley of the Oisc and the plains of Flandcr.s, to the west of them. Ethnologically the Ardennes and Yosges are even more important than in a military point of view, for thev form a linguistic boundary, and have prevented the Germanisation of Xorth-eastern France. vor,. n. \ A 350 FEANCE. Lorraine, or Lotharingia, thus named nfter Lothar, the grandson of Charle- magne, is French in sjjite of its German name. The inhabitants, as far as records can prove the fact, have always spoken a Latin dialect. Physicall}'- the Lorrainers differ from the Germans by having short and nearly round skulls. Their minds, too, are differently constituted. Cool, reflective, calculating, and circumspect, they have none of the mj'sticism of their neighbours the " Swabians.'' These latter have at all times designated them as " "Welsh." TorOGKAPHY. Meuse is named after the river which, rising on the plateau of Laugres, traverses the department in a north-westerly direction. A portion of it is drained into the Seine. Jurassic and cretaceous rocks cover the whole of the country, and the hills are for the most part wooded, more especially in the Argonne, on both banks of the Meuse. The naked plain of the Woevre, intersected by the Orne and its tributaries, lies to the east. Ilorse-breeding is carried on extensively, and there are iron and steel works. Bar-k-Duc (16,643 inhabitants), on the river Ornain, is the most populous town of the department. It has \n\n\ manufactories, and the canal which con- nects it with the Rhine and the Marne offers great facilities for the export of wine and other products. The town is noted for its candied fruits and pastry. The museum of the town contains a few Roman antiquities discovered near Ligny- rn-Barrois (4,128 inhabitants), on the Upper Ornain. Vfuwouk'urs ("2,475 inhabitants), associated with the history of Joan of Arc, is the first town met with on descending the Meuse. Then follows Commercy (4,960 inhabitants), with a fine castle, now used as barracks. The pastrycooks of Commercy are famous for their " madeleines." St. Miliiel (5,146 inhabitants), the old capital of Barrois, boasts of two fine churches, with sculptures by Ligier Richier, who was born here. It is defended by a modern fort. Verdun (15,433 inhabitants), lower down on the Meuse, is one of the most important fortresses of France, defending the defiles of the Argonne. In history it is famous for the treaty of 843, which partitioned the Carlo vingian Empire. The town is noted for its confectionery and liqueurs. Elain (2,815 inhabitants) lies to the east of Verdun, in the plain of "WoSvre, and on the road to Metz. Stenay (2,376 inhabitants), on the Meuse, has iron works and biscuit bakeries. ITonfmedy (2,219 inhabitants), on the Chiers, is merely a fortified village, whilst Clermont and Varennes, on the river Aire, and near the great Forest of Argonne, are places of no importance whatever. Louis XVI. was arrested at the latter in 1791. AuDEXXES is named after the old forest which still covers about one-fifth of its area. Champaign plains of cretaceous formation extend in the south ; the Jurassic hills of Argonne occupy the centre ; and the cold schistose plateau of Ardenne spreads out in the north, traversed by the deep gorge of the Meuse. There are iron mines, slate quarries, beds of jjhosphatic nodules, iron works, and woollen-mills. AUDEXXES. 851 St'daii (15,8G2 inhabitants), on the Mouse, below its contliionco with the Chiers, first rose into importance in the thirteenth century, when the Dukes of IJouillon made it their capital. The town suffered much in consequence of the revocation of tlie Edict of ^»antes ; but its cloth nuinufacture revived soon after, and is now of very great importance. There are likewise iron foundries ; and the valley of the Chiers, in which lies Carignan (1,874 inhabitants), is one of the great centres of the iron industry of the department. Turcnne and Macdonald were natives of Sedan. Its capitulation on September 2nd, 1S70, put a termination to the Second Empire. Chaikville (12,881 inhabitants) and Meziircs (5,204 inhabitants) are twin l-'ig. 202.— Chaklkville and MkziKues. Scale 1 : 60,000. 1 Mil, cities. The latter, occupying the neck of a peninsula formed by the Meuse, is a strong fortress, often besieged, but rarely taken. Bayard, in 1521, successfully defended it against Charles V. Charleville, only founded in 1G06, is a place of commerce and industry, with foundries, nail works, and manufactories of tools. In the valley of the Sormonne, which joins the Meuse near Mezieres, are the slate quarries of Rimogne. Still descending the ileuse, we pass Nouzoti (5,225 inhabit- ants), which manufactures nails, railway rolling stock, and agricultural machines, and Fumay (4,589 inhabitants), with immense slate quarries, and finally reach the S A 2 352 FRANCE. triple town of Givet (6,272 inhabitants), with its citadel of Charlemont, constructed by Charles V. Pipes, pencils, sealing-wax, gl^e, and hardware are manufactured. Rocio;i (1,053 inhabitants), on the cold plateau to the east of the Meuse, is an important fortress. The south-western portion of the department is drained by the river Aisne. Its most important town is Rethcl (7,364 inhabitants), formerly a fortress, with Fig. 263.— Epixal. Scale 1 : 30,000. Ualf a Mile. manufactures of merinos. Ascending the river, we pass Affif/»;/, where the Merovingian and Carlovingian kings frequently resided, and Wittekind, the chieftain of the Saxons, was baptized, and reach Vouziers (3,425 inhabitants), at the head of navigation. Gerson, the birthplace of the famous Chancellor of the Paris Universit}', stood a few miles to the north of Rethel. VosGEs is the name of a department bounded by the Vosges Mountains in the VOSGES. 353 east, but occupied for the greater part bv the Monts Faucilles, which form the water-shed betweon the Rhine and the Saoue. Its nortliern portion is drained by the rivers Meurthe, MostUe, and ileuse, whilst the Saune and several of ita tributaries rise in the south-west. The climate is inclement, and one-fourth of the country is covered with forests. The manufacture of pai>cr and of co:ton stuffs is of importxiuce. Neiifihatcan (.■J,l).20 inhabitants) is the only town on the ileuse, which crosses the western corner of the department. It is the Noviomagus of the Romans, and Roman remains abound throughout this region. Files, nails, and tools are manu- factured. Domreini/-la-Piicelle, the birthplace of Joan of Arc, is close by. In the valley of the Vair, which joins that of the Meuse, are the mineral springs of Contrejrecille and Vittel. The neighbourhood of the latter is noted for its tine oak forests, and there are glass works and iron forges. Mirt'voiirf (5,169 inhabitants), on the Madon, a tributary of the Jloselle, has tan-yards, and manufactures violins, organs, and other musical instruments. Much lace is made in its neighbourhood. The river Moselle, not far from its source, flows past Biissaiig (798 inhabitants), noted for its gaseous springs. Retniremoiit (7,211 inhabitants), delightfully situated at the confluence of the Moselle with the Moselotte, has a fine old abbey, now used as a court of justice, a library, and a town-hall. La Brcsse (1,50G inha- bitants), in the picturesque valley of the Moselotte, is known for its cheese, butter, and wood car\'ings. There are several cotton-mills lower down on the river. The Valley of AJol, near Remiremont, with its numerous villages, is famous for its picturesque beauties. Still descending the iloselle, we arrive at Epinal (13,827 inhabitants), the capital of the department. The town possesses a fine picture gallery and rich geological and archtcological museums. Coarsely painted images of saints are manufactured, and the number of cotton-mills has largely increased since the annexation of Alsatia hy Germany. Chamagne, a village lower down on the Moselle, is famous as the birthplace of Claude Gelee, known as Claude Lorraine. Gerardmer (2,331 inhabitants), a town in the valley of the Yologne, which joins llie Moselle above Epinal, is the principal seat of the wood-carvers, and a hand-loom is found in nearly every house. Rambervillers (4,910 inhabitants), on the Mortagne, a tributary river of the Meurthe, is surrounded by factories and hopgardens; \)\xt St. Die (12,020 inha- bitants), on the Meurthe itself, far exceeds it in importance. The cathedral and several of the other churches are venerable for their age. Cotton stuflls, carpets, hardware, and paper are manufactured, and there are numerous saw-mills. Raon-rEfupe (3,G0l inhabitants) is the principal place in the Vosges whore paper is manufactured from aspen-wood. Moi/enmoulier (1,622 inhabitants) and Senonea (2,542 inhabitants) are two old towns in the valley of the Rabodeau, each with a cotton-mill installed in an ancient castle. There are no large towns in that portion of the department which lies within S54 FRANCE. tlie basiu of the Saone. Plomhieres, to the south-west oi Remiremont, is noted for its hot and cold springs, which attract thousands of visitors annually. Bains, a village farther west, has springs equally efficacious as those of its more popular neighbour. Xertigny (^2,025 inhabitants), Fontenoy-Je- Chateau (1,738 inhabitants), and other villages in the neighbourhood engage in the manufacture of nails, cutlery, and tools, and embroider lace for Paris houses. Meurthe-et-Moseli.e, the principal river of which is the Moselle, with its tributary the Meurthe, includes two-thirds of the old department of Meurthe and about one-fifth of that of the Moselle, the remainder having been surrendered to Germany. The country is generally well cultivated, its mineral wealth con- siderable, and its industry flourishing. Iron and steel, glass, china, and paper are the principal articles produced. Baccarat (5,128 inhabitants) is the first town on the Meurthe lying within the department, and is famous on account of its glass. Lttnicille (15,878 inha- bitants), at the confluence of the Meurthe and the Vezouze, manufactures watch glasses, and carries on much commerce. The treaty of 1801 was signed here, and in the eighteenth century Luneville was the residence of the Duke of Lorraine, whose palace has been converted into barracks. Blnmont (2,337 inhabitants) and Circy (2,324 inhabitants), both on the Yezou.ze, are small manufacturing towns, the former having a cotton-mill, the latter glass works. Once more descending the Meurthe, we pass St. Nicolas-dii-Povt (4,109 inha- bitants), from which the salt obtained from the mines in the vicinity ia exported, and reach Nancy (66,303 inhabitants), the ancient capital of Lorraine. In the seventeenth century this was a small ill-built town, for modern Nancj'-, with its wide and straight streets, was in reality founded by Stanislas, father-in- law of Louis XV. A triumphal arch, numerous statues, a ducal palace, now converted into an archteological museum, remind us that Nancy formerly had a court of its own ; but the most interesting building of the town is the Franciscan church, in which are several fine monuments of the Dukes of Lorraine. Nancy has its university, a librarj', a natural-history museum, and botanical gardens, and is ambitious of becoming the mediator of scientific thought between France and Germany. Several of the great cotton lords of Alsatia have transferred their mills to Nancy and its vicinity, besides which the manufacture of cloth, of hats, and of artificial flowers is busily carried on. Frouard (2,404 inhabitants), at the confluence of the Meurthe with the Moselle, has been strongly fortified since the war. Pont-u-Mousson (9,904 inhabitants), on the Moselle, was the seat of a university up to 1763. It is important now on account of its iron works and needle manufactories. Pagny, on the German frontier, is an important customs station. The ruins of the feudal fortress of Pr^nj', the finest in all Lorraine, are near, and Roman antiquities abound through- out this region. Toul (9,566 inhabitants), on the Moselle, an old episcopal city, boasts of two fine Gothic churches. As a fortress defending one of the great historical high- ways of France it has been frequently besieged, and ofcen taken and devastated. 3F THE 'JNIV£f?S/TY of ILLINOIS. MEURTHE-ET-MOSELLE. 855 Abuve the town the canul couneeting thu Muruu with the Rhiuu its curried ucro88 the Moselle. The narrow slip of territory in the north, ull that remains to France out of the old depurtnient of Moselle, has Brivy ('2,U'J'J inhabitants), to the north-webt Fig. 264.— NA.Ncr. Pnilr 1 : ,v>,iii«. 'zJ 3" io E of Paj-o 1 Mile. uf Metz, for its cajntal. South of it is the village of Murs-la-Tour, rememberetl in connection with the events of 1870. Loinjin/ (2,939 inhabitants) and Loixjiii/oii (2,020 inhabitants), both on the Chicrs, close to the Belgian frontier, have iron works, forges, and other industrial establishments. Longwy is defended by a citadel. CHAPTER XIV. STATISTICS OF FRANCE.* Population. nlN order to enable us to judge of the strength of a nation we must carefully inquire into the statistics available with respect to it, and weigh their import. Such an inquiry we now propose to institute. History may exhibit the genius peculiar to each nation, but statistics certainly make known to us the resources available for continuing the struggle for existence. " The future of a nation," says a Japanese proverb, " lies in its present, as the unfledged eagle lies within the shell of its egg." One great fact meets us at the outset of our inquiry. The population of France has vastly increased since the Revolution, and men live longer now than they did formerly. Still that increase has not been as rapid as in most other countries of Europe, and there were actually periods when the population decreased.! The calamities of the war of 1870-71 are plainly indicated in the population statistics. But there are other causes which retard the increase of the population of France. The number of births in excess of deaths was 172,950 in 1872, 101,775 in 1873, and 131,920 in 1876, which is far less than in other countries; and whilst at the beginning of the century Frenchmen constituted one-fifth of the European popu- lation of the world, they now constitute only one-tenth. Physical degeneration is not the cause of this slow increase, for the number of exemptions from military service granted on account of physical infirmities is decreasing from year to year. The large number of bachelors and spinsters is certainly one of the causes, for 500,000 soldiers and sailors are not allowed to marry, 200,000 priests and nuns have taken vows of chastity, and many others are compelled by circumstances to lead a life of ceUbacy.J But there are other causes, • M. Block, "Annuairede I'Economie Politique" and "Statistique de la France;" E. Levasseur, " La France avec ses Colonies; " L'Economiste Fran^ais ; Journal des Economistes. t Population within present limits of France :— 36,469,836 in 1866; 36,102,921 in 1872; 36,905,788 in 1876. X Of every 100 Frenchmen 21 years of age and upwards, 51 are bachelors, 41 are married, and 5 are widowers; of every 100 women of the same age, 48 are spinsters, 40 are married, and 11 are widows. POPULATION. 867 of a moral nature, and fur more deep-soatod. Purcuts, led by the very luudablu desire of leaving their children well provided for, take cure that their number is limited. Some philosophers may approve of this solicitude, but it cleurly exliibits much want of faith in tlic future, and substantially weakens the strength of the country, as compared with other countries. In poor departments more children are born, as a rule, than in rich ones. A poor man may teach each of his children a trade ; a rich one is expected to divide his capital amongst them when he dies. Fig. 265.— I.NCUE.KSE OF PoPCLATIOS IN TUB PulNClPAL C0UNTUIE3 OF TlIK WollLD. In Normandy this voluntary limitation of families is carried to the greatest length , in the department of Eure one-eighth of the inhabitants lead a life of celibacy, and there are few families with more than two children. Need we wonder that the population decreases ? Frenchmen are the most sedentary of Europeans. The "trappers" and "voyageurs" of Canada prove that they are quite able to accommodate them- selves to the rough life of a colony ; but, for all that, thej' prefer to remain at home. Even in Algeria, which lies within easy reach, but few Frenchmen 858 FEANCE. are met with as voluntary settlers.* In fact, the number of foreigners who annually immigrate into France far exceeds that of Frenchmen who leave the country. Migration is going on actively within the limits of France. The rural popula- tion is steadily moving into the large towns. In 1830 three-fourths of the iuba- Fig. 266. — Density of the Popvlation in Fraxce (1872). I J Densiiti Au"J thaiL' the. ''Ar'" M E D I T £ It n A .V JS.4-V ^l-*^ jMtfi^'^CC^ Ov^j^ maaev Cvt lAj M — law \ tm* E~3 Cr *»yt^ t^^ ,•*},/ *r'f IT r ^ Cc^C^a/ tt^£fP«rii 0? JtofCr. Over' 10. "/<, tS-ctpVa to-^SpS^o J—iop.^o NaJxu-Ai'' nasturcJ Aiea of pastui'es, 1^,415,000 acres j of meadows, 6,727,SS1 acres. cover the costs of transfer. In some parts of France large estates are increasing, and most of the land is cultivated by farmers. Elsewhere the subdivision of the soil is progressing at an increasing rate. Upon the whole, however, the number of proprietors is becoming larger from year to year. Wealthy peasants certainly endeavour to increase their estates, but they understand very well that land only repays their outlay if thej' are able to cultivate it themselves. "Agricultural AGEICULTUEE. 86S distress" really exists only amongst the large proprietors, who are called upon to pay mucl) higher wages now than formerly.* Small j)roperties have their advantages, no doubt ; but tliey do not admit of agricultural operations on a large scale, uud the soil produces less. In France the subdivision of the land is excessive. The number of " plots," or patches, is no less than 127,000,000, divided amongst 3,025,877 cultivators, of wlioiu each owns on Fig. 270.— AvEKAOB Valve of AouiriLTiHAL Phodvce, that of the Vineyakub exceitei). According to Delease. • o'iM.of pzrr' HE D I TERRAKEXV Clear I^tnnc framj eaicjty Seclarey l/v l&Si- Siga ssm sa iHi ^m czzi lOo frtuus d over Stj: Soy. it J, ^ff. Lui thmvxo franu £4 and ovfr. £3 49. £2 89. £1 12s. 16s. Less thnn Ifis. an average about 36 acres. No less than 2,435,401 own less than 25 acres each, and only 154,107 more than a hundred. This multitude of small fields necessitates a multitude of roads, and agricultural inacliiuery, sucli as the steam plough, cannot be employed with advantage. The yield is less than in countries where large estates are the rule ; and whilst in England an acre yields from 20 to 28 bushels of • Agricultural wages formen daily in 1700, 6d. ; in 1811, 9d. ; in 1852, Is. 4d. ; in 1872, 1». 6d. 864 FRANCE. wheat, it only yields from 14 to 17 in France. If French agriculture is to attain a position comparable with French industry, the land must be cultivated on sounder principles than now. The peasant proprietors must either combine for the common cultivation of their plots, or they will have to be ousted by the State or by companies of capitalists. Drainage and irrigation works on a large scale cannot be carried out under existing conditions. All that has been done hitherto in this direction in France is patchwork. But tradition is strong among the peasantry. The model farms, thirty-three in number, appear to be appreciated, but the three agricultural schools at Grignon, Montpellier, and Grand Jouan are but indifferently attended. More than half the area of France is cultivated in an antiquated manner. There are vast stretches of heaths in the Pyrenees, in Gascony, and Brittany, which might easily be con- verted into arable land. The swamps on the Atlantic coast have only in part been converted into meadow land ; the Caraargue and the littoral region of Languedoc still breed fevers ; the rivers almost annually inundate their banks ; and m the Alps, the Cevennes, and the Pyrenees the country is becoming unin- habitable on account of the forests no longer preventing the vegetable soil being carried away by the torrents. Nearly 20,000,000 acres are covered with forests, but most of the timber used is imported from abroad, the country annuallj' pa3'ing four millions for that commodity. It is supposed that there are 2,718,000 acres of land which might advantageously be planted with forests, but even supposing this work to be taken in hand with vigour, a century must pass before its full benefit will be felt. Mixing. The mineral wealth of France is perhaps less than that of any other country of equal extent. Neither platina, gold, silver, nor mercury is found, or at most in very small quantities. The mines of zinc, nickel, tin, lead, antimony, manga- nese, and copper yield but little, and France consumes ten times as much as they yield. The iron ores are of importance, but unfortunately they are found, as a rule, far away from coal, which is indispensable for their conversion into iron. The coal raised does not cover the home demand. The coal basins, though inferior to those of England or Belgium, are sufficiently extensive, but being for the most part situated in the interior of the country, the cost of transporting the coal to the centres of industry is very heavy. In building materials of every kind France is exceedingly rich, and most of the towns are built of solid stone. Clays suited to the manufacture of earthenware abound. Beds of phosphate were discovered in 1857 in Southern France and in the North, where they cover 494,000 acres. Salt-pans abound on the coast ; saline and all kinds of mineral springs in the interior of the countrj', more especially in the Pyrenees, in Auvergne, in the Alps, and in the Vosges.* • Mineral productions about 1876 : — Pig iron, 1,449,.538 tons ; iron birs, 733,272 tons ; steel, 254,191 tons; coal, 7,047,761 tons; copper, zinc, lead, tin, &c., value £380,000 ; salt, 754,506 tons. MANUFACTURES. 8G5 MaNIKACTI'KKS. The industrial progress mado by France has been enormous. In articles requiring taste and deft workraansUip that country preserves its traditional pre-eminence, and in many other objects, including machinery, it has become a rival of England. In IS'20 there were only 20 steam-engines in all France; in 18G9, 32,H27, includ- ing locomotives and ships' engines. These engines do the work of 25,000,000 labourers. Nearly 10,000 mill streams set in motion the wheels of 80,000 mills, and recentlj' even the tides have been pressed into the service of man as a motive power. The great centres of industry are Paris, Lyons, and Lille, but not a depart- ment exists now where the steam-engine is not at woi"k. 'Wherever coal mines are opened factories spring up overnight. The beds of iron ore, of clay, or kaolin, likewise attract manufacturers, and so do the commercial towns on the sea coast. The mountaineers, whom long winters debar from their usual occupations. Fiir. 271. — The Increase of Steam Ekgixes sixce 1840. iftfo jrj>. — — — — — 1 '~~ — — — "^~ 1 — p— -"" ,__ _ J •' ^ /' y ^ , -p' ^ ^ — -^ — — — 1 — — — ' — ' — — ^ ■*— — — — — — ^ ^ / X y ^ — ^ — ' — , ~-t f5 ftH 1 iSi m m m m E m m m M m w. ^ M ^S 2^^ m & usJMs M m im m Somraw engage in various industries. The women of Velay, Auvergne, and the Yosges are famous as lace-makers ; in the Jura the men carve in wood or make watches. The textile industries alone occupy more than 2,000,000 hands. The silks of France are the best in the world ; in woollen stuffs, cloth, carpets, and flannels it successfully competes with England ; whilst in cottons it excels in quality, if not in quantity. The lace manufactured in France probably equals in value that produced in any other country ; and the manufacture of linens and other textile fabrics is likewise of considerable importance. M. Block estimates the textile fabrics and the clothing produced annually at the enormous sum of £192,100,000.* In all other branches of manufacture France holds a distinguished position. Its iron industry is far inferior to that of England, but enormous progress has been made. Up to 1830 nearly all machinery was imported from England, whilst • Silks, 200,000 hands, £36,000,000 ; woollen stufTs, 180,000 hands, £48,000,000 ; cottons, 250,000 hands, 6,200,000 spindli-s, £20,000,000; linen, &c., 150,000 hands, £12,000,000 ; mixed stuffs, 100,000 hiinds, £16,000,000 ; lace, 240,000 hands, £4,800,000; clothing, 1,200,000 hands, £56,000,000. Vol .II. U U 86G FRANCE. French machinery now finds its way into every quarter of the world.* The manufacture of beet-root sugar, which originated during the First Empire, now emploj's 73,000 workmen, who produce more than 400,000 tons of sugar annually, as compared with 7,000 tons in 1827. The great chemical works are another creation of our century, and annually increase in importance. Chemistry, indeed, has exercised a most potent influence upon every kind of industry, unfortunately not in every instance for the best. In every branch of art industry, such as the manufacture of furniture, jewellery, china and glass, bronzes, and engravings, France still maintains her superiority, though Germany excels in china and glass, and England, where many of the workmen are French, in ceramic productions. M. Maurice Block in 1875 estimated the productions of French industry at £511,680,000, not including ships or heavy machinery. f The factories and small workshops contribute almost equally toward this vast sum. These latter, how- ever, are fast disappearing, not being able to sustain the struggle against powerful capitalists. This concentration of the working popidation in huge establishments is the greatest social feature of our century, and future generations will have to deal with it.* Commerce. The progress of commerce has kept pace with that of agriculture and industry ; and three towns, viz. Paris, Marseilles, and Havre, do a greater trade now with foreign countries than the entire nation did fifty j'ears ago. A network of roads covers nearly the whole of France, but the mountain districts are as yet ill provided with them. Only one road leads across the Pyrenees ; two, those of Mont Cenis and Mont Genevre, across the Alps. The high-roads of France (1872) have a length of 102,870 miles; the provincial carriage roads of 156,030 miles; and 138,900 miles more are being constructed. The rivers and rivulets of France are spanned by 2,000 large, and more than 200,000 small bridges. The railway age only began in France in 1832, when a line connecting Lyons with St. Etienne was opened for traffic. Railway building up to 1842 made but little progress, and even now much remains to be done before the system of rail- ways can be called complete. Lines radiate from Paris in all directions, but many provincial towns are still deprived of this means of locomotion. In 1878 France * Iron industry (1875) :— Castings, 14,157,000 tons; fashioned iron, 7,5o4,000 tons; steel, 2,.516,O00 tons. t Textile fabrics and clothing, £183,800,000 ; articles of food, £117,180,000 ; buildings, £67,200,000 ; metals, £34,600,000 ; chemical products, including soap and candles, £30,000,000 ; furniture, £22,000,000 ; leather and skins, £16,000,000; jewellery, £8,000,000; earthenwaie and glass, £6,000,000; paper and instruments, £6,000,000 ; various, £12,000,000. X Distribution of French workmen in 1874 according to 51. Ducarre: — Mines 14,117 masters 164,819 workmen '\ Factories 183,227 „ 1,420,006 „ ( Including families, Small Workshops . . .596,776 1,060,114 „ j 8,400,000 persons. Total . . 794,120 .. 2,644,9f0 -) LIBRARY OF THE !lN!VFRQiTv ,f ILLINOIS, COMMERCE. 8G7 had 13,072 miles of railway, coustruct«jd, for the most part, in a very substantial and conscientious manner. On an average each mile cost £28,800. Plans for the construction of additional lines, and more especially of great trunk lines, affording the most direct, and consequently the cheapest, conunuDic-ulious for tlio transit of passengers and merchandise, are now under consideration. One of these projected lines is to connect Calais with Dijon, without passing through Paris. Another, piercing the Alps at the .Sinijilon I'ass, will pl;ieo I'aris in direct communication with Upper Italy. The railways of France are the property of six great companies, and this Kig. 272. — The Haii.ways of FitANrK. d ^ -J 51 t\ S 'L '' 'V"«~H 1> 1-' 1* V» f \7 4 "^ ^^^^^^ {^^^J^^^^d to ^ ^ V^ r?T7^ -^^wui^M'"^ c ^ ' ^5^^^ ^^^^^R^^vS^'^^V^^^ U '^^^''l^^^^^^^^^i^''^-^^^^^^^^^^r\^ '^ .^VJ~^^ ^-k?y^^^^^VA^^K^ "X ^^ ^1^^'^^^^^P^^^^d^i ^x* — is V»3 '^^i<)f^f^^-X\ ^^?S^^S^^*' O t6 O ^^^^^^^m"^' U t* -^^^^^^ > ij » jZ^iw^ "^ ^ ^r^F^^twffiliJJfrlk? ^^^ ^'^'^fTEBRAn e Ajv ij y"^ ^N/^M>^^9]SriMR/^&^%j^"~ ''■ 'j7~ — ^ ■- ' '/ ,- : -1 t '■! 1 z centralization is by no means an unmixed good. Rival lines are opposed, and arbitrary rates charged for the conveyance of merchandise. The charges of the Great Southern Line, for instance, are so exorbitant that it is cheaper to forward goods from Paris to the East by way of Liverpool than by way of Marseilles. General interests thus suffer to promote private ends. The progress of railways has withdrawn public attention from the canals, which afford a much cheaper means of conveyance. No new canals have been constructed since 1820, and those existing are for the most part of local importance only. In II II 36S FRANCE. their construction no general guiding principle has been adhered to, and tranship- ment is frequently required. Of late years, ho'wever, the importance of canals and other navigable highways has attracted public attention, and !M. Krantz has suggested a scheme, the execution of which would meet every reasonable want at an expenditure of £33,200,000, and would likewise provide for the " regulation " of some of the most erratic rivers. The existing canals have a length of 3,051 miles, and cost £32,740,000 ; the length of the navigable rivers is only 3,541 Fi?. 273. — The Canals a.nd Navigable Rivers op France. miles ; and 1,564,666,000 tons of merchandise were conveyed by water in 1872, the conveyance of a ton per canal costing 0'8d. a mile, including interest upon the capital expended. France is poor in good natural harbours, and it is therefore aU the more necessary that artificial ones should be created. This subject, too, has recently received attention, and one great artificial port, very much needed, is being con- structed at Boulogne. COMMKRCK. 8G9 France is admirably situak>ire (Haute-) . Loire-Infericure Loirct .... 1,838 1,916 2,654 2,614 650.611 308,732 602.706 353,021 690,613 313,721 612,972 360,903 321 1C4 231 138 3 3 5 4 30 28 46 31 328 262 215 319 St. Etionne. I^ Puy. Nantes. Orleans. Lot Ix>t-et-Garonnc . J>07.ire . . . . ilaine-et-Loire . 2,012 2.067 1,996 2,749 281,404 319,289 135,190 518,471 276.512 316,920 138,319 817,258 137 153 69 189 3 4 3 5 29 35 24 34 321 319 194 380 Cahors. Agin. SlonJe. Angers. Mamhe . . . M.Tcnee9 '(Hautes-) ) ' P>Tenees- 1 Orientales } * 2,261 2,354 2,551 3.070 ) 2,943 1,749 1,592 396.804 398,250 761,158 566,463 426,700 235,1.56 191,856 401,618 392.526 793,140 570,207 431,525 238,037 197,940 177 167 311 186 147 136 124 4 4 6 5 5 3 3 35 36 44 60 40 26 17 701 611 904 456 558 480 231 Beauvais. Alencjon. Arras. Clermont-Ferrand. Pau. Tarbes. Perpignan. Rhone . . . . Saone (Haute-) . Saone-et-Loire . Sarthe . . . . 1.077 2,062 3,302 2,396 670,247 303,088 598,344 446,603 70.5,131 304,052 614,309 446,239 653 147 186 186 2 3 6 4 29 28 60 33 264 583 683 386 I-yon. Vesoul. Macon. Le Afann. Savoie .... Savoie (Haute-). Seine . . . . Seine Inf erieure 2,224 1,667 184 2,330 267.958 273,027 2,220,060 790,022 268,361 273,801 2,410.849 798,414 121 164 13,102 343 4 4 3 5 29 28 '-8 51 227 313 72 759 Chambery. Annecy. Paris. Kouen. Seine-et-llame . Seine-et-Oise . Sivres (Deux-) . Somine 2,215 2,164 2,317 2,379 341,490 680,180 331,243 557,015 347,323 561,990 336,655 556,641 157 260 145 235 6 6 4 6 29 36 31 41 629 685 356 833 JJelun. Versailles. Niort. Amiens. Tarn .... Tam-et-Garonne Var Vaucluse . . . 2,217 1,436 2,349 1,370 3.52,718 221,610 293,757 263,451 359,232 221.364 295,763 255,703 162 154 121 187 4 3 5 4 35 24 28 22 317 194 145 150 Alby. Montauhan. Dniguipuan. Avignon. Vendee . . . Vienne .... A'ienne (Haute-) y.jsgts. . . . Yonne .... 2,688 2,691 2,130 2,266 2,868 401,446 320,.i98 322,447 332.988 363,608 16,102,921 411,781 3.10,916 336,061 407,082 359,070 16^906,788 100 123 157 179 126 3 30 5 31 4 27 6 29 6 37 362 2,863 298 300 202 631 485 36,056 Roche-sur-Yon. Poitiers. Limoges. Epinal. Auxerre. Tot*l . . ." 204,091 ! 384 FEANCE. Area and Population of French Colonies. Area. Inhabitants Engl. Sq. Population. to a Sq. MUes. Mile. Africa: — Algeria .... 122,912 2,867,626 23 Senegal 62,000 221,000 3 Gabon .... 100 5,000 50 Reunion 764 183,163 239 Mayotte, &c. 257 26,196 98 Asia : — India .... 196 271,460 1,385 Cochinchina . 21,707 1,600,000 74 Cambodia (protected) . 32,380 890,000 27 America: — St. Pierre and Miquelon 81 5,481 68 Guadeloupe . 720 173,149 240 Martinique . 381 160,831 422 French Guiana 46,848 32,500 0-7 Polynesia :— New Caledonia 6,78.") 68,300 9 Loyalty Islands . 830 13,334 16 Marquesas . 478 6,011 13 Clippertou . 2 no inh. Tahiti (protected) . 438 10,703 25 Tubuai, Vavitu, Oparo (do.) 56 700 13 Tuamotu Arch, (do.) 2,670 8,000 3 Gambier Islands (do.) . Total Colonies 12 1,.500 125 299,517 6,633,954 22 France . 204,091 36,905,788 181 Grand Total . 603,608 43,439,742 86 FEANCE ; Its Departments, Natural Regions, and Principal Communes in 1876. Each Commune consists of a town and its environs. Its population, therefore, is greater than that of the town bearing the same name. In the text the population of the towns is given. Departments. CORSE (COR- SICA). ArrondissementB. Ajaccio, Bastia, Calvi, Corte, Sartene. Natural Regions. Banda di Dentro, Banda di Fuori. Communes of over 5,000 Inhabitants. Bastia (17,572), Ajaccio(17,050). THE PYRENEES, THE LANDES, AND THE BASIN OF THE GARONNE. PYRENEES- ORIENTALES. ARIEGE. HAUTE-GA- RONNE. PYRENEES (HAUTES-). PYRENEES (BASSES-). 6ERS. TARN-ET-GA- RONNE. LOT-ET-GA- RONNE. Perpionan, Prades. Ceret, Foix, Pamiers, St. GiRONS. Toulouse, Muret, St. Gaud ens, Villefranche. Tarbes, ARQELiS, Baqn^kes. Pau, Bayonne, Mau- lEon, Oloron, Orthez. AucH, Condom, Lectoure, Lo.m- BEZ, MiRANDE. JIoxtauban, Castel- Sarkasin, Moissac. Aden, Mahmande, Nerac, Ville- necve-d'Agen. Capsir, Val de Segre, VaUespir, Aspres, Valleys of the Tet, the Agly, Salanque, &c. Valley of the Ariege, Couse- rans, &c. Lauraguais, Couserana, Com- minges, Nebouzan, Quatre- VaUees,Lomagne,Toulousain. Valleys of the Aure and the Adour ; Plateau of Lanne- mezan, Nebouzan, Astarac. Valley of the Gaves of Beam, Soule, Labourd, Lower Navarre, Landes, Touyas. Comminges, Astarac, Arma- gnac. Plateau of Quercy, VaUey of the Garonne, Lomagne. Agenais, Lomagne, Armagnac. Perpignan (28,353), Rivesaltes (6,329). Pamiers (8,967), Foix (6,362). Toulouse (131,642), St. Gaudeus (5,955), Revel (5,613). Tarbes (21,293), Bagnferes (9,508), Lourdes (6,471). Pau (28,908), Bayonne (27,416), Oloron Sto. Marie (8,644), Orthez (6,624), Hasparren (6,566), Biarritz (5,507), Salies (5,140). Auch (13,785), Condom (7,873), Lectoure (6,507). (26,952), Moissac Castel-Sarrasin Montauban (9,137), (6,906). Agen (19,503), VUleneuve (14,448), Marmande (8,961), Tonneins (8,199), Nirac (7,586). DEPARTMEXTS, NATURAL REGIONS, AND PRINCIPAL COMMUNES. 385 THE PYRENEES, TUE LAKDES. AND THE BASIN OF THE GARONNE— (OwriHiiorf). DepulBMBti. LANDES. GIRONDE. Antndianmanta. Mont-db-Mabsan, Dax, St. Sever. BoBDKAi'X, Bazas, Blaye, La H£ulb, Lbspauhe, Li- BUL'KXE. Natnnl Bagiooi. Landce, Buch, MaranBin, Cha- losse. London, JI6doc, Bordclnis, Baza- dais, Benangc, Entre-Ueux- Mers, Libounmu, Blayais. Com m une* of over &,000 InhaUtaaU. Dax (10,260), Mont-do- Manuin (9,310). Bordeaux (216,140), Libourno (15,231), Bigles (6,202), Caud6ran (6,3U6), La Toate (6,311), Bazas (6,073). THE ALPS, THE RHOXE, AND THE MEDITERR.VNEAN COAST REGIONS. AUDE. HERAULT. CARD. ARDECHE. BOUCHES-DU- RHONE. TAB. ALPES-MARL TIMES. VAUCLUSE. ALPES (HAUTES-). ALPES (BASSES). dr6me. ISERE. SAVOIE. SAVniE (UAl'TE-). Cariassos.ve, Cas- TELNAIDAKV, Ll- Morx, Narbosse. MONTPBLLIER, B£- ZIBB8, LOD^YE, St. Pons. NiMEs, Alais, Lk Vioan, Vzis. PRrvAs, Labgen- TltRE, TOIRKO.N. Marseille, Arles. Aix, Dbaguiokan, Bai- OXOLES, TOCLON. Nice, Grasse, Pu- oet-Tuemers. Avignon, Apt, Cab- PBSTBA8, OhANOE. Gap, Bbiakcon, Embrl-x. Digne, Barcelok- NETTE, CaSTEL- lane, Forcal- QUIBR, .SiSTERON. Die, Mont£limabt, Nyoss, Valence. Grbxoblb, La Tour- Dv-Pis, St. Mah- CELLO', ViENSE. Ciiaxb£bt, Albebt- TILLE, Moi'TIEUK, St. jEAM-DE-MAt- rikknz. Aknecy, Bovsi- VILLI, St. JVLIEM, Tuoson. Monbigno Noire, Corbiires, RazO'S, Laiuaguais, Valley of the Aude, Lagoons (Etangs). Cevennes, Valleys of the Lez, the H6rault, the Orb, and the Aude, Lagoons. Cevennes, Valleys of the Gardons, A'auuage, Garrigucs, Marshes, and Dunes. Mountains of Vivarais, Coiron, Valley oi the Rhone. Camargue, Crau, Valley of the Durance, Hill Region, Shore Region. Basin of the Argens, Mountains of the Moors, Valley of the Gapeau, Shore Region. Valleys of the Roya, the Vesu- bie, the Tinee, and the Var, Shore Region. Ventoux, Leberon, Palus, Valleys of the RhGne and of the Durance. Que}Tas, Oisans, Champsaux, Devoluy. Mountains of Upper Provence, Valley of the Durance. Devoluy, Diois, Forest of Saou, Tricastin, Valley of the Rhone. Oisans, Devoluy, Lans, Vercors, Grande-Chartreuse, Grandcs- Rousses, Sept-Laux, Graisi- vaudan, Bifevrc. Plain of Savoy, Bauges, Mau- rienne, Tarentaise. Genevois, Faucigny, Chablaia. Carcassonne (26,971), Narbonne (19,968), Castelnaudary (9,042), Limoux (6,661). Montpellier (66,268), Beziers (38,227), Cette (28,690), Lodeve (10,628), Lunel, (8,315), Agdo (8,261), Pfeenaa (7,966), Bcdarieux (7,961) M^zo (6,826), Oermont- I'Herault (6,964), St. Pons (5,809). Nimes (63,001), Alais (20,893), Besseges (10,668), La Grand'- Combe (10,162). Beaucaire (8,777), St. Gilles (6,302), Uzds (6,586), Le Vigan (5,389), Anduze (5,110). Annonay (15,848), Aubenas (7,781), Privas (7,763), Tour- non (6,083). Marseille (318,868), Aix (28,693), Aries (26,095), Tarascon (10,409), La Ciotat (10,058), Aubagne (8,027), Salon (7,021), Martigues (6,963), St. Remy (6,999). Toulon (70,609), Hyferes (12,289), La Se\Tie (10,656), Draguipnan (9,223), Bri- gnoles (5,840). Nice (53,397), Cannes (14,022), Grasse (13,087), Menton (7,819), Antibes (6,762). Avignon (38,008), Carpentras (10,479), Orange (10,212), Cavaillon (8,454), L'Isle (6,608), Apt (6,687), Pertuis (6,649), BoUtoe (6,478). Gap (9,294). Digne (7,222),Manosque(6,l36). Valence (23,220), Romans (12,923), Mont^limart (11,946), Crest (6,600). Grenoble (46,426), Vienne (26,502), Voiron (11,064), Bourgoin (6,021). Chamb^ry (18,545). Annecy (10,976), (6,501). Thonon 886 FEANCE. THE JURA AND THE BASIN OF THE SOMME. Departments. AIN. JUEA. DOUBS. EHIN (BAS-). SAONE (HAUTE-). COTE-D'OK. sa6ne-et- LOIRE. RHONE. Arrondissements. BouRG, Belley, G ex, Nantua, Trevoux. LONS - LE - SaUNIER, Dole, Poligsv, St. Claude. BESANfON, Bai'me- le,s-Dames, Mont- beliard, pontar- LIER. Belfort. VesouLjGiuy, Lure. Dijon, Beaune, CH.i- TiLLON-suii - Seine, Semur. M.icON, AUTUN, Ch-\- LON - SUR - SaoNE, Charolles, Lou- HAN'8. Lyon, Ville- FaANCHE. Natural Eegions. Jura, Bugey, Dombes, Bresse. Mountains and table-laud of the Jura, Bresse, Finage. Mountains and table-land of the Jura. Gap of Belfort. Vosgos, FauciUes, Mountains of Lure, Valley of the Saone. Morvan, Auxois, Chatillonnais, Cote-d'Or, Plain of the Saoue. Morvan, Autunnaia, CharoUais, Brionnais, Bresse. Mountains of Lyonnais and Beaujolais, Valleys of th( Saone and the Rhone. Communes of over 5,000 Inhabitants. Bourg (15,692). Dole (12,924), Lons-le-Saunier (11,8'Jl), St. Claude (7,-550), Salins (6,271), Morez (6,419), Arbois ( 5,027 ), Poligny (5,010). Besau<;on (54,404), Montbeliard (8,938), Poularlier (5,714). Belfort (16,173). Vesoul (9,206), Gray (7,401), Fougerolles (5,459). Dijon (47,939), Beaune (11,421), Auxonne (6,532). Le Creusot (26,432), Chalon- Bur-Saoiie (20,895), Macon (17,570), Autun (12,8891, Montcuau-les-Mines (11,011), Tournus (5,527). Lyon (342,815), Tarare (14,383), Villefranche (12,486), Givors (11,910), ViUeurbanne (9,033), Caluire - ct - Cuire (8,702), Amplepuis (6,915), Coura (6,157), OuUins (5,674), Venissieux (5,224), Ste. Foy- lea-Lyon (5,118). THE CENTRAL PLATEAU. lozere. LOIRE (HAUTE-). AVEYRON. TARN. LOT. CANTAL. PUY-DE- DOME. CORREZE. DORDOGNE. VIENNE (HAUTE-). CREUSE. ALLIER. Mende, Flokac, Marvejols. Le Puy, Bkioude, yssinoeaux. RoUEZ, ESPALION, MiLLAu, St. Af- FRIQUE, VlLLE- FRANCHE. Alby', Castres, Gaillac, Lavaur. Cahors, Figeac, GOURDON. AURILLAC, MaURIAC, Murat, St. Flour. Clermont-Ferrand, Ambert, Issoire, RioM, Thiers. Tulle, Briye, Ussel. Perigueux, Ber- GERAC, NoNTRON, Rikekac, Sarlat. Limoges, Bellac, Roche - Chouart, St. Yrieix. Guebet, Aubusson, BoUROANEUF, BoUSSAC. MOULINS, Gannat, La Palisse, Mont- lUfON, Plateau of Gevaudan. Plateau of Velay. Causses, Segales, Hills of Kou- ergue. Montague Noire, Hills of La- caune, Sidobre, Albigeoia. Causae of Lot, Valleys of the Dordogne and the Lot. Cezallier, Cantal, Placeze. Plateau of Auvergne, Mountains of Forez, Valley of the Li- magne. Plateau of Limousin. Perigord, Nontronn.'iis, Sarla- dais. Valley of the Dordogne, Double. Plateau of Limousin. Plateaux of Marohe and Li- mousin. Plateaux of Bourbonnaia, Val- leys of the Loire and the Ailier. Mende (7,300). Le Puy (19,250), Y'ssingeaux (8,371). Millau (15,695), Eodez (13,375), Villefranche (10,124), Aubin (9,864), Decazeville (9,547), St. Afifrique (7,622). Castres (25,856), Alby (19,169), Mazamet (14,168), Gaillac (8,124), Lavaur(7,563).Graul- het (6,940), Cai-maux (6,160), Rabastens (5,161), Pay lam-ens (5,141). Cahors (13,660), Figeac (7,333), Gourdon (5,098). Aurillac (11,211), St. Flour (5,381). Clermont (41,772), Thiers (16,343), Riom (10,801), Issoire (6,250), St. Remy (5,572). Tulle (15,342), Brive (11,920). Perigueux (24,169), Bergerac (13,120), Sarlat (6,554). Limoges (59,011), St. Junien (8,221), St. Yrieix (7,429), St. Leonard (5,989). Aubusson (6,847), Gueret (5,859). Montlu(;on (23,416), Moulins (21,774), Commentry (12,978), Vichy (6,428), Gannat (5,568), Cusset (6,308), Montvicq (6,242). DEPABTMENTS, NATUKAL KEOIONS, AN1> PEINCIPAL COMMUNES. 887 THE CENTRAL PLATEAU.— (C«»/iiiii«0- Departments. LOIBE. ArtoodiMemanta. St. Etienne, Mont- BRISu^', 1{UA.NNE. Natural Regioua. Hills of Foipz, Valley of llii Loixo, UcuujolaU. Commune* of over B,000 InhuUUnti. 8t. Etipnno (126,019), Itounno (22,797), Uivo - do - Gier (1.5,004),St.C'hiimond(U,420), Firminy (11,972). Chambun- Feugerolles (8,314), Rica- marie (6,700), Terronoire (6,378), Montbrison (6,363), St. Julien-en-Jarret (6,230), Chazelles-siir-Lyon (6,915), Tssieuz (0,194), Panissi&rcs (6,017). CHAREXTE AND VENDEE. CHARENTE. CH.\RENTE- INFERIEURE. VIENNE. SEVRES (DEUX-). VENDEE. AxGOl'LtME, BaRBE- ZIEIX, CoG.VAC, CONFOLEMS, BUF- FEC. La Rochelle, Jon- ZAT, ^IaHENNES, RoCHEFOKT, St. Jkan - n'A>'G£LY, Saintes. POITIEBS, ChATEI- LBKAl'LT, ClVRAY, LOCDU.V, MONTJIO- RILLON. NlORT, Bbesscire, Melle, Parthe- NAY. La Roche- srR- Von, Fo.NTEN A Y - le - Comte, Sables- d'Olonkes. Confolcnnais, Terres-Chaudes, Pays-Bas, Bois, Champagne, Double. Double, Champagne, Socage, Murais. Plateau, Valleys of the Vienne and the Chareute. Socage, Plain, Miirsh. Socage, Plain, Marsh, IslanJs. Angouleme (30,513), Cognao (14,900). Rochefort (27,012), La Rochelle (19,583), t>aint«8 (13,725), St. Jean - d'Angely (7,172), St. Georges (5,208), Royas (5,165). Poitiers (33,253), Chatellerault (18,053), MontmoriUon (5,105). Niort (20,923), (5,091). Parthcnay Roche - BUT - Yon (Napoleon) (9,755), Sables - d'Olonne (9,347), Fontenay-le-Comte (8,453), Lu<;on (6,247), Noir- moutier (5,787). THE SASIN OF THE LOIRE. NIEVBE. CHER. INDRE. LOIRET. LOIR-ET- CHER. EURE-ET- LOIR. INDRE-ET- LOIRE. MAINE- ET- LOIRE. SABTHE. MAYENNE. Neters, Chateav- Chison, Clamecy, Cos.se. BouROEs, St. Amand- Mont-Rond, San- CERRB. Chateaubocx, Le Blakc, La Ch.\tre, Ibsoudck. OblSans, Oies, MoNTABOIS, PlTHI- VIER8. Blois, Bohorantin, Venuome. Chabtbes, Chateai- DVK, Dbeix, No- OE>T-LE-RoTB0f. TofRs, Chinon, Loches. ANCEB«,SAfOfe, ChO- LET, SaVHUR, SECRi. Le Mans, La FlJche, Mameb«, St. Ca- lais. Laval, Chateav- Gontier, May - ZNX Morvan, Valleys of the Yonne and the Loire. Plateau, Sologne. CTiampagne, Bois - Chaud, Brenne. Solopne, Val, Puisaye, G&tinais, Forest of Orleans, Beauce. Beauce, Val, Sologne. Beauce, Dunois, Drouais, Thy- m^rais, Perche. Oatine, Varenne, C!hampeigne, Plateau of St. Sfaure, Brenne. Anjou, Valine, Mauges, Socage. Coevrons, Lower Maine, Beli- nois, Giitine. Cocvions, Upper Maine, (Traon- Dais. Nevere (22,704), Cosne (6,851), Fourchambault (5,884), Clamecy (5,432), La Charile (6,086). Bourges (35,785), Vierzon-Villa (8,995), St. Amand-Mont- Rond (6,499), Vierzon-Village (6,731), Mehun-sur-Y6vro (6,326), Dun-le-Roi (5,001). Chateauroux (19,442), Igsoudun (13,703), Le Blanc (6,122), Buzan(;ais (6,109), Argeutoa (6,582). Orleans (52,157), Montargig (9,176), Gien (7,555), Briare (•5,152), Pithiviers (6,006). Blois (20,515), Vendome (9,221), Romorantin (7,826). Chartrcs (20,468), Dreux (7,922), Nogent - le - Rotrou (7,638), Chateaudun (6,694). Tours (48,325), Chinon (6,301), Loches (5,085). Angers (66,846), Cholet( 14,288), baumur (13,822), Chalonnes- Bur-Loire (5,530), Trelaz^ (5,264). Le Mans (50,175), La Flicha (9,406), Sabld (5,947), Mamers (6,342). Laval (27,107), Mayenno (10,098), Chateau - Gouticr (7,218), Erncc (.5,330). 388 FRANCE. THE BASIN OF THE l,01RE—{Confi,med). Departments. LOIRE - INFE • RIEURE. Arrondissements. Nantes, Ancenis, Chat EAUB RIANT, Paimbceuf, St. Nazaibe. Natural Regions, Plateau of Brittany, Valley of the Loire, Brifere, Guerande, Retz. Communes of over 5,000 Inhabitants. Nantes (122,247), St. Nazaire (18,300), Chantenay (9,953), Eeze (6,849), Blain (6,807), Guerande (6,804), Guemene- Penfao (6,167), Nort (5,765), Vertou (5,471), Chateaubriant (5,228), Vallet (5,200), An- cenis (5,177), Plesse (5,154). BRETAGNE (BRITTANY). MORBIHAN. FINISTERE. COTES-DU- NORD. ILLE-ET- VILAINE. Vannes, Lorient, Ploermel Pon- Quimper, Brest, Chateal'Lin, Mor- laix, Quimperle. St. Brieuc, Dinan, GUINGAMP, LaN- NION, LoUDEAC. Rennes, Focoeres, MoNTFORT, Redox, St. Malo, Vithe. Landes of Lanvaux, A'^annetais, Coast Region, Islands. Comoiiaille, Muntagne Noire, Valley of the Aulne, Landes of CarhaLx, Hills of Arree, Leon. Monts Menez, Leon, Tregorrois. Basin of the Vilaine, Marsh of Dol, Pays Malouin. Lorient (35,165), Vannea (17,946), Ploermeur (10,600), Ponti\'y (8,252), Languidio (6,433), Hennebont (6,050), Sarzeau (5,718), Caudan (6,707), Ploermel (5,505). Brest (66,828), Morlaix(15,183), Quimper (13,879), Lambe- zellac (12,379), Doiiarnenez (8,637), Landerneau (8,195), Crozon (7,763), St. Pol de Leon (7,005), Quipavas (6,802), Quimperle (6,633), Plougastel-Daoulas (6,506), St. Pierre-Quilbignon (6,301), Briec (5,906), Plougeumeau (5,951),' Pleyben (5,229). St. Brieuc (16,355), Dinan (8,180), Guingamp (7,895), Lannion (6,294), Loud^au (5,901), Plevin (5,664), Plouha (5,229). Rennes (57,177), St. Servan (12,281), Fougeres (11,873), St. Malo (10,295), Vitrj- (9,870), Le Grand Fougerae (6,370), Cancale (6,239), Re- don (6,446), Combourg(5,6o8), Pleurtuit (5,238). LOWER NORMANDY AND COTENTIN. MANCHE. ORNE. CALVADOS. St. Lo, Avranches, Cherbourg, Cou- tances, mortadj, Valognes. AiENfON, Aroentan, DOMFRONT, MOE- TAGNE. Caen, Bateux, Fa- LAISE, LiSIECX, Pont - L'EvtauE, ViRE. Avranchin, Cotentin, Hague, Marais (Marsh). Percbe, Merlerault, Alen(;on- naia, Marches. Bocage, Campagne of Caen, Auge, Lieuvin, Ouche. Cherbourg (37,186), Granville (12,627), St. L6 (9,706), Avranches (8,157), Coutances (8,008), Valognes (5,831), Tourlaville (5,757). AIen(;on (16,615), Flers (11,155), La Ferte-Mace (9,769), Ar- gentan (5,788), Laigle (5,196). Caen (41,181), Lisieux (18,396), Honfleur (9,426), Bayeux (8,614), Falaise (8,428), Conde-sur-Noireau (7,350), Vire (6,718), Trouville(5,886). BASIN OF THE SEINE. YONNE. AUBE. AUXERRE, AVALLON, JoioNT, Sens, tonnerre. Trotes, Nogent- sur-Seine, Arcis- SUR-AUBE, BaR- SUR-AUBE, BaR- sur-Seine. Avallonnais, Auxerrois, Pui- saye, Gatinais, Senonais. Champagne. Auxerre (16,239), Sena (12,309), Joigny (6,317), Avallon (5,930), Tonnerre (5,536), VLUeneuve-sur-Yonne(6,084). Troyes (41,376), Romilly-sur- Seine (6,190). DEPAETMENTS, NATURAL REGIONS. AND PRINCIPAL COMMUNES. 889 BASIN OF THE SEINE-<0)«s»,,J^^_ :..-g .'~":r;-4lii_„.i j | i i J % ^...0..;-?— its _^ -J--"-T-!- - :-|-il-^ &hanJ HoTizontal Scale I : 1&5,0CI0. Teitical Scale 1 : l,lS5,00a hide the villages scattered over the lower spurs and foot-hills. Lower still, the terraces extending up the hillsides are planted with vines and mulberry-trees. All is verdure there, except a few steep rocks mirrored in the waters of the Ceresio. We have left far behind us the mountains of the north, and are, in truth, in Italy. But whilst the political boundaries of Switzerland extend in this manner fur into Lombardy, the Italian valley of the Toce takes us close to the St. Gotthard. There, within a space hardly 8 miles across, the Toce, the Ticino, and the Rhone take their rise and flow towards different points of the horizon. This narrow mountain isthmus, continued in the Monte Leone and the other summits of the Simplon, connects the St. Gotthard with the stupendous mountain masses of the Monte Rosa and Mont Blanc. The ridges which connect these moim- tain groups have evidently undergone a vast amount of degradation in a former epoch of the history of our earth. Originally the main crest extended from the St. Gotthard towards the south-west ; and an ideal line drawn in that direction SWITZEELAXD. AVD THE Scale 1 : 230,000. actually passes througt several very elevated mountains, including those of the Mischabel-Horner, the highest summits situated wholly upon Swiss soil. But this ancient mountain crest, being formed of mica slate, limestone, and felspathic rocks, not capable of offering a continued resistance to the action of water, was speedily destroyed by the mountain torrents. The water-shed recoiled more and more to the south, as far as the solid crystalline rocks of the Slonte Rosa ; and the imposing masses of the Mischabel, which formerly rose upon the main crest, look down now upon lateral valleys. Thus has the persistent action of water, con- tinued for ages, succeeded in displacing the crest of an entire mountain system. Destructive agencies are still at work Pig. 282. — The Sources op the Ehose, the Ticixo, i ^-l i • • ^ j _, ' ' amongst these mountain giants, and a traveller passing along the valley of the Rhone can scarcely fail to observe the heaps of debris resulting from them. Now and then the river is hemmed in by accumulations of this kind, having the appearance of veritable mountains. On ascending them we find ourselves face to face with gigantic amphitheatres of erosion, carved out of the mountain sides, and growing in size from year to year, owing to the continued action of snow and rain combined with frost. One of the most remarkable of these amphi- theatres is that known as the Illgraben. It measures nearly 2 miles across, and few volcanic craters can bear compari- son with it. A similar amphitheatre occupies the southern face of the beau- tiful mountain of Pierre-a-Voie, thus named on account of an ancient pil- grim's path paved with flagstones which leads right up to its summit. If we would form a just idea of the extent to which the mountains in that part of Switzerland have been demolished, we cannot do better than contemplate the jagged " Dents " du Midi and of Morales, which face each other on opposite banks of the Rhone. The magnificent portal opening between these mountains, rising to a height of more than 10,000 feet, has been carved out of the solid rock by atmospheric agencies alone. The mountain rampart which formerly connected these two peaks, joining the Bernese Oberland to the main chain of the Alps, has been swept away. The Dent du Midi is crumbling to pieces before our eyes. Frequently after heavy rains or sudden thaws, or in consequence of earthquakes, cataracts of OENKRAL ASPECTS.— THE ALPS. 897 rocks descend its Huuks into the valleys, and sometimes these obstruct the course of the Rhone, and would lead to disastrous inundations if labourers were not at once hurried to the spot to clear away the obstruction, and to open a way to tho pent-up waters. In 1855 showers of stones fell for weeks and mouths, and Fig. 283. — Ami'hitiibatub ui' tub Illoeadbn. Bmla 1 : 90,000. ■■': '^'^- ■ -a r '^ _ 1 MUt. artillerymen were placed upon a conspicuous promontory, who watched tho mountain and fired ofi" a gun whenever a rock detached itself from its summit, thus giving timely warning to travellers and the inhabitants of the valley. The valley of the Rhone, with its barren soil and tracts covered with pebbles VOL. II. I) u S98 SWITZERLAND. and swamps, would hardly lead us to expect that so much beauty shoidd be hidden in the valleys of the main chain of the Alps, which cliffs, hills of debris, and sudden turns in the road conceal from -view. We almost wonder how the inhabitants of the mountain villages are able to reach their homes, for many of their valleys are so completely shut in that the wind is hardly felt there, storms are almost unknown, and the quantity of rain is far less than in the wide valley of the Rhone. But having once surmounted the obstacles presented by the mouths of these Fig. 284. — The Matterhorn (Mont Cervin). Scale 1 : 150,000. 'IflfTWi I p*\ v^cvw.^- ■ 2 Miles. valleys, where the rivulets escape through narrow gorges, we find ourselves in quite another world. Amongst the lateral valleys ascending towards the main range of the Alps there are some to which groves of trees, small lakes, rivulets meandering amid a carpet of flowers and a covering of turf, impart a character of privacy. Others there are, of greater width, where the eye can range afar over barren mountain summits, fields of snow, and glaciers. One of the most charming of the latter, and, indeed, one of the most beautiful in the world, is the valley traversed LIBRARY OF THE yNIVERSlTY of ILLINOIS, GENEILUi ASPECTS.— TUE ALPS. 8. Milea. sustain the average volume of a river like the Seine for eighteen months. In comparison with this formidable glacier, those on the northern slope of the Ober- land are but of secondary importance. They do not present the same spectacle of sublime calm, but being more rugged, and descending farther down their steep valleys, they are more attractive to the beholder. They almost look as if they flowed down from the mountain summits. Seen from below, their white or bluish tints contrast with the green of the meadows and the forests. Sometimes they almost invade fields and orchards, and the inhabitants of Grindelwald have seen cherries ripen close to huge detached blocks of ice. The lower glacier of Grindel- iJNiV£fiSlTKof(LUNOlS. 1, I'll I,, , lll II I I " I' I , " I I I II. I'll Im'I,;ii,|'i ' I, 1 1' ii . " ' 1 1 ii'i'|ii ■ ' ,i,i . II 1 1 h I , I, ,l'l,h "''I' I ' Il ' 'l l|,,'i'.''l| I'll II II ' 'I ■' I II I|, .I'lll ," I ill I l| ''l| GENERAL ASPECTS.— THE AEPS. 401 wald, though recently its end has been melting awuy, and it appears to be retiring into the mountains, is still that amongst the glaciers of Switzerland which pene- trates farthest towards the lowlands. The glaciers of the Aar, at the eastern extremity of the Oberland, though comparatively small and sometimes almost concealed beneath mud and stones, possess an interest of their own. It was there the famous Agassiz, with some of his friends, established himself during several summers in succession in order to watch the phenomena of the glaciers. The rock which sheltered this band of conscien- tious explorers, facetiously called the " Hotel des \eucliatelois," exists no longer. It was incapable of resisting the persistent assaults made upon it by the glaciers. Its fragments were precipitated upon the glacier, and arc now descending upon its Fig. 286. — TuE Glacier of thb Blcmlisalt. WndaFrmn. Blamlisalpstock. back into the valley, to become in the end the prey of torrents which will triturate them into sand. The spot where these important researches into the nature of glaciers were instituted will always be hallowed to men of science. The formidable schistose summits of the Oberland, which for a long time were looked upon as inaccessible, now form the goal of the more ambitious amongst our Alpine climbers; but the limestone mountains to the west of them, and more especially the advanced buttresses of the Faulhorn, the Niessen, and the Stockhom, though less elevated, afford prospects of equal beauty. These were first visited by tourists in the sixteenth century, and do not, consequently, exercise the same attraction upon our modem tourists as the Jungfrau, the first ascent of which was accomplished in 1811. Standing upon one of these promontories, we are sus- pended, as it were, between the valley and the snowy giants which tower above 402 SWITZERLAND. it. At one glance we embrace the bold profile of the mountains, fields of snow, glaciers, pastures and forests, smiling valleys, and placid blue lakes, either reflecting the cliffs which bound them, or embedded in gardens and meadows. Equally beautiful are the landscapes which present themselves to the tourist in the valley of the Aar, whether near its head, where the torrent forms the fine waterfall of the Handeck ; lower down in the delightful valley of Hasli, with its gushing cascades, where the sculptured chalets of Meyringen nestle under the shelter of steep rocks ; or lower down still, in the plain of the Boedeli, upon which rises Interlaken, the leading town of pleasure of entire Europe. The mountains of the western Oberland consist almost entirely of oolitic lime- Fig. 287. — The Diablebets. Scale 1 : 100,000. y\.'!o/;ofia ■ / ■H" '4 ^^" ■^■?rB '"f1 Spxpou^c n\.r: te^x)-^' "iV^ Oldenhom - . , . •.■ .. f ' ,.ii ^■a;^^^ 7 \l(' L, OT or. IMUe. stone and chalk, capable of offering but sniill resistance to the combined chemical and mechanical action of water, and are fast crumbling to pieces, producing in their decay some of the most magnificent spectacles to be witnessed in the Alps. Two of the jagged grey "teeth" of the Diablerets, a group rising superbly above the green pasture-lands, detached themselves in the last century, and tumbled down into the valley of Deborence, 6,000 feet beneath, where their broken fragments now cover an area of several square miles. Similar catastrophes have evidently occurred farther north, but in so remote a time that no tradition respecting them survives amongst the inhabitants of the countrj'. The huge circular valley known as the GENERAL ASPEOTS.— THE XI.V&. 403 Creui-du-Champ may be likened to n gigantic punch-bowl, not unlike in its shape to the famous amphitheatre of Ga%arnie, in the Pyrenees. Like the latter, it forms a natural fortress of great strength, being surrounded on all sides by cliffs rising in terraces, and surmounted by extensive glaciers, from which descend numerous cascades. In the north and west the Bernese Alps ramify into numerous spurs and sub- sidiary chains, which gradually sink down into the plain. This is one of the great pasturing regions of Switzerland, the grass and herbage on these calcareous hills being most savoury. It is, too, a region of flowers. In spring the slopes of the mountains of Montreux are covered with narcissi, which are visible from a distance of 15 miles. An inexperienced traveller, on first seeing these carpets of flowers from afar, might be inclined to mistake them for particles of snow forgotten b)' the sun. Their odour, wafted by the wind to a considerable distance, is no less penetrating than that of the orange groves on the coast of Sicily.* Once more returning to tlie St. Gottbard as to the natural centre of the Swiss Alps, we perceive a distinct mass of mountains to the north-east of those of the Oberland, and on the same axis. This group gives birth to the glacier of the Rhone. Its principal summit is the Dammastock, rising in the midst of glaciers, and a range extends from it in a northerly direction. In these ranges rise some of the most glorious summits of Switzerland, such as the Titlis, with its vast pasture- grounds, and the Uri-Rothstock, bounded on all sides by steep precipices. These mountains of Unterwalden and Uri are formed of granite, oolitic limestone, chalk, and strata of eocene age. They ramify in the most extraordinary manner the labyrinthine Lake of the Four Cantons (see Fig. 324), being their exact counterpart. The summits, which rise to the north of the lake, appear to have formed part of the same mountain system at some former period. The principal summit is the Rigi, the most famous and most frequented Belvedere in the world. This mountain, rising in solitary grandeur from the lakes and plains lying at its foot, and afibrding a magnificent prospect of the snowy summits towards the east and south, forms, in truth, an admirable natural observatory, and tens of thousands of travellers are attracted to it annually. Railways not only convey these visitors to its summit, but also to many favourite points of view. In summer the top of this mountain exhibits more animation than many a town, and the telegraph wires which connect the numerous hotels with the dwellers in the plain are incessantly at work.t The Rigi is the first mountain in Europe which the engineers have rendered accessible by means of a railway, but it is no longer the only one. Sooner or later, all those mountains in Switzerland which annually attract crowds of tourists will be treated similarly, and Mount Pilatus, the ancient Fract-Mont, • Altitudes in the Bernese Oborland (in feet):— Main range: Finstcraarhom, 14,028; Junpfrau, 13,671; Monch, 13,439; Schreckhoni, 13,386; Diablercta, 10,667. Outliere : Faulhorn, 8,800; Niesen, 7,760; Stoclchorn, 7,196. t In 1876 there were thirteen telegraph offices on the top of the Rigi. The seaion of 1878 is supposed to have proved disastrous to several of the proprietors of hotels, the number of travellers having been very SDUill, owing to the commercial crisis in Germany. 404 SWITZERLAND. whose craggy points are visible to the south of Luzern, is sure to have its railway at an early date.* The Eigi covers an area of about 15 square miles, and is formed almost solely of nagelfluh ; that is, a soft conglomerate enclosing an immense number of pebbles, derived, not from the Alps, but from the Black Forest, and carried thither and deposited in regular layers during the miocene period. The Rossberg, to the north of the Rigi, belongs to the same formations. It has become widely known through a landslip which occurred in 1806, when 52,000,000 cubic yards of rock slid down the mountain side, burying the village of Goldau, with its smiling fields, and filling up a portion of the Lake of Lowerz.t The mountain mass of the Todi, to the east of the valley of the Reuss, forms with the mountains of the Rhone that region of Switzerland which exhibits the most extensive traces of geological disturbance. The contortion and inversion of the strata are more considerable there than in any other part of the world hitherto examined by geologists. From the Gliirnisch to the Hausstock, a distance of 10 miles, the beds have been uplifted and bent back in such a way that the lower beds rest apparently upon those which were originally deposited upon them, and the lower appears to be the higher part of the series. Similar features may be observed also in the valley of the Rhine beyond the Glarnisch. A most remark- able instance is afforded by the Windgiille, a mountain rising above the valley of Altorf. Upon its summit it bears a cap of porphyry, which has not been erupted, as Studer supposed, but has been uplifted by lateral pressure, together with the limestone beds upon which it reposes. The mountains to the north of the Todi are formed, like those of Unterwalden, of Jurassic and cretaceous rocks. Tertiary slates, locally known as fi/'ich, are also met with ; and these must have been deposited in a sea of considerable depth, for they abound in fossils of fish, but are altogether devoid of fossil molluscs and sea-urchins. The mountains belonging to this formation have gentle slopes, and their valleys are of exceeding fertility. The limestones, on the other hand, frequently form vertical cliffs. The Glarnisch, which rises in terraces above the town of Glarus, stiU belongs to the Alps, for glaciers descend from its upper slopes. They are the northernmost of Central Switzerland. Others, still farther to the north, are met with in the rano-e which extends from the Todi towards the north-east, and terminate above Chur, in Mount Calanda, famous on account of its crumpling rocks. That moun- tain is formed of fissured dolomite, resting upon beds of soft rock, incapable of resisting the action of denudation. The waste washed down from the mountain has formed huge sloping mounds at the foot of the cliffs, which constitute a characteristic feature of the landscape. Landslips are of frequent occurrence. One of these partially destroyed the village of Felsberg, at the foot of the Calanda. The inhabitants built themselves another village at a spot not menaced * According to Gatschet the name of Pilatus is derived from the old German word hilhta ; that ia, " split mountain." Popular legends connect it with Pontius Pilate, whose spirit is said to haunt a small lake near the summit. t Altitudes in feet :— Dammastock, 11,937 ; Ehoncstock, 11,822 ; Galenstock, 11,805 ; Titlis, 10,628 ; Uri-Bothstock, 9,610 ; PUatus, 6,792 ; Eigi, 6,906 ; Rosaberg, 5,190. OEXEKAI. ASPECTS.— THE ALPS. 405 l)\- falling rocks, but finding tlio situation too much exposed, they have returned to their old village, preferring to run the risk of a possible disaster rather than submit to an ever-present inconvenience.* The Calanda has been the goal of mountain climbers for centuries post. The mountains of St. Gull and Appenzell, which occupy the north-eastern corner of Switzerland, enclosed botwecu the Khine and the Lake of Constance, have proved equally attractive to admirers of nature on account of the fine prospects which may be enjoyed from their summits. One of them, the Speer ((),418 feet), is formed of the same conglomerate as the Ivigi. Another, the famous Scntis (S,213 feet), is justly admired for its fine buttresses, sweet pastures, piled-up rock masses, and small lakes hidden away in its upper valleys. Farther to the south, the jagged crest of the Churfirsten (7,554 feet), as seen from the shore of the Fig. 288.— The Intsrted Strata op thb WindoIllb. Acooidiog to A. Hein. H'alitt lladtraa •"» tOTo" I t MMT Jam LtM^ Jura I>olomU(Tt\aty mufniM "Wallen Lake, presents a truly formidable appearance. So precipitously do the rocks rise from the lake that a site for only a single village could be found at their foot. The chaotic mountains of the Grisona, cut up as they are by innumerable gorges, and valleys, almost defy classification. Their geological structure is most complicated ; their crests more sinuous than elsewhere in Switzerland ; and the two hundred valleys and their ramifications form a veritable labyrinth. Yet these mountains, too, are joined to the central group of the St. Gotlhard, and that by one of the boldest and most formidable mountain masses of Switzerland, the granitic pinnacles of which form the culminating points between the valleys of Altitudes in Engliih feet :— Todi, 11,887 ; Hausatock, 10,355 ; Olamitch, 9,654 ; Calanda, 9,210. 406 SWITZEELAND. the Eeuss and of the Inn. This group of the Adula, which alone of all the mountains of the Central Alps retains its ancient name, is partly buried beneath glaciers which feed the Further Rhine (Hinter Rhein). Other mountains of great height, likewise bearing glaciers upon their shoulders, continue the principal crest which bounds the upper valleys of the Rhine in the south. Beyond we enter a natural region of the Alps which lies within the basin of the Danube. The deep depression through which the Inn flows towards the north-east, and which is separated from the head- waters of the Adda by no marked natural feature, forms one of the most curious breaks in the system of the Alps. Bounded on either side by irregularly grouped mountains, some of Fig. 289. — The Group op the Beknina. Scale 1 : 300,000. E o< Cr 0. ferron 6 Miles. them naked rocks, others covered with perennial snow and ice, this depression, for a distance of over 10 miles, is almost horizontal. The waters collect there in lakes, and it needed but the removal of a few yards of ground to divert the head- waters of the Inn into the Italian valley of Bregaglia. This " gap " of the upper Engadin is remarkable, too, on account of its direction. Unlike most other passes, which cross the main crest at right angles, it has the same direction as the axis of the Swiss Alps, and coincides with the limits between difierent geological formations. One of the grand mountain masses of Europe, that of the Bernina, rises in the Engadin immediately to the east of the head-waters of the Inn. This group of GENERAL ASPECTS.— THE ALPS. 407 mountains, with its boldly contoured granitic rocks, and its glaciers creeping low down into tbo valleys, may fairly challenge comparison with the mountains of the Oberland ; and neither forests nor verdant pastures, sparkling cascades nor placid lakes are wanting to produce a picture of great beauty. The prospect from the culminating points of the Bernina are all the more highly spoken of as only expert climbers are able to enjoy them. Standing upon the Roseg or the Morte- Fig. 290.— ThB CiLACIEKS or TSCHIERTA AXB MoKTBHATSfH. Accordinfr to 7.i.u!ir. SoOo 1 : 100,000. ^.*wr --'*'--s MLiLA#^^3 I at C- 1 ililf. ratsch, the eye embraces at a glance fields of enow and ice extending for 20 miles from east to west, and we are able to trace the crystal streams to which the glaciers give birth. But the view afforded by the isolated summits which face the glaciers to the north of the deep valley of Pontresina is far superior. Stationed on the simimit of the Piz Languard (" Long Regard "), we see spread out before us not only the entire group of the Bernina, the mountains of the Grisons, of the Tyrol, and of Northern Switzerland, but far beyond the St. Gotthard we 408 SWITZERLAND. perceive Monte Rosa and the hazy outline of the French Alps, A panorama of almost equal extent may be enjoyed from the Piz Linard, which rises to the north on the other side of the Inn, and on the confines of the Austrian Vorarlberg. This mountain belongs to the group of the Selvretta, which is geologically interesting on account of the great variety of its rocks, which embrace nearly aU formations, from gneiss and crystalline slates to sedimentary deposits of eocene age. We even meet there with springs of carbonic acid gas — near Tarasp, in the valley of the Inn — the only springs of that kind hitherto discovered in such a locality, for they do not rise from a bed of lava, but from decomposed schists, and commu- nicate probably with the acidulous springs which rise lower down in the valley. The bodies of numerous small animals are found near the poisonous springs. Earthquakes frequently occur in the Engadin, but not as often as in the other two earthquake districts of Switzerland, viz. in the valley of the Visp, at the foot of Monte Rosa, and in the environs of Eglisau, betweep. SchafEhausen and the mouth of the Aar.* The Central Alps attain their greatest height and most considerable width in the Grisons and in the neighbouring Tyrol. They neither form a mountain- chain there nor a number of detached masses lying in the same axis, but form a veritable plateau, from which rise separate groups and numerous ranges ramifying in the most puzzling manner. All that portion of Switzerland which lies to the east of the Rhine rises from a platform no less than 3,200 feet in height, even in the valleys, and the mountain ranges extend thence into Germany and Italy. The contrast between Eastern and "Western Switzerland is indeed most striking, for the latter does not lie within the region of the Alps at all, and is bounded, not by an entangled mass of mountains like that of the Grisons, but by a succession of parallel ridges separated from each other by longitudinal valleys. * Heights of the mountains in the Grisons: — Piz Valrin (Adula group), 11,139 feet; Bemina, 13,294 feet; Eoseg, 12,557 feet; Morteratsch, 12,31"feet; Laqguard, 10,717 feet ; Piz Linard, 11,210 feet. CHAPTER II. THE JURA.« TIE parallel ranges of the Jura form but a secondary mountain system in comparison with the suow-clad Alps. Nevertheless they arc an importmt feature in the general geography of Europe, aud by their influence upon the climate, the flow of rivers, and the distribution of the population, they have played a prominent part in history. In Switzerland the contrast between these two mountain systems, the Alps and the Jura, is most striking. Standing upon the plain which separates them, we look, on the one hand, upon the serrated chain of the Bernese Oberland, upon verdant slopes extending up to the snow-fields and glaciers, and, in spite of the great distance, are able to distinguish the varied hues presented by barren rocks, snow, meadows, and forests. The foot-hills present the greatest variety in their slope and height ; and wide cultivated valleys, penetrating far into the mountain recesses, and dotted over with towns and villages, still further enliven the picture. Turning round towards the Jura, we find ourselves face to face with a steep and uniform slope. Towns and villages form a thin white streak along its foot ; fields and vineyards occupy the lower slopes ; and sombre pine woods cover all above up to the bluish pasture-grounds in the far-off distance. A few rocky crets here and there rise above the long-stretched backs of the mountains, but they do not break the monotonous appearance of the chain. Some of these ranges, seen from a distance, appear to be of uniform height for miles ; but if we penetrate through one of the gorges scooped out by torrents, and scarcely visible from the plain, wo are surprised to find ourselves in delightful valleys. It is only towards Switzerland that the Jura presents itself as an apparently unbroken rampart. On the French side the mountains are not only lower, but they are idso far more irregular in their outline. True the culminating points of the chain rise to the south, entirely within the French territory, but the Swiss summits are little inferior to them in height, and the general elevation of the * Jacard, '* Deflcription da Junk Kouchatvlou et Vaudois;" A. Veziao, "Etudce Oeologiqucs but lo Jura." 410 SWITZEELAND. mountains is more considerable. Between Besancon and Neuchatel the parallel ridges of the Jura increase in height as we proceed from west to east, and the highest amongst them forms a rampart bounding the plain of Switzerland. But to the north of Solothurn the ridges gradually grow lower, until their height hardly exceeds 2,000 feet. To the east of the Aar the Jura is represented by the small ridge of the Lagern, whilst beyond the Rhine, near Schaifhausen, it rises once more in the Randen group, and then gradually merges into the plateau of the Rauhe Alp.* The Swiss Jura presents all those features which we have already noticed in connection with the French Jura — elongated valleys separated by parallel ridges, " combs," and gorges connecting one valley with the other. These features in Fig. 291.— The Vailey of Traveks. Scale 1 : 170,000. , - \ tAAo-»w3 . 2 Miles combination produce picturesque scenery of astonishing variety. All the depres- sions are old lake basins, which were still covered with water during miocene ages. The valley of Travers, now drained by the Reuse, or Areuse, a tributary of the Lake of Neuchatel, is an instance in point. It receives the torrents descend- ing the terraced slopes of the " comb," or amphitheatre, of St. Sulpice at its upper end, and appears to terminate at the foot of a cliff which shuts it in on the east. But the slow erosive action of the water has overcome this obstacle. The river is now able to escape through a narrow gorge, its waters rushing headlong far beneath the railway suspended upon the flank of the mountains. All at once we perceive on our right a vast crater-shaped amphitheatre, known as the Creux-du- * Altitudes of the Jura (in English feet) :— Mont Teudie, 5,512 ; Mont Dole, 5,606 ; Chasseron, 5,286 ; Chasaeral, 6,280; Weissenstein, 4,580; Liigem, 2,827. TUE JURA. 411 Tent, or " Windy Pit." A geological exuiuiiiution of the ground shows tlmt this is a fullen-in cavity, or comb, such as are l'rev. i Miles. men, for in winter, when the remainder of the lake is covered with ice, the water immediately above them continues open. Fish and wild fowl abound there, and hence they are known as entner, or duck pools. If the level of the lakes were to fall, these springs would give rise to rivulets. vol,, n. K E CHAPTER III. GLACIAL PERIOD* HE Jura, which affords so many opportunities for studying geo- logical and hydrographical problems, furnishes likewise the most decisive proof of the vast extension of the glaciers in a former age. When exploring these mountains scientific men obtained the first glimpse of an age in which a great portion of Europe was covered with a cap of ice. The Jura itself had its valley glaciers, which carried down blocks of rock to a lower level ; but in addition to these rocks, which are clearly derived from the Jura itself, we meet with others on its eastern slope which are as certainly of a different origin. Formerly geologists were perplexed when asked to account for the presence of these prodigious masses of rock. Were they ruins of mountains no longer in existence ? or had they been carried thither from the Alps, in spite of their being at a distance of 120 miles ? We now know that the latter hypothesis was the correct one. These enormous erratic blocks have really been carried down the Alps, and we are even able, in manj' instances, to point out the locality whence they have been derived and the route which they followed. This mass of granite, we are able to say, came hither from the Monte Rosa ; that block of mica schist tumbled down the sides of the St. Gotthard. Formerly the whole of the northern slope of the Alps was bounded bj^ a vast sheet of ice, formed by the confluence of five glaciers, which filled up the valleys now drained by the Rhone, the Aar, the Reuss, the Linth, and the Rhine. The blocks of rock which tumbled down from the mountain-tops slowly travelled with these glaciers down the valley. They were carried over the plains and the cavities now converted into lakes, and would have been carried bej'ond the frontiers of Switzerland had not the trans- versal chain of the Jura interposed a barrier. It was upon its slopes they dropped when the glaciers melted away, and there we find them still, after hitndreds and perhaps thousands of centuries. Some of the blocks carried by the Rhone glaciers * Oswald Heer, " Le Monde rrimitif de la Suisse ; " Arnold Guyot, in Bull, de la Societe dcs Sciences Naturelles de Neuchutel ; VioUet-le-Duc, " Le Massif du Mont Blanc ; " J. Tyndall, " The Glaciers of the Alps ; " Studer, " Ueber Schnee und Eis." GLACIAL PEKTOD. 415 have been deposited upon the flanks of Mont Chasseron, at a height of 4,G00 feet above the sea. It was there, right opposite to Martigny and Villeneuve, at the entrance to the Rhone valley, that the central stream of the Rnone glacier struck the Jura ; and on either side of the Chasseron, whether we proceed north or south, the height at which erratic blocks are met with graduallj' decreases. Some of these blocks have a volume of 176,000 cubic feet, and are quarried as building stones. Erratic blocks of this kind are not only met with on the slope of the Jura, upon which the ancient glaciers impinged, but also along the slopes of all the Alpine valleys down which they formerly crept. Blocks of enormous size may be seen in the valleys of the Limmat, the Reuss, and the Aar. The Luegiboden, near Interlaken, is nothing but a huge erratic block of granite, having still a volume of 460,000 cubic feet, although much of it has been carried away by quarrymen, including a block forwarded to America to serve as the pedestal of a monument to "VTashington. The erratic rock, known as bloc monstre, on the hill of ilontel, near Bex, above the valley of the Rhone, has a volume of no less than 530,000 cubic feet. Many of these glacier-borne rocks have been deposited on the banks of the Lake of Geneva, and close to that town there is one of huge size known as the Pierre a Niton. The Romans probably consecrated that rock to Xeptune, and in our own days it has been converted into a gauge for registering the oscillations of the lake. But what is the volume of these huge blocks in com- parison with that of the pebbles, the sand, and the mud carried down the hills by these ancient glaciers, and further distributed by the floods when they melted away ? Most of the rocks and the soil removed whilst the existing valleys were being scooped out by the glaciers have been deposited upon the wide plains below them. Sometimes the glaciers melted so rapidly as to carry away the soil in streams ot mud, similar in all respects to those which descend from some of the volcanoes of the Andes whenever a subterranean lake bursts it« bonds. Pieces of ice were in every instance carried along with the mud, and the cavities which they filled have been discovered in the hardened conglomerate into which age has changed the mud. These rivers of mud sometimes filled up whole vallcvs to the brim. Below Sembrancher, in the valley of the Dransc, the mud rose to a height of 1,400 feet, as proved by the traces of it still existing upon the sides of the valley. But this enormous liquid mass at length burst the rocky barrier, stretching across the valley from the superb pyramid of Catogne to the mountain of Vence, and, when liberated, it inundated tlic lower portion of the valley. The ancient moraines of valley glaciers, though in reality far less important witnesses to glacial action than the horizontal strata to which they gave birth, nevertheless more frequently attract attention on account of their uneven surface and the prominent part they play in the scenery of the country. The valley of the Limmat is traversed by no less than six ancient terminal moraines, one of which crosses the Lake of Zurich opposite Rappcrswyl, and has been made use of in the construction of a bridge 5,250 feet in length. Zurich itself is built upon an ancient moraine, and so are several other towns at the lower end of lakes, and E E 2 416 SWITZEELAND. even some in the plain, including a portion of Bern, the capital of Switzerland. The interesting district to the north-west of Luzern, which a flood would convert into parallel islands, and where are the Lakes of Sempach, Boldegg, and Hallwyl, and the swampy grounds crossed by the Eeuss, exhibit many traces of an inva- Fig. 295. — The Catogse. Scale 1 : 80,000. '4.° WE.o)P.-i.-is ^fo::: Cifi.VE. of Gr IMile. sion of glacial mud. The scenery and aspect of a considerable portion of the rugged plain which separates the Alps from the Jura are due to ancient moraines. There these accumulations of stones no longer present the chaotic appearance of former days. Their surface now is covered with soil, and they nearly all are clothed with woods, forming a most charming contrast with the lakes which sepa- GLACIAL PERIOD. 417 rate them, with the rivulets windinp: nlong their foot, and with the cultivated fields surrounding the villages. The charniing .scenery at the lower ends of the Lakes of Thun, Ziirieb, and liienno (Bid) is the outcome of the diversities of contour resulting from the passage of ancient glaciers. The flora of this region of moraines proves that a remarkable change took place in the climate when the ice invaded the country. The ocean still covered the plain between the Alps and the Jura during the miocene age. The sandstones and pebbly conglomerates deposited at that time are rich in species of plants and Fig. 296. — The .Vnciknt Oi.AriEiis of Kasteiin Rwittfrlavp. r I E. of l'w» ^}^ it nit r If •••i/niiaty animals, whose presence proves to us that the mean temperature must then have varied between 04" and 08^ Fahr. To this climate of Louisiana or Florida suc- ceeded one analogous to that of Greenland. The Alpine plants, which are the same as those of Lapland, descended from the mountain summits into the valleys, and from the latter into the plain, and they are found now throughout Switzerland as far as erratic blocks are met with, their limit coinciding in a most remarkable manner with a flora of arctic aspect. M. Martins, who has more especially studied the vegetation of the Arctic regions and of the Alps, tells us that the aspect of the valley of Fonts, in the Jura of Neuchitel, and at an elevation of 3,300 feet 418 SWITZERLAND. above the sea, recalls certain portions of Lapland. But then the Alpine flora of that valley grows upon glacial mud carried hither from the Alps. These vestiges of the past — erratic blocks, glacial mud, and Alpine plants — have enabled geologists to draw a map indicating the ancient glaciers. The most important among them was that of the Rhone. It filled up the basin of the Lake of Geneva, covered the plain of Switzerland to a depth of more than 3,000 feet, and extended north as far as what is now known as the Aargau, where it was joined by the glacier of the Aar. But it did not penetrate the Alps of Fribourg, which had their own system of glaciers. The erratic blocks deposited within this wide area have mostly been traced to that portion of the Alpine chain which extends from the St. Bernard to the Simplon. The glaciers of the Reuss and of the Linth likewise extended to the barrier of the Jura, but only at its eastern extremity, whilst the glacier of the valley of the Rhine spread itself over a con- siderable portion of Southern Germany. Glaciers of vast extent likewise crept down the Italian slope of the Alps, filling up, wholly or in part, the existing lakes. The Lake of Lugano, like that of Ziirich, is divided into two portions by an ancient terminal moraine, which the retiring glacier left behind, and which is used now as a road. ^X^^^^fe^i CHAPTER IV. RIVERS AXD I^VKES.' T^!=rp7r][N comparison with the glaciers of a former age, the geological reconstruction of which has led the way to other discoveries con- nected with the history of oiir earth, the glaciers of the present day are of small account. They hardly cover more than 5 per cent, of the total area of the country, and their average thickness is certainly small compared with that of the ancient glaciers which made Switzerland another Greenland. Still, if there were to occur a sudden cessation of rain, and if these glaciers, which now hang like huge reservoirs above the rest of Europe, were to be melted to keep up the present volume of the rivers rising in Switzer- land, the supply would suffice only for five years, even though we estimated them to have an average thickness of 300 feet.t But it is well known that the difference in bulk which a glacier exhibits in summer and winter is relatively small, and that rivers and lakes are in the main dependent upon rain and melting snows for their supply of water, which they obtain either indirectly through springs, or directly through avalanches and surface drainage. The most important river of Switzerland, as respects the area of its catchment basin, is the Ticino, or Tessin, which is to a less extent fed by glaciers than any other river of the country. Though its principal vallej' is called Bedrette, which is synonj'mous with " glacier valley," the streams of ice which descend into it melt away before the mid-day sun. After heavy rains the volume of the Ticino, measured above where it enters the Lago Maggiore, lias reached 150,000 and even 200,000 cubic feet a second (the average throughout the year being only 3,700 cubic feet), and it is then a river t\vice as powerful as the Rhone at the forks of Arches. The Verzasca is likewise a largo river. After leaving • Riitimeyer, "Thai- u. Sctbildung ; " Studcr, " Gesclucht*; der rhysischon Gcographio der Sehwciz." t A Government Conunission (in 1871) computed the ana covered by glaciers at 8091 square miles, viz. 390-3 square miles in the basin of the Rhone, 289G square miles in the basin of the Ithinc, 70'6 square miles in the basin of the Inn, and 4S'G square miles in the basin of the Po. An official statement published in 1878 gives lower fifjures, viz. 710 square miles for the whole of Switzerland, 375 for th« canton of Wallis (V'ulais), 138 for the canton of the Urinous, 108 for that of Bern, 44 for Uri, &c. 420 SWITZEELAND. its wild gorge it spreads over a bed of gravel, which it pushes far into the lake, in front of the mouth of the Ticino. The Maggia, on the other side of the lake, is ordinarily a river like the Adour, but when in flood it may well bear comparison with the mighty Ehone.* The alluvium brought down by these three rivers is rapidly silting up the upper end of the lake. A comparison of ancient documents with our most recent maps would appear to show that this silting up, aided, no doubt, by the devastation of the forests which formerly clad the mountain slopes, is proceeding at an increasing rate. Seven hundred years ago the village of Gordola was the principal port on the upper part of the lake ; it is at present hardly a mile from its shore ; whilst the new port of Magadino has to be shifted every ten years, the shore of the lake flying it almost visibly. The port of Locarno, close to the delta formed by the Maggia, has to be perpetually dredged, at a Fig. 297. — The Upper Exd of the Laoo Maggiore. Scale 1 : 100,000. EofP /?S^-^^^L,„>^—ry . 1 Mile. considerable expense, for the sand is for ever invading it. If we assume that the matter held in suspension by the three rivers, the Ticino, the Verzasca, and the Maggia, and annually deposited in the lake, amounts to the one-thousandth part of their entire volume, the Bay of Locarno, in spite of its depth of 160 feet, will be silted up in the course of three hundred and fifty years, and the three rivers, then united into one, will be able to invade the lower portion of the lake. The alluvium deposited by these rivers remains injurious to health as long as it has not been turned over by the hoe or the plough. In summer the swampy plain of the Lower Ticino exhales deadly miasmata, and the inhabitants of several villages are at that time obliged to fly to the cabins they have in the mountain valleys. * Average rolume : — Ticino (Tessiii), 3,700 cutic feet ; Verzasca, 353 cubic feet ; Maggia, 2,200 cubic feet. RIVERS AND LAKES. 421 Far more sixlubrious are the shores of the Cerisio, or Luke of Lugano, a double bafiin, within which the two ancient ghiciers of the Ticino and the Adda formerly united into a single river. AVhen the glaciers retired the basin of the Cerisio was left with but a few inconsiderable affluents. The alluvium brought down by them from the mountains is only of trifling quantity, and the lake shrinks conse- quently very slowly. This lake, not being subjected to sudden flood.s, might easily Fig. 298. — The Lakeb of Luoako avd Como. f-ciUc 1 : 250,000. K.xl I'. fi Miles. E.»(Cr. . be transformed into a huge reservoir, whence the neighbouring fields of Lombardy might be irrigated. Signor Yilloresi, an Italian engineer, has proposed to connect it by means of a tunnel, only 2 miles in length, with the Lake of Como, and to convert the latter into a basin of distribution, whence the water would be conveyed to the sterile lands of the Somma. The water available for such a purpose has been estimated at between 560 and 1,120 cubic feet, according to the season. 422 SWITZEELAND. If the Ticino is fed only in a small measure by melting ice, such is not the case with respect to the Rhone, which has more extensive glaciers in its upper valley than any other river of Europe. The glaciers occupy nearly one-half the total area of those of all Switzerland, and the ice river of the Aletsch, as well as the ice streams creeping down the slopes of Monte Rosa, is without a rival. The Rhone glacier, properly so called, is not only of considerable extent, but it is also much admired for its natural beauties, more especially on account of its terminal face, furrowed by huge crevasses. Formerly it was bounded only by naked rocks and Fig. 299. — The Aletsch Glacier. Scale 1 : 100,000. if.-f- 8°|5'E.ofCr. lllils. turf, but M. Gosset has planted its banks with Scandinavian trees, and a forest may be seen in close proximity to the ice. From this frozen river issues a small torrent, which is usually regarded as the head of the Rhone. The mountaineers, how- ever, do not look upon the glacier as the veritable source of the Rhone ; they derive that river from a small tepid spring which rises at the foot of a neighbour- ing rock. In addition to the Rhone glacier there are two hundred and sixty others which regulate the flow of the river, for it is precisely in summer, when the rain- fall is least and the evaporation greatest, that the ice melts most rapidly. Some- ElVERS .VXD UiKES. 423 times, however, these glaciers fhemselvcs give rise to floods. Some of tho upper side valleys are closed in by iialurul dams, formed of moraines and fragments of ice. The water accumulated behind these barriers, when it bursts them, rushes down the valley, carrying fragments of stone, houses, and trees before it, and denuding the fields of their arable soil. In order to prevent the recurrence of such floods it has been found necessary to pierce these dams, so that the water may escape. The small Lake of Moeril, or Merjelen, on the eastern side of the Aletsch glacier, from which it is separated by a lateral moraine, has been treated in this manner, and it has since remained permanently at the same level. The Dransc, which joins the Rhone where it abruptly changes its direction before entering the gorge of St. Maurice, was blocked up by the glacier of Grctroz in 1818. Its upper valley was converted into a lake, and, when the pent-up waters at length liberated themselves, they produced one of the most disastrous floods known in connection with the Rhone valley. Immediately on issuing from the rock-bound gorge referred to, tho Rhone enters upon an alluvial plain, formerly covered by the Lake of Geneva. This plain has an area of 34 square miles; and the depth of the alluvium which covers it, and all of which has been deposited there by the Rhone, is unknown. A few ancient moraines rise above it. The village of Port-Valais, which formerly stood upon the banks of the lake, is now at a distance of over a mile away from it, the whole of the intervening land having been deposited in the course of three centuries. It is also asserted that the delta of the Rhone has so rapidly grown during a single generation that the inhabitants of Yilleneuve are no longer able to see Le Bouveret, which faces them on the southern shore, it being now hidden from view by a peninsula covered w^th poplars, willows, and houses. The heavier fragments brought down by the river form flats and sand-banks close to its mouth, whilst the triturated sand is carried a considerable distance into the lake. It has been ascertained, by soundings, that the bottom of the eastern extremity of the lake is slightly convex in front of the mouths of the river, a phenomenon satisfactorily explained by the deposition of alluvial matter. Though much smaller now than in former ages, the Lake of Geneva, or Leman, is the largest lake of Western Europe. It is also one of the deepest, its bottom extending down almost to the level of the sea.* To drain it bj' a river equal in volume to the Rh(5ne would require no less than ten years, supposing, of course, that its tributaries ceased to flow. Like the ocean, it has its storms, its waves, its surge ; but the most careful observations have not hitherto established the existence of tidal currents. The seiches are a phenomenon of quite a difiercnt kind, and are produced by sudden changes in the pressure of the atmosphere, which result in a swelling up of a portion of the lake, sometimes to the extent of 6 feet. These seiches occur at regular intervals, and the laws which govern them are now thoroughly imderstood.t * Lake of Oenera: — Average height above sea, 1,217 feet; average area, 223 square miles; greatest depth, 1,099 feet ; average depth, 492 feet ; approximate contcDt«, 86,193 million tons of water, t See Forcl in Bull. tf n^ i SI lies. GJJa^o del The dark shading expresses a depth of over 660 feet. navigable canal, will regulate the discharge of the lake. In making the excava- tions for this canal a Roman tunnel, 2,800 feet in length, was discovered near the village of Hageneck, at a depth of 300 feet below the level of the di%'iding ridge. The redoubtable Aar is " regulated " in its upper course by the twin Lakes of Brienz and Thun. Formerly these two lakes formed one sheet of water, but during the glacial period immense quantities of mud and stones, the waste of the mountain masses of the Oberland, were carried down the valley of the Lutschine, and deposited in the very centre of the elongated lake, which was thus separated into two basins.* Denudation and deposition still proceed, though at a very slow rate, and both lakes are gradually being silted up. The Upper Aar, which enters the upper end of the Lake of Brienz, collects the debris throughout its basin, which includes the glacier of Unteraar, and, rushing over the Handeck Falls, Height aljove the sea, in feet . Average area, in square miles . Depth, greatest, in feet. . Depth, mean, in feet Contents, in million tons of wulor e of BrieDz. Luke of Thun 1,853 1,837 110 185 856 702 6G0 600 G,000 7,940 428 SWITZEELAND. deposits it in. the lake. Lower down, the Lake of Brienz is joined by the Lutschine, which is fed by the vast glaciers of the Oberland, including that of Grindelwald. Formerly this furious mountain torrent frequently devastated the country around Interlaken ; but about the middle of the thirteenth century it was confined within an artificial channel, and diverted by a direct course into the lake. Amongst the rivers which join the Lake of Thun the Kander is the most important. It brings down immense quantities of pebbles and mud. As recently as the beginning of last century it joined the Aar, about a mile below the town of Thun, but the sudden Fig. 304. — The Gkindelwald Glacier. Scale 1 : 100,000. _ 2 Miles. inundations which it caused were ot so disastrous a nature that the patricians of Bern caused it to be diverted into the lake. The roof of the tunnel which they constructed for that purpose has since fallen in, but the river continues to flow in the desired direction. The alluvium deposited by it covered an area of 142 acres in 1870, and, as the depth of the lake there cannot have been less than 200 feet, its mass may be estimated at 42,000,000 cubic yards. The ancient lakes which formerly extended along the foot of the Jura, below the confluence of the Aar and the Thiele, exist no longer. The alluvium carried down by torrents, the growth of peat mosses, and the labour of man have converted BIVEBS ANP LAKES. 429 them into pasturc-lmids. All the small lakes of Northern Switzerland, ns those of Scmpach, Baldegg, Ilallwj-l, Grcillon, and Pfiitfikon, ns well as tlie three largo ones of Luzem, Zug, and Zurich, belong to the hydrographical domain of the Alps, or of their foot-hills. The junction between the river systems of the Alps and the Jura takes place at the triple confluence of the Aar, the Rouss, and the Liniraat. At a fonner geological epoch these three rivers flowed along the foot of the Jurassic ridge of the Liigern, towards the Lake of Constanz ; but in the end the united force of these rivers broke through the barrier of the Jura. Geo- graphically the passage which they opened for themselves forms the Gate of Switzerland to a traveller coming from the direction of Germany. The centre one of the rivers, the Heuss, is the effluent of the Lake of the Four Cantons, which of all the lakes of Switzerland most resembles a Norwegian fiord. Between Luzern and Brunncn, or between Kiissnacht and Stad, the lake appears to consist of a single sheet of water, but in reality it is formed of several separate basins, some joined to each other by narrow straits, others intersecting each other at right angles. At a former geological epoch, when the Lakes of Zug, Lowerz, Sarnon, and Lungern still formed part of the system of the Four Cantons, the labyrinth of these water-ways was even more intricate. Abrupt turnings, bold promontories, wide bays bordered by villages, glistening villas and sombre forests, cultivated fields and distant views of the Alps, are productive of the most picturesque efiects, and many there are in whose opinion this is the most beautiful lake in all Switzerland. Historical associations increase the interest with which we contemplate its beauties. Formerly the lake was popu- larly considered to be almost unfathomable, and fishermen seriously talked about abyssal depths of 5,000 feet. They believed that the steep precipices which bound it continued at the same gradient mitil they met beneath its waters. They do extend beneath the surface of the lake, but only as far as its flat bottom, which in the basin of Uri lies at a depth of Cl^ feet. The depth of the large basin is 853 feet, that of the Lake of Zug 644 feet.* The lakes drained by the Limmat have a geological history similar to that of the twin Lakes of Brienz and Thun. They, too, were cut in two by alluvial masses carried down by the glaciers. The Lake of "Wallenstadt, or Wallen, most resembles an abyss. Bounded by the steep walls of the Churfirstcn, this narrow and sombre lake resembles a gorge which has been invaded by a river. And such has actually been the case. The Rhine, which now flows to the east of the mountain masses of Appcnzell and enters the Lake of Constanz, formerly flowed through the narrow mountain defile which opens to the south of the Churfirstcn, and, taking the direction of the river Linth, the Lake of Ziirich, and the present bed of the Limmat, it joined the Aar. A strip of alluvial land, about 43 miles in length, and only IG feet high in the centre, now separates the Rhine from • Height above the sea, in feet . Average area, in square miles . Depth, greatest, in feet .... Depth, average, in feet ■ . Contents, in million tons of water VOL. 11. F K Lake of Luicm. Lake of Zug. 1,431 1,367 437 14-7 853 644 490? 390 P 16,950 4,560 430 SWITZEELAND. its ancient bed. A flood of unusual height might some day enable it to overcome this obstacle, as very nearly happened in 1817 ; and, if once it resumed its ancient course, it might not again return to its present bed. The people of Ziirich fear such an event, and for this reason they offer the most powerful opposition to the construction of a canal which is to join the Linth to the Rhine, and the railway engineers were prevented from carrying their line through a cutting. Below the Lake of Wallenstadt commences the valley of the Linth, formerly a swamp, converted into dry land by the detritus washed down from the Alps of Glarus. The torrent which performed the greater portion of this geological work was formerly much dreaded on account of its sudden floods, which laid waste the fields, and decimated the population by breeding miasmatic fevers. The famous rig. 305.— The Swamps op the Linth. Scale 1 : 220,000. . 2 Miles. Swiss geologist, Escher, surnamed of the Linth, diverted the course of this river into the Lake of Wallenstadt, and canalised the sluggish Mag, which formerly meandered amongst swamps. The Limmat (Linth- Mag), which drains the Lake of Zurich, is joined in the suburbs of that town by the Sihl, a river which frequently overflows its banks, but which might easily be diverted into the lake. The Aar, haviag been reinforced by the Eeuss and the Limmat, is a larger river than the Rhine * at the confluence of the two rivers, but its course being more sinuous, and its valley of less importance than that of the smaller river, the name of the latter has been bestowed upon the united streams. In its general * Average volume of the Rhine at the confluence with the Aar, 15,010 cubic feet a second ; of the Aar, 18,080 cubic feet. RIVERS AND LAKES. 431 features the Rhine bears a striking resemblance to the Rhone. Both rivers rise near the St. Gotthard, in a great transversal valley of the Central Alps ; both purify their waters in a large lake; and, in their passage through the same Jurassic range of mountains, fhey both form cataracts and waterfalls, though separated by that time by an interval of 180 miles. The elbow at Basel has its analogue in the elbow at Lyons. Both rivers then flow straight towards the sea, the one to the Mediterranean, the other to the German Ocean, and the volume of water they discharge is about tlie same. The principal head-stream of the Rhine is not the Vorder-Rhein, which rises in the neighbourhood of Andcrmatt, but the Hinter-Rhein, or Further Rhino, which has its source on the Adula. It is not " born amongst reeds," but rises from an icy cave, amidst a chaotic mass of rocks, rejoicing in the epithet of " Hell." Lower Fig. 306. — Thb Socrces op thb Rhine. Bade 1 : 926.000. 10 Miles. down it traverses many another "hell," the most famous amongst which is the fearful gorge of the Via Mala, bounded by precipitous rocks rising to a height of 1 ,500 feet. Immediately below that famous cleft in the mountains, within which the river is confined to a bed hardly 30 feet wide, the Rhine is joined by two mountain torrents. One of these is the Una, the waters of which are sometimes black as ink, owing to the triturated slate they hold in suspension ; the other is the Albula, or " white river," which is a more formidable stream than the Rliine itself. It issues from the gorge of Schyn, or Mai Pass, hardly less wild than that of the Via Mala, and exceedingly interesting on account of its geological formation. Formerly, before the Albula had opened itself a passage through this gorge, it flowed north, in the direction of Chur. The Rhine, now an imposing river, flows past the piled-up rock masses of the F F 2 432 SWITZERLAND. Calanda, and is joined by several valleys, amongst which that of the Tamina is best kno^vn on account of its overhanging rocks, at whose foot rise the thermal springs of Pfaffers. The Rhine then flows through a wide alluvial plain, and below Sargans, where its old bed branches off to the left, in the direction of the Lake of "Wallen- stadt (see p. 429), it enters the ancient lake basin, now to a great part filled up by its alluvium. This filled-up basin is more extensive than that of the Rhone above the Lake of Geneva, its area amounting to no less than 116 square miles, and it is continually encroaching upon the Lake of Constanz. A few isolated hills, not yet destroyed by errosive action, rise in the midst of this vast alluvial plain. The river, which here forms the boundary between Switzerland and Austria, frequently overflows Its banks, and the maintenance of embankments * and the drainage of the land require unremitting attention, in spite of which the Rhine has repeatedly broken through the barriers which confine it, and excavated itself a new bed. In many parts of the vaUey the average level of the river is from 6 feet to 10 feet higher than the adjoining plain. When building a bridge near Buchs, an old stone embankment was discovered at a depth of 16 feet below the actual level of the valley. The Lake of Constanz is the remnant of a vast sheet of water which formerly stretched from the Swabian Jura to the mountains of the Tyrol. It is a German lake rather than a Swiss one, and its German name, Bodensee, is derived from a small village at its north-western extremity. In its general features it resembles the Lake of Geneva, but it is smaller and more shallow. Its waters present the phenomenon of seiches, locally known as Ruhssen. Its elevation above the sea being greater than that of the Lake of Geneva, and its position more northerly and less sheltered against cold easterly winds, ice forms along its banks nearly every winter, and five times in the course of the last four centuries the lake was frozen over entirely. The Lake of Geneva formerly discharged its waters Into the Rhine, whilst the Lake of Constanz was tributary to the Danube. Subsequently, after the latter lake had become a member of the basin of the Rhine, its waters discharged themselves, towards the north-west, through the arm now known as the Lake of TJeberlingen. At the present time the lake overflows through a canal 2J miles in length iato the Untersee, or Lower Lake, which may almost be looked upon as a distinct lake, as it lies about 3 feet below the Bodensee. It is much shallower. For- merly its waters escaped through a vaUey now occupied by the rivers Aach and Biber, but they now Issue from the south-western corner of the lake at Stein. In its passage through the Jurassic hUls below that town the current of the river is strong. At Schaff hausen a forsaken bed of the river, now known as the Klettgau, branches off on the right. A short distance below that town, close to the old castle of Laufen, the Rhine plimges over a ledge of rock and forms a waterfall 66 feet in height. In the midst of the foaming waters rise two jagged rocks, the one pierced by a natural tunnel, through which the waters rush when the river is In * Lake of Constanz (or Bodensee) t-^Height above the sea, 1,306 feet ; area (average), 208 square nnles ; depth, greatest, 906 feet ; depth, average, 490 feet ; contents, in tons of water, 80,850 millions. RIVEKS AKD T.AKl'.S. 488 flood, and both covered with shrubs, whose leaves are over moistened by tho mist which perpetually hangs over tho fulls and is drifted about by the wind. Tho Falla of Laufeu, frequently called after tho neighbouring town of Schufi'hausen, are the most considerable of Europe, no less than 330 tons of water, on an average, roaring over them every second. They set in motion the wheels of numerous factories. Above its junction with the Aar the lUiiuo is joined by the Thur, an impetuous river, which frequently overflows its banks. Below the Aar the Rhino has still to surmount several obstacles before it reaches tho plain. It forms a few small rapids, known as the Kleine Laufen. They present no obstacle to vessels descending tho river, but the Great Rapids, or Grosse Laufen, near Laufenberg, interrupt navigation. The Rhine by this time has traversed the whole width of the Jura. It flows over a bed of granite con- nected with the Black Forest, and enters a natural region very diflerent from Switzerland. Soon after, at Basel, the river turns abruptly towards the north, and intersects the wide plain of Alsatia and Baden, bounded on the one side by the Vosges, on the other by the Black Forest. Two-thirds of the surface drainage of Switzerland pass beneath the arches of the bridge of Basel. The volume of the Rhine, not including the water conveyed into it by tributaries not fed from Swiss sources, is double that of all the other rivers of Switzerland (Rhone, Ticino, Maggia, and Inn) at the spots where they leave Swiss territory.* • Average volume of the rivers of Switzerland at the Swiss frontiers, as determined by a Federal Commission in 1871 (cubic feet per second) :—Khine, 28,854; Rhone, 9,535; Ticino (Tessin), J,708 ; Haggia, 2,190 ; Verzasca, 353 ; Inn, 1,765 ; minor rivers, 424 ; total, 46,829. The volume of the Rhine at Basel, including the water conveyed into it by its Grennan tributaries, is 35,300 cubic feet a second. CHAPTER V. CLIMATE, FAUNA, AND FLORA.* HE variety in the vertical configuration, of the country materially affects its climate, and nearly every valley and every mountain side has a climate of its own. Speaking in a general way, we may observe that the climate in the Jura and on the northern slope of the Alps is far more inclement than would be exiDected from the latitude, whilst the towns on the southern slopes, being protected against northerly winds, enjoy a milder climate than other places equally distant from the equator, but situated on an open plain. Thus, whilst the mean annual temperature at Locarno, on the bank of the Lago Maggiore, amounts to 55° Fahr., that of the Swiss plain, between the Lakes of Geneva and Constanz, does not exceed 49° Fahr. In fact, every place in Switzerland has its distinct climate, t On ascending a mountain the mean annual temperature decreases 1° Fahr. for every 349 feet we ascend. This is the average, the extremes being 300 and 419 feet, according to the locality. The mean annual temperature on the passes of the St. Gotthard and Simplon is not much below freezing point ; that on the St. Bernard is considerably less. The mean temperature of the Monte Rosa and of the highest peaks of the Oberland has been estimated at 6" Fahr., which is the climate of Greenland or the Arctic regions. The average height of the snow- line is 9,180 feet, but in exceptionally warm summers the * H. C. Lomtard, " Les Climats des Montagnes ; " Dufour, " Eecherches sur le Fohn du 23 Sept., 1866, en Suisse ; " Tschudi, " Des TTuerleten der Alpenwelt." Meteokological Table. Height. Mean Temperature (Degrees Pahr.) Precipitation Lat. N. Feet. January. July. Year. Inches. Basel, 47° 34' . . . . 804 31° 66° 48° 25 St. Gallen, 47° 26' 1,810 29° 65° 49° — Zurich, 47° 23' 1,420 29° 66° 48° 33 Bern, 46° 57' . 1,910 27° 63° 46° 46 Chur, 46° 50' . 2,000 29° 66° 49° — Neuchatel, 46° 49' 1,440 33° 64° 47° — Lausanne, 46° 31' 1,640 30° 64° 49° 40 Geneva, 46° 12' 1,330 31° 5' 64° 48° 32 St. Gotthard, 46° 3 V 7,090 18° 46° 30° — St. Bernard, 45° 50 8,170 15° 43° 28° 61 CLIMATE, FAUNA, AND FLORA. 486 snows completely melt away on summits having an altitude of over 11,000 feet ; and even the jagged rocks of the ilischabel, which rise to a height of 14,000 feet, may then occasionally bo seen without a patch of snow. The mountains of Switzerland intercept winds and clouds, and tho amount of precipitation is consequently more considerable than in tho neighbouring countries. Dense fogs frequently drift over tho swampy plains, the lakes, or shut-in valleys, but, as a rule, tho sky is rather loss clear half-way up tho moun- tains than either in tho lowlands or upon tho mountain summits. The clouds are generallv intercepted by tho mountains at an elevation of 5,000 feet, and then descend in rains. Higher up, precipitation, in the form of snow, is less abundant. The annual rainfall varies in the plain of Switzerland between 25 Fig. 307. — Rain Map op Switzerland. I«- !»• !«• ,r .riotr. =^ ^!§^t— 7/ M ^^ :: J jfcl ^ £^^^ - .-.1,-ii.i 1,1.1: t - .J 1 J*^^^~ — — -.^^^fcfc^fc^f^ ^ Cf il h ,1 /( tl I h tfc '*-w ^ ^ 80— to in. 60-80 in. and 4G inches. This is far more than falls in France, but very much less than falls on the upper mountain slopes. On the Pass of St. Bernard the annual amount of precipitation, including rain and snow, exceeds 5 feet. Agassiz saw more than 56 feet of snow fall upon the passes in a single winter. On the southern slope of the Alps, in the valley of tho Ticino, the rainfall resulting from the contact of warm winds witli the cold mountain slopes is more consider- able still, and sometimes exceeds 9 feet in the course of a single year. Proportionately to its area, Switzerland receives a greater quantity of rain than any other country in Europe ; and the quantity of water which flows down its rivers to the sea is very considerable. The combined volume of these rivers, which flow to the north, west, and south — into Germany, France, and Italy — is four times greater than that of the rivers of France, always bearing in mind 436 SWITZEELAND. the difference between the areas of the two countries. In addition to these rivers, which carry fertility to distant countries, Switzerland possesses in its lakes and glaciers vast reservoirs of water. North-easterly and south-westerly winds prevail, as in France and Germany, and the conflict between the polar and equatorial currents is going on perpetually and with varying success. Mountains and valleys, however, by intercepting or turning aside the atmospheric currents, produce the most extraordinary irreo-ularities. Sometimes a violent wind blows on a pass, whilst in the vaUey below the air is calm, or moving gently in an inverse direction. It is by no means rare for a northerly wind to penetrate some valley from the south, or for a westerly wind to do so from the east. Moreover, in all the valleys which are bounded by high mountains, the wind must either blow up or down. In the canton of Valais, for instance, the winds either blow from the west or from the east ; whilst in the valley of the Rhine, between Chur and the Lake of Constanz, only northerly and southerly winds are known, and the same is the case in the valley of the Ticino, between the St. Gotthard and the Lago Maggiore. The general law in accordance with which the winds blow down the hills durinc the night and in the morning, and up the hills during the heat of the day, has been observed to prevail throughout Switzerland, and more especially on the lakes, where fishermen are obKged to pay special attention to this phenomenon. Except when interfered with by general atmospheric currents, a breeze begins to blow every afternoon from the bottom of the lake towards the mountains, the air above which has become rarefied through the heat of the sun. After sunset the mountains cool suddenly, and during the night the wind blows down the lake. Local circumstances, such as temperature and configuration of the mountains, cause the hour of change to vary for each lake basin. Thus in the canton of Ticino, where the steep slopes are exposed to the full heat of the sun, the breva, or uphill breeze, begins to blow at eleven in the forenoon, whilst the contrary current sets in early in the evening. On the Lakes of Ziirich and Constanz, which occupy valleys open towards the west, and are surrounded by mountains of less height, and less exposed to the rays of the sun, the breezes set in several hours later. The fdhn, known to the Romans as/avonins, brings about the most sudden changes of temperature, and disturbs more than any other wind the general equilibrium of the atmosphere. This wind, so much dreaded and yet so bene- ficent, has been a subject of frequent discussion amongst meteorologists. Dove, Miihry, and others look upon the fcihn as a tropical counter- current of the trade winds. Others, including Escher of the Linth and Desor, believe that it originates in the Sahara, and flows in towards the area of low atmospheric pressure in "Western Europe. M. L. Dufour, who most carefully investigated the fohn of the 23rd of September, 1866, found that the meteorological conditions of Algeria coincided on that day in the most striking manner with those of Switzer- land, both countries having been visited by the same tempest. The fohn usually blows in winter or in early spring, and difiers much according to season or CLIMATE, FAUNA, AND FLORA. 487 locality. As a rule it is hot, dry, and enervating. During its passage over the high Alps it cools, and causes heavy rains to fall upon the Monte Rosa and other summits of Ticino ; but, as it plunges down again into the valleys, it regains its heat by condensation, and blows warm. It is the fiihn which melts most of the snow in spring, sometimes in the course of a few hours laying bare extensive mountain slopes. " Without the fiihn," stiy the peasants of the Orisons, " neither God nor the golden sun would prevail over the snow." But this wind, so beneficent on many occasions, is terrible in its fury. "Woo to the vessel that ventures upon a lake exposed to its full blast. It lashes the surface of the water into mighty waves, and converts the lake into a culdrou of seething water. As we rise from one climatic zone to the other, all that has life in it — plants, Fil?. SP*. — A C.*"1N "K T!IK Am'TNF ('ivI', with f VtVW "!■ TUF AlTFI* AM> CNv M TFMIOHV. animals, and human beings — diminishes. Nearly the whole of the population of Switzerland has settled down in the plains, in the hilly regions, and in the valleys which extend into the Alps. A contour-line drawn at a definite height along the mountain slopes would mark, in many parts, the upper limit of human habitations. There is only one town, viz. Chaux-de-Fonds, in the Jura of Neuchatel which has been built at an elevation of more than 3,200 feet, and that almost in despite of the climate. Many villages in the Alpine valleys have an elevation of between 4,000 and 5,000 feet, and in the dreary valley of Avers, which is tributary to the Vorder-Ilhein, where the year is made up of "nine months of winter and three of cold," wo meet with the hamlet of Juf, inhabited by descendants of German settlers. Juf, at an elevation of 6,700 feet above the sea-level, is the highest village in Europe permanently inhabited. 438 SWITZERLAND. The hospice of the Great St. Bernard, at a still higher elevation (8,108 feet), is open throughout the year for the reception of travellers crossing the pass. A few huts have been built even beyond the limits of perennial snow as places of shelter for mountain climbers. The most elevated amongst these is the one on the Matterhorn, which stands at a height of 12,790 feet. It is well known that the climate exercises a most potent influence upon the inhabitants of the upper valleys. The movmtaineers, as a rule, are stouter and heavier-limbed than the dwellers in the plain. Owing to the light air they breathe, they are less subject to maladies ; and consumption, which carries o£F so many victims in "Western Europe, is hardly known amongst them. Experience has clearly established this fact, and thousands of consumptive patients now pass the winter in the midst of snow and ice, in the villages of the valley of Davos and in the Grisons, which have an elevation of 5,080 feet.* On the other hand, the deaths from lung diseases and pleurisy increase with the altitude. These diseases are contagious amongst the mountaineers, and are much dreaded. In German Switzerland they are known as A/peiisfic/i, or " stroke of the Alps." Asthma, scrofula, and rheumatism are more frequent in the Alpine valleys than in the plains. In damp places deficient in sunshine, and more especially where the water runs over magnesian rocks, many of the inhabitants are afflicted with wens or suffer from cretinism. Cleanliness, however, and an improved diet, cause these diseases to diminish from year to year. Bodily and mental afflictions are more frequent in Switzerland than in the neighbouring countries, and only the number of blind is less.t But Switzerland possesses, in its diversified climate, varying with the elevation above the sea, the most powerful means of combating these maladies. By a change of residence we may obtain lighter air, more warmth, or less moisture. Jean Jacques Rousseau clearly perceived these advantages when he expressed his surprise that " bathing in the salubrious and beneficial mountain air had not yet become one of the great resources of medical science or of moral education." The wish of the great philosopher has been amply fulfilled, and thousands of our townsfolk now annually visit Switzerland in search of bodily, if not of moral strength ; and they crowd the great hotels on the mountains and in the valleys, on the Rigi, the Seelisberg, the Muverau, the Bellalp, and many others, where a prospect may be enjoyed of the Monte Rosa or of the snow-clad peaks of the Bernese Oberland. The watering- places of the country, such as Schinznach, Baden, Pfaffers, Leuk (Loueche), or St. Moritz, are quite as much indebted to the pure mountain air for their success as to the character of their water. As to the mountaineers themselves, they are always having " changes of air," though by no means for the sake of their health. • Deaths from consumption amongst a thousand inhabitants : — All Switzerland, 77 ; Basel (836 feet), 106 ; Geneva (1,230 feet), 101 ; Valais (1,640 feet), 49 ; Fribourg (2,060 feet), 37 ; Zug (1,670 feet), 17. In England the proportion is 1 24 per mille. t Insane, in the canton of Bern, according to Dr. Fetscherin (1871), 1,292, or 1 in 391 ; idiots, 1,512, or 1 in 335 ; idiots in Switzerland (census of 1870), 7,764, or 1 in 344 ; deaf and dumb, 6,544, or 1 in 408 ; blind, 2,032, or 1 in 1,313. In France the number of deaf and dumb is only one-fifth of the above, but the blind are slightly more numerous. CLIMATE. FAUNA, AND FLORA. 439 They ascend the mouutaius to mow the grass ; retiu-u to the lowlands to attend to their vineyards ; and grow their oats and potatoes at some intermediate point. In the Valais we meet with numerous parish communities alternately inhabiting three distinct villages, according to the season. It would not by any means be easy to trace the upper limits of various zones of vegetation, for local conditions, exposure to the sun, and human industry or interference bring about numerous exceptions. Even at Juf, far above the region of forests, the perseverance of the inhabitants compels the soil to yield a few vegetables. On the southern slope of the Alps, and in the valleys of the Valais (Wallis), which are sheltered against northerly winds, the vegetation ascends to a greater height than in German Switzerland. The vine, for instance, flourishes on the slope of Monte Rosa up to a height of 2,950 feet, whilst in the canton of St. Gall it cannot be grown beyond 1,700 feet. In Northern Switzerland cereals can be gro\\'n up to 3,600 feet, whilst rye succeeds up to 5,900 feet in the Grisons, and up to 6,500 feet on the slopes of ilonte Rosa. Irrespectivelj^ of exceptional cases, we mav sav that cultivation in Switzerland ceases at 3,940 feet. About one- half of the country lies thus above the region of agriculture, and much of the lower land is either unfit for cultivation or covered with lakes or forests. Fields, pro- perly so called, only occupy the seventh part of it, and they diminish almost every year, as meadows prove more remunerative. Next to Norway, Switzerland, of all European countries, derives least support from its agricultural resources, and nearly half the bread eaten by the inhabitants is imported from abroad. The great wealth of the country consists of its forests, its meadows, and its mountain pastures ; for trees cover one-sixth of the total area, and pastures nearly one-third. In the Valais, in the Grisons, and in the Ticino we find many barren slopes, but, as a rule, the mountains of Switzerland are distinguished for their verdure. The lower slopes are covered with forests, their upper ones with aro- matic herbs and grasses ; and their freshness and beauty impress us all the more if we call up in our mind the tottering precipices of the Alps of the Dauphine, the scorched rocks of the Apennines clad with meagre shrubs, or the dreary sierras of Spain, ashy-coloured or of a glaring red. The oak is comparatively rare in Switzerland, but nearly all the other forest trees of the lowlands of Europe ornament its valleys and the lower spurs of the Alps. The walnut-tree grows to an enormous size ; beeches and chestnut-trees cover the slopes a little higher up ; and to these succeed black woods of firs and pines, the most cha- racteristic trees of Switzerland. Higher still we meet with larches, the wood of which is highly valued, until at last the creeping pine alone is capable of success- fully struggling against the wind and the cold. Its roots are longer than its branches, and these latter repose flat upon the ground amongst a carpet of rhodo- dendrons, and are thus protected against the violence of the storms. Formerly the forests extended higher up the hillsides, either owing to the refrigera- tion of the climate, as some meteorologists assert, or, what is more probable, because of the wanton destruction of forests by man, for a single tree soon perishes 440 SWITZEELAND. where an entire forest would survive. The trunks of trees discovered in peat mosses prove conclusively that the slopes of Val Piora and of the Lukmanier were formerly covered with forests up to a height of 7,200 feet, where only pastures are found now. The upper limit of the forests has retired no less than 1,300 feet. As we ascend the mountains the minor flora likewise changes its character. Down in the valleys carefully manured meadows yield abundant crops of hay, hut hio-her up our grasses disappear, and species of arctic plants take their place. In spring the herds of cows leave the stables in which they pass the long winter, and, headed by a " leader " crowned with flowers and furnished with melodious bells, they depart for the Alps. They stay for some time on the lower pastures, but when the snow melts away from the upper slopes they mount higher and higher in search of the aromatic herbs which impart so delicious a flavour to the milk they give. Every patch of pasture is made use of ; and if cattle cannot reach it, sheep or goats are taken thither, the herdsman frequently carrying the animals upon his back. On the approach of winter the herds once more return to the valleys, and the Alps are given up to solitude. Far below the upper limit of mosses and other arctic plants animal life has ceased to exist in the mountains of Switzerland. Only about thirty species of insects and arachnidoe venture into the regions of persistent snows, which extend from 9,100 feet upwards. Between 9,800 and 10,800 feet we meet only with a few spiders. A field rat (Arvicola nivalis) has been seen at an elevation of 13,000 feet above the sea, but it has not yet been determined whether this little animal, which burrows its holes beneath ice and snow, lives permanently at such a height, or only visits such altitudes occasionally during summer. Not only quadrupeds and other land animals diminish with the height, but also fishes. The small lakes above 6,900 feet, which are frozen during a great part of the year, are very poor in them. Many plants have disappeared during the historical epoch, more especially species peculiar to heaths, swamps, and lakes, and the huntsmen have exterminated several beasts which formerly inhabited the forests and the mountain sides. The bison, or auroch, and the beaver, still numerous during the Middle Ages, exist no longer. No deer has been seen in Switzerland for more than a century ; the roe and wild boar have become exceedingly scarce, if they have not disappeared alto- gether ; and it is very doubtful whether a tortoise was seen a short time ago, as asserted. There stiU remain a few wild goats and wild cats. "Wolves are more numerous, and frequently invade the sheepfolds. The last bear was killed in AppenzeU in 1673 ; and as those in the Grisons, in Ticino, and in the Upper Yalais are sure of early extermination, the city of Bern will have to send to Asia or Africa for its symbolical animals. The chamois, or gemsbuck, is being pursued to extermination — eight himdred and twenty of these animals were killed in 1876 — and the time is not very distant when the Swiss mountains will be inhabited only by herds of domesticated animals. Birds of prey^ and more especially the lammergeier, or bearded vulture, which sometimes attacks even children, are diminishing too, but there is no reason to CLIMATE, FAUNA, AND FLORA. 441 suppose that even a single species has been exterminated. The species of birds are three times more numerous than the species of all otlicr vertebrate animals together, but three-fourths of these are merely birds of passage or occasional visitors, which make their home in Switzerland during w^ter or summer. Looking to the geo- graphical position of Switzerland, in the verj' centre of the temperate zone, and to its bold mountain ranges, it is easily understood why so large a variety of birds of passage should temporarily stay in its valleys. These birds, when crossing from one slope of the Alps to the other, will naturally seek out the lowest depressions ; and the Pass of St. Gotthard, with the valley of the Rcuss leading up to it from the north, and that of the Ticino from the south, forms one of the great high-roads most frequented by those winged migrants. The high valleys at Urseren and Andermatt afford convenient resting-places, and it is there that Swiss ornitholo- gists have captured some of their most valued specimens. These birds, indeed, pointed out to man, long before Alpine roads were thought of, the easiest passages across the mountains. CHAPTER VI.* THE PEOPLE. ] HE plains of Switzerland were inhabited centuries before the time to which our most ancient historical documents go back. Even the ages which intervened between the two glacial periods saw man encamped in the valleys of the Alps. At Yizzicone, on the Italian slope, the beds formed by moraines belonging to these two periods are separated by a layer of lignite, within which has been found a mat made of rush. Branches cut off from firs have been discovered in a sedimentary deposit dating back to the interglacial period, at the eastern extremity of the Lake of Ziirich ; and Herr Riittmeyer feels convinced that these branches were to be used for making baskets or a hedge, and prove the existence of man at that remote age. When the Romans took possession of the country several epochs of civilisa- tion had already successively passed over it without a line to record what had happened, and it is only in our own days that evidence of these past ages has been discovered in caverns, in the lakes, and in the peat bogs. The first remains of human beings, together with their primaeval implements, were discovered in caverns. At Veyrier, near Mont Saleve, Messrs. Gosse and Thioly discovered human bones and implements made of the horns of reindeer, which afford us a glimpse into the life led by these troglodytse. Other caverns at Thayngen, near Schafi"hausen, which were inhabited during the reindeer period, have yielded veritable treasures, including a bone upon which an artist of that bygone age has rudely engraved the figure of a reindeer. Of the mammals which then inhabited Switzerland there now remain only three, viz. the stag, the wild cat, and the wolf. The southern slopes of the Alps appear to have been inhabited by men of a different race, perhaps by Etruscans, and of these, too, prehistoric remains have been discovered. One of the tributary valleys of the Maggia, the Val Lavizzara, or "potters' valley," is thus named on accoimt of a soft stone, which was formerly made into pots. It is very probable that this name refers to an epoch of primitive * Eiitimeyer, "AtcIut. fiir Anthropologie," VIII. ; " Veranderungen der Thierwelt der Schweiz;" RazoumoTsky, " Histoire Naturelle du Jura ; " F. Keller, " Die Keltischen Pfahlbauten in der Schweiz ; " Troyon, "Habitations Lacustres;" Oswald Heer, "Die Pflanzen der Pfahlbauten ; " A. Heim, "Fund aus der Kenthierzeit." THE PEOPLE. 448 ^ig. 309.— The Lakb op Pfaffikon. Scale 1 : GS,000. »• !6XotP«pi civilisation, when man, not yet acquainted with the potter's wheel and the burning of chiy, made his vessels of stone. When the reindeer had disappeared, the glaciers had retired up the valleys, and the mosses of Lapland had been superseded by forests and grasses, the country was inhabited by a different race, known to us as the Lake dwellers. Swiss fishermen liad long been acquainted with the fact that there existed rows of piles in the shallow bays of some of the lakes, but they had no notion of their origin, and the archfpologists of the neighbourhood merely looked upon them as the remains of Roman embankments. Razoumovsky, towards the close of the last century, correctlj' guessed their origin, but his explanation passed into oblivion until an unexpected discovery enabled the learned to arrive at the truth. During the whiter of lSo3-0-l the level of the Lake of Ziirich fell much more than is ordinarily the case. The inhabitants of Obermcilen availed themselves of this op- portunity, and, by throwing up embank- ments in advance of the old coast, they managed to secure a considerable tract of land. On this land, beneath a layer of mud, were discovered pieces of charcoal, stones blackened in the fire, cut bones, and utensils of every description, which clearly showed that a village had an- ciently existed there. Herr Ferdinand Keller carefully examined these remains, and soon after made known the result of his examination in a work on " Celtic Pile Dwellings in the Swiss Lakes." This was the starting-point in a subject of inquiry which has largely contributed towards laying the foundations of the new science of prehistoric anthropology. It was no difficult task to reconstruct the pile dwellings of the.se distant ages. The carbonised beams discovered amongst the piles clearly belonged to a platform constructed a few feet above the water. Interlaced branches and fragments of clay hardened in the fire formed the circular walls of the huts, whose conical roof was constructed of reeds, straw, or bark. The stones of the hearth have fallen beneath the place which they formerly occupied. Vessels of clay, heaps of leaves and moss, which served as beds, arms, trophies of the chase, such as the antlers of stags or the heads of bisons, which ornamented the walls — they all have been discovered embedded in the mud. In the peat bogs which formerly were jMiIra m^ Swamps. Islands TTith pile dwell UigB. Woods. 444 S'^^TZEIlLAND. covered by the Lake of Pfaffikon, even stuffs made of flax and hemp, and pieces of carbonised wheaten bread, have been discovered. By the side of the piles we are still able to identify dug-out trunks of trees which were used as boats, whilst rows of piles indicate the position of a bridge which connected the pile village with the mainland. In a few instances an estimate of the number of houses and of their inhabitants could be made. Fp to the present time no less than two hundred of these villages have been discovered in the Swiss lakes, some of them having as many as five hundi-ed houses. The population of these villages, which need not, however, have existed simultaneously, may be estimated at 100,000 souls. This much is certain, that these lake dwellers of Central Europe were perpetually at Fig. 310. — The Pile Dwellings of Simtzerland. Scale 1 : 2,200,000. 60 Miles. war with each other, and that, like the Papuans and Dayaks of our own day, they built their houses in the midst of the waters in order to be secure against sudden attacks. The only lakes of Switzerland in which no remains of pile dwellings have hitherto been discovered are those which are very deep throughout, as the Lake of Lugano, or which are in the cold zone, as those of Thun and Brienz. Lake dwellings, some on piles, others placed on heaps of stone, bordered nearly the whole of the shore of the Lakes of Neuchatel, Biel (Bienne), and Morat (Murten). Nearly one-half of all those known to exist in Switzerland were discovered there. But they are not the oldest, it appears, for it is principally on the banks of the Lakes of Ziirich and Constanz that pile dwellings belonging to the stone age are Till-: I'KOl'I.K. 416 met with. M. Troyon has calcuhito .^- », •. andOlacierB). PopuJahon Density g j£ (lb70). {In. toil Sq. Mile). • Alps 8,885 809,531 90 Pkin 4,082 1,400,856 345 Jura 1,669 438,014 202 t Tieitio{in German and French Teuiii). — Area, 1,088 square milts; population (1870), 119,620 (1876) 121,768, almost without exception Roman Catholics. German is spoken in the village of Boseo ; Itjiliau, more or less pure, throughout the rest of the canton. Ticino includes the valleys of the 'l"ieiuo, Verzasca, and Maggia, which flow into the Lago Muggiore, as well as a portion of the fertile basin of tho Lake of Lugano, which is separated from the rest of the canton hy the Pass of Monte Cenere (3,775 feet). The principal passes leading into Northern Switzerland are those of the St. Gotthard and tho Lukniunier. At the foot of the former is the \'iUage of Airolo. The northern portion of the canton is ^Upiiie, tho southern Italian, in its character. Exports ; — Cattle, silk, straw mats, eheeso, timber, chestnuts, snails, and pot-stono. Thousands of tho inhabitants annually leave their homes and make a living as chestnut- roastcn, chocolate-makers, masons, or bricklayers in Lombardy and elsewhere. Most of the Italian iee and coffee shop-keepers in London are Ticiuesc. The principal tuwns are Lugtino, Locarno, and Bellinzona. 454 SWITZERLAND. In the upper valleys of the Ehone, on the French slope of Switzerland, we onlj- meet with small villages. Brieg (Brigue, 1,076 inhabitants) , at the foot of the Simplon, is a bustling place, and, owing to its many old towers with sparkling roofs, has something Russian in its aspect. Viq^ (Viege, 723 inhabitants) is a favourite resort of tourists (see p. 399). Lcnk (Loueche, 1,220 inhabitants) is famous on account of its saline waters. Sion (Sitten, 4,895 inhabitants), on the Rhone, the capital of the ancient Seduni and the principal town in the canton of Valais,* is an old Gallo-Roman city, commanded by two ruined castles, one of them, though only dating back to the Middle Ages, being known by the Roman name of Valeria. Martigny (Martinach, 1,490 inhabitants), at the foot of the Great St. Bernard, is a place of considerable strategical importance. St. Maurice (1,666 inhabitants), known up to the thirteenth century as Agaunum, is no less so, for it defends the gorge through which the Rhone enters the alluvial plain extending to the Lake of Geneva. Not far from St. Maurice, within the canton of Vaud,t is the wealthy village of Bex (3,804 inhabitants), with productive salt works, and one of the favourite resorts of foreigners, who take the baths or breathe the invigorating forest air. Foreign visitors have likewise contributed towards the prosperity of towns or villages like Montreux, Clarcns, and Vecei/ (7,887 inhabitants), which stand on the northern side of the Lake of Geneva. The beauty of this lake, within whose placid waters are mirrored the surrounding mountains, and the mild climate, have naturally attracted many foreigners to this favoured corner of Switzerland, and towns like Vevey are quite cosmopolitan in their character. Lausanne (26,520 inhabitants), the capital of the canton, occupying a hill about the centre of the lake, commands as fine a prospect as the towns higher up, and, like them, it annually attracts swarms of visitors. But, in addition to this, it is a • Valuis (in German Wal/U).—Axe&, 2,026 square mUes ; population (1870), 96,887, (1876) 100,490, nearly all Eoman Catholics. The canton includes the valley of the Ehone, from its source down to the Lake of Geneva. It is bounded in the north hy the Bernese Alps, in the south by Alpine ranges, culmi- nating in the Monto Rosa. The Furka Pass leads from the head of the Ehone into the valley of the Eeuss, and to the northern foot of the St. Gotthard. The Grimsel and Gemmi Passes, the latter above Leiik, and certainly one of the finest in Switzerland, connect the Valais with Northern Switzerland, and the Nufenen, SimplOn, and Great St. Bernard with Italy. The products are wine, walnuts, cherries, cattle, sheep, goats, cheese, iron, argentiferous lead, sulphur, anthracite, anda little gold in the sand of the rivers. About two-thirds of the inhabitants speak French, one-third German, and a few Eomanche. The Valais joined the Confederation in 1597. The principal tovras are Brieg, Leak (Loueche), Sion, Martigny, and St. Maurice. t Vaud (in German Waadt).—Aieii, 1,244 square miles ; population (1870), 231,700, (1876) 242,439. In 1870 there were 211,686 Protestants, 17,592 Catholics, and 610 Jews. French is spoken almost through- out. The canton extends along the northern shore of the Lake of Geneva as far as the Lake of Neuchatel, and beyond the Jura to the French frontier. The greater part of the country is hiUy and of exceeding fertility. It produces com, tobacco, fruit, chestnuts, walnuts, wine. The breeding of cattle and dairy farming are important. The mineral kingdom furnishes coal and salt. There are iron works, where ores from the Bernese Jura are smelted, and watchmaking is carried on in the Jura, but other branches of industry are hardly known. Much has been done for popular education within the last forty years. Up to 1803 Vaud belonged to the canton of Bern ; since then it has been an independent member of the Confederation. The principal towns are Bex and Aigle, in the Ehone valley ; Vevey, Lausanne, Merges, and Nyon, on the Lake of Geneva ; and Yverdun, on the Lake of Neuchatel. GliNEVX. 455 busy commercial place, upon wliich several lines of railway converge, and the seat of the principal Court of App.\il of the Confederation. It grows rapidly, and at Fig. 314. — The £A^T(u.\ Kxtrehity of thk Lake or Geneva. Scale 1 : 60,1_^^_ 1 Mile. no distant time will form one town with its port of Oiichy, with which a railway, having a very steep gradient, connects it. Genera {Genire in French, Genf in German, 67,357 inhabitants, including the 456 SWITZERLAND. suburbs) occupies an excellent geograpbical position at the lower extremity of the Lake of Geneva,* where the Rhone issues from it, and is joined by the Arve. Upon it converge all the roads which connect Central Germany with Southern Fig. 315.— Geneva. Scale 1 : 35,000. E.of Or. Km^ «-l3 Half a Mile. France, for it is there that the gap between the Alps and the Jura permits of an * Gwera .■— Area, 108 square miles; population (1870), 93,195, (1876)99,352. In 1870 there were 47,858 Catholics, 43,638 Protestants, and 961 Jews. The canton includes the town and the surround- ing country. The soil is not fertOe, but hy perseverance it has heen converted into a flourishing garden. Nearly one-half of the cultivated area is planted with vines. CiENKVA. 467 easy passage, Geneva is the natural mediator between Lyons, lower down on llio Rhone, and Central Europe. It is almost matter for siu'iiriso that this city, wliich has so frequently been chosen for international meetings, should to this day remain the " greatest amongst the small towns " of Europe. But the rigorous winters, the cold northerly winds, or bises, the fogs which frequently hang over the country, and the small area capable of cultivation, sufficiently account for the slow growth of the population. At present only a single line of rail- way passes the town, namely, that which connects Lyons with Bern and Basel. No branch lines have yet been constructed to Annecy, to the foot of Mont Blanc, or to the Jura, and for the present there is little prospect of their being built. Geneva, which became the capital of a cirifas in the foui'th century, has occupied for ages a position quite exceptional. Restricted to its narrow terri- torj' and overshadowed b}' a mountain ■wliieh it could not even call its own, the city remained for a long time a republic of exiles. Calvin disciplined its citizens in his repellent fiishion, and strangers differing from them met with no friendly reception. The men who governed it were for the most part descendants of French or Italian refugees, whom religious difTerencos had driven from their homes, and they souglit above all things to keep up the energy and the spirit which had dictated the doings of their forefathers. But this small body of men, so remarkable on account of its exclusiveness, was equally so for its love of study and intellectual vigour. Geneva, during the last three centuries, has produced more men of eminence in science and literature than any other town of equal size. It was the birthplace of Jean Jacques Rousseau, of Horace de Saussure, of Necker, Sismondi, Topffer, and Pradicr, and some of its families have almost become scientific dynasties. Manj' amongst the famous children of Geneva may perhaps be claimed also by the Parisians, amongst whom they found a second home ; but, for all that, the Swiss city has at all times been distinguished for its patronage of education and science. Its schools are among the best of the country ; its newly founded university occupies an honourable position ; there are valuable natural-history collections and many learned societies, including a geographical one. The " city of Calvin," which is just now erecting a sumptuous monument in honour of a Duke of Brunswick, might certainly be called upon to place an expiatory memorial upon the spot where Michael Servetus, the illustrious Spaniard, was burnt at the stake. Geneva is no longer the " Rome of Protestantism." Its old walls have fallen ; its ramparts have been converted into walks or sumptuous streets ; new roads, lined by countrj' houses, extend in all directions, and join the former villages of Plainpalais and Carouge to the city. The time when the whole of the alluvial peninsula between the Arvc and the Rhone will be covered with houses is fast iipproaching. The " old Genevese " now constitute onl)' a minority in their own town, which has become one of the most cosmopolitan cities of Europe, within which reside about one-fourth of the foreigners who remain during the winter in 458 SWITZERLAND. Switzerland.* Geneva, though its population is now double what it was some j'ears ago, has unfortunately lost the two great branches of industry which carried its fame into all parts of the world, viz. the manufacture of jewellery and watches. France and the United States, which formerly obtained these articles from the workshoiJS of Geneva, are now able to supply their own wants by home manufac- ture, and many of the Genevese masters have been ruined. t The Arve and the Rhone are capable of supplying motive power to an almost unlimited number of factories, but have not yet been utilised (see p. 424). As a place of commerce and money market Geneva possesses considerable resources. Geneva owes its importance to the vicinity of France ; but, as long as Italy remained the centre of civilised nations, the most populous town of Switzerland naturally existed in a different part of the countrj'. Aventicum, a Celtic town, having as patroness a deity named Aventia, became the capital, and its geogra- phical position justifies the selection made. It stood on the shore of the Lake of Morat, or Murten, which was more extensive then, in a depression of the undu- lating plain which separates the Alps from the Jura. It was nearer to the Lake of Geneva than to the northern frontier of Helvetia, and the Romans were able to reach it from Agaunum (St. Maurice, in the Rhone valley) in two or three days' march. At it they established the central custom-house for the whole of the eastern frontier of Gaul. The Alemanni destroyed the town, and there now only remain a few walls covered with shrubs, two towers, pavements, statuettes, mosaics, and inscriptions. The surrounding country, which was amongst the best culti- vated in Helvetia, became one of the most barren, and in the Middle Ages was known as Urhtlancl ; that is, "fallow land." Since then a new town, Avcnclies, has been built upon the hills overlooking the site of ancient Aventicum, and numerous villages have sprung up in the environs. To the north-east of it, on the shores of the lake, is Morat (Murten, 2,328 inhabitants), still enclosed by a turreted wall, and famous on account of the defeat inflicted upon Charles the Bold of Burgundy in 1476. To the south-east is Frihourg (Freiburg, 10,904 inhabitants), the capital of the canton of the same name, and, like Murten, near the linguistic boundary. Its Gothic cathedral and gabled towers command the deep valley of the Sarine (Saane), here spanned by a suspension bridge nearly 1,000 feet in length, and • Population of Geneva, according to M. P. L. Dunant : — 1843. lOTO. Natives of the canton 68 per cent. 384 per cent. „ other Swiss cantons . . . . 20 „ 22-6 „ Foreigners 21 „ S90 „ Foreigners residing in Geneva : — 1880. 1870. French and Savoyards 11,579 14,251 Germans 1,509 2,038 Italians 600 763 Others 500 1,127 14,188 18,179 1865. 1875. t Master jewellers and watchmakers .... 225 205 Workmen employed by them 1,586 1,028 NEUCHATEL. 450 passing higli above the river, llic liousi's, and fields. Another bridge crosses the neighbouring gorge of the Gotterin at a height of 318 feet.* From Tverdiin (5,889 inhabitants), near the southorn extremity of the Lake of Xeuchatel, diverge all the roads which lead to the Lake of Geneva. It is the modern representative of the Gallic city of Ebrodunum, and fourteen centuries ago the lake, from which it is now separated by a swampy plain, still washed its walls. The castle of Granson, three miles to the north, defended the road Fig. 316. — MoRAT (Mcbten) am) its Laks. Bode 1 : 100,000. tofP (ofO 1 Mile. which passed between the Jura and the western shore of the lake, and near it Charles the Bold suflFered a terrible defeat in 1476. Neuchatcl.i the capital of a canton, occupies a commanding position near the • Fribourg (Freiburg).— Area, 664 square miles ; population (1870), 110,832,(1876) 113,952. In 1870 there were 93,0.51 Catholics and 16,819 Protestanta. About 74 per cent, of the inhabitants speak French. The canton is drained by the Saane, or Sarine. The south-eastern portion is mountainous, but none of the Bommits reach the snow-line. ITie greater portion is hilly, with rich meadows and pasture-lands, and Gruyire cheeses are known throughout the world. The cereals grown generally cover the requirements of the population. Amongst the products are timber, wine, fruit, peat, and coal. Straw-plaiting is carried on extensively, and there are tan-yards, saw-mills, a glass factory, and a beet-sugar factor}-. Watches are manufactured at Murten. In educational matters the canton is very backward, except in the district of Murten, which is inhabited by German Protestants. The principal towns are Fribourg, Murten, and Bnlle. t XeueliiUl (Xcuenburg).— Area, 312 square miles ; population (1870), 97,284, (1878) 99,729. In 1870 there were 84,334 Protestants and 11,345 Catholics. Eighty-seven per cent, of the inhabitants speak French. The canton lies between the eastern shore of the Lake of Kcuchitel and the French frontier. It is intcr- ■ect«d by four parallel ridges of the Jura, covered with forests or poor herbage. Wine is grown along 460 SWITZERLAND. point of junction of the roads and railways which skirt the shores of the hike and run through the valley of Travers into France. It is a fine town, the houses in its modern quarter being for the most part built of a light-coloured limestone. The wealthy landowners and nobles of the canton form a sort of aristocracy, but Neiichatel is justly proud of its schools, its museum, and its library. Chaux-dc-Fonds (19,930 inhabitants), in a valley of the Upper Jura, close to the French frontier, and about 3,300 feet above the sea, is the great industrial centre of the canton, and its most populous town. In the sterile mountains, where the soil refused to yield subsistence to the men who dwelt iipon it, it became necessary to look to industrial occupations as a means of subsistence. The first watch was made at Chaux-de-Fonds in 1680, and since then that branch of industry has grown immensely, and is carried on also at Le Lode (10,334 inhabitants), and in many villages in the vicinity. The district remains to the present day the chief centre of watchmaking in the world, and although the number of workmen has recently decreased, the number of watches turned out is larger than ever.* Ironically the natives compare the " village " of Chaux-de-Fonds with the "city" of Neuchatel. A portion of the manufacturing district of the Jura lies within the canton of Bern, which extends from the highest summits of the Alps to the frontiers of France.t The capital of this canton and of the entire Confederation (3,600 inha- bitants) occupies an advantageous site half-way between the Rhone and the Rhine, and on the Aar, which affords the easiest access to the Oberland. During the the foot of tho Jura. Clipose forms an article of export, l)ut two-thirds of the com required have to be imported. The manufacturing industry is of importance. Cotton stuffs, lace, and watches are the chief articles produced. The principal towns are Neuchatel, Chaux-do-Fonds, and Le Locle. The principality of Neuchatel originally belonged to Burgundy. Rudolf of Haljsburg ceded it in 1288 to John of Chalons. In 1707, the reigning prince having died without heirs, the Estates acknowledged the claims of Frederick of Prussia, and Neuchatel remained a Prussian dependency until 1857. As such it became a member of the Swiss Confederation in 1815. * In 1870 there were 4,505 watchmakers at Chaux-dc-Fonds; in 1877 only 4,172. About 1,450,000 watches are annually manufactured in the Swiss Jura, their estimated value being £1,200,000, or 16s. each. t .B,-™.— Area, 2,660 square miles; population (1870), 500,455, (1876) 528,670. In 1870 there were 436,307 Protestants, 66,015 Roman Catholics, and 1,400 Jews. About one-seventh of the inhabitants speak French. Geographically this canton, next to that of the Grisons, the largest of Switzerland, consists of several well-detined regions. The Bernese Oberland, with its glaciers and lakes (including those of Brienz and Thun), has been fully described elsewhere. Cattle-breeding and dairy -farming are the principal occupa- tions of the inhabitants. The valleys of Simmen and Saanen — the one tributary to the Lake of Thun, the other to the river Aar^are famous for their fine breeds. Wood-carving employs many of the inha- bitants during winter. The principal towns or villages of the Oberland are Thun, Interlaken, Brienz, Meiringen, and Saanen. The Mittelland, or hilly region, is intersected by the rivers Aar and Emmen, and is for the most part a fertile region. It extends north into the Upper Aargau, the most productive district of the canton. The Emmen Thai is famous for its cheese, its wooden houses, its wrestlers, and its floods. The principal towns in this section of the canton are Bern, the capital, on the Aar ; Langnau and Burgdorf, on the Emmen ; and Wangen, in the Upper Aargau. The Seeland (see page 425) is drained by the rivers Aar and Zihl. the latter being the effluent of the Lake of Biel, or Bienne. Lastly, there is the Bernese Jura, comparatively sterile, but a busy seat of industry. Its leading towns are Moutiers and Porentruy. The canton of Bern is wealthy, no doubt, but in no other part of Switzerland are the contrasts between rich and poor so marked. Cattle-breeding, dairy-farming, and in the plain the cultivation of com and potatoes, employ the bulk of the inhabitants. About 150,000 tons of iron are produced annually in the Jura, and the manufacture of linens and other textile fabrics, lace, watches, carved woodenware, leather, &c., is of some importance. The national costume of the Bemese is amongst the most picturesque to be met with in Switzerland. BEBX. 461 wars of the Middle Ages this po&ition entailed great strategical advantages, more especially as the town stands upon a peninsula bounded on thi-ee sides by the steep banks of the river. A wall built across the neck of this peninsula thus sufficed to protect the inhabitants in case of attack. Bern, unfortunately, is not favoured bv Fig. 317.— Bern. Scale 1 : (0,000. I MUc. the climate, and the extremes of temperature are greater hero than in any other town of Switzerland.* It is much exposed to the winds, and the death rate is very high, especially in the poorer quarters. The damp tortuous street following the • Extremes of temperatoro at Bern, 972 and —22° Fahr. DifTerence, 119-2° Fahr. Mean unuual temperature, •16' Fahr. VOL. II. 11 U 402 SWITZERLAND. windings of the Aar is one of the most insalubrious places in Europe, and maladies reign there permanently as in a hospital. The wretched streets of this quarter con- trast painfully with the palatial buildings which rise among the gardens to the west of the city, and whence may be enjoyed the fine panorama presented by the mean- dering Aar and the snow-clad Alps rising in the distance above verdure-clad hills.* Amongst the most remarkable buildings of the town are the Federal Palace, Fig. 318.— View of Been. ■f*^ erected in 1852 — 57, the Gothic Minster, the Hospital, the Post Office, and the bold Nydeck Bridge which leads to the famous Bear Pit. Bern is the seat of a university, possesses several libraries and miiseums, but cannot compare with Ziirich as regards scientific associations. Amongst its famous children more warriors are mot with than men of learning : of the latter A. von Haller (died 1777), the poet and physician, is perhaps the most widely known. * Death rate of Bern (1855 — 67), 35-2 per 1,000 inhabitants; in the upper quarters of the town, 12'6 per 1,000; in the Aarherger-Gasse, 748 per 1,000. BEEN. 4C8 Bern, which according to some etymologists is i\ corruption of the Celtic name of Verona, whilst others derive it from Barcii ("bears"), still preserves a mediaival physioguomy in its interior (juarters. The pomp uud strength of feudal Switzer- land are called up before our mind when wo look at the solid walls of the houses, at the buttresses which support them, at the "rows" similar to those of Chester, at steep-peaked roofs, and fountains ornamented with quaintly sculptured figures. We can almost fancy these streets being filled with men-at-arms flushed with victory or returning from the pillage of a village, waving their banners and blow- ing their horns. Uern has u few factories on the banks of the Aar, industrial suburbs beyond the public walks, and extensive quarries near the neighbouring Fig. 319. — Ikterlaken. Scale 1 : 70,noo. 1 Mile. C xm ^£vw village of Ostermundingen, but the great industries of the country, the manufacture of cheese, linens, and cloth, and straw-plaiting, are principally carried on in the wealthy communes of the Emmenthal, at Laiignau (G,214 inhabitants), Sumisicald, and 2?Mr(/f/o/;/" (Rerthoud, 5,078 inhabitants), each of which towns has its agencies throughout Switzerland and in many foreign countries. In tlie old castle of Burgdorf Pestalozzi established his educational institute (1798 — 1804). At T/iiin (Thoune, 4,623 inhabitants), whore the Aar escapes from the lower lake of tho Obcrland, there are likewise a few factories, but that town is important ratlier because so many travellers annually pass through it on their road to Intcrlaken, within easy reach of the delightful scenery of the Obcrland. It is the military capital of Switzerland, the seat of the Military College of the Confederation, and 11 II 2 464 SWITZEELAND. of an arsenal. It is a quaint city, with " rows," overlooked by an old castle, now converted into a prison, and the parish church built ujDon the summit of u commanding hill. In the vicinity of Bern and in the Alpine valleys of the canton there are many wealthy and populous villages, some of them remarkable on account of their huge wooden houses ornamented with sculptures. Interlaken, on the alluvial plain of the Bodeli, which separates the Lakes of Thun and Brienz, is one of the favourite haunts of tourists. It is named after a convent ("inter lacus"), suppressed in 1481 in consequence of the immoral life led by the nuns, and now occupied as a school. The climate is mild, and the environs abound in delightful v.alks. The valley of the Lauterbrunnen, in the south, leads up to the famous falls of the Staubbach and Schmadribach. The icy summits of the Jungfrau tower majestically beyond it. The glacier of Grindel- wald is within easy reach, and a steamer rapidly conveys the traveller to Brienz, Fig. 320. — BiEL (Bienne) and the New Bed of the Aak. Scale 1 : lon.onn. ,E.i of Pari 7"2o'E.ofCr. C rerroi 1 Jlue. with its pretty boating girls, to the Giesshaeh, and the charming Hasli valley, whose chief viUage, Meiringen, fell a victim to a fearful conflagration in February, 1879. Biel (in French Bienne, 8,113 inhabitants), favourably situated at the northern end of the lake named after it, opposite to the mouth of the valley of Suze, which leads into the Jura, and close to the Aar navigation, has become a great place of commerce, and its inhabitants speak of it as a Zukunftstadt ; that is, a town having a future in store for it. Quite the reverse might be said of Solothurn (Soleure, 7,054 inhabitants),* lower down on the Aar, which reflects its turrets and crenel- lated walls, and almost deserves to be called a " town of the past ; " whilst Olten • Solothurn.— Area, 303 square miles; population (1870), 7-l,713, (1876) 77,803. In 1870 there were 62,072 Catholics and 12,448 Protestants. German is spoken thi-oughout. The canton includes a portion of the fertile valley of the Aar, which abounds in orchards, and produces com for exportation, whilst the Jura, in the west, is sterile. There are valuable quarries of marble, limestone (at Olten), and millstones, as well as iron mines. Silk-wea^ong is carried on on the northern slope of the Jura, in the BO-caUed " Black Boys' Land." The only towns of note are Solothurn and Olten. Li5RARY OF THE UNIVERSITY of ILLINOIS. BASEL. •IG5 (2,998 inhubitauts), still lower down in tlie valloy, has bwome an iiiipirlaiit railway centre, and increases annually in connuorce and industry. Hosiery, glass, and parquetry are manulacturcd, and there arc huge railway workshops for tbo con- struction of locomotives and rolling stock. The railway which pierces the Jura in tlie tunnel of llauensfein, and runs past Liintiil (.■1,87.'3 inhabitants) to Basel, placca Olten in cunununication with the railway sj'stums of Frauce and Germany. Basel* (44,834 inhabitants), by its commerce, history, and general influence upon the economical condition of Switzerland, has much in common with Geneva. Fig. 321.— Basel (Bale). Roilo 1 : 50,000. >°t.l > t-... l.~ UuU n SUlc. Admirably situated upon a terrace at the great elbow of the Rhine, where that river enters upon the plain of Alsatia, it occupies commercially the same position towards Germany and Xorthern Franco as that held by Geneva with reference to Southern France. Nay, its market is even more extensive, and two-thirds of the • lintrl tia French Siilr) furms two oantons, viz. Basel To«ii (14 squnro miles, 51,515 inhaliiUintj in 187C|and Basil Countrj- (103 B:<-. b Miles. felden, and Ryburg. Augst occupies the site of Augusta Rauracorum, a town founded by Lucius Munatius Glaucus, which formerly experienced the same amount of com- mercial prosperity as that enjoyed in our own days by Basel, its fortunate successor. One-half of the village of Augst lies within the canton of Aargau, the capital of which is situated in the valley watered by the Aar.* Aargau (5,449 inha- • Aargau (in Vrejieh Argov'u). — Area, 543 square miles; population (1870), 198,875, (1876) 201,567. In 1870 there were 107,703 Protestants, 89,1^0 Catholics, and 1,541 Jews. The canton includes the lower valley of the Aar, which is joined within its boundaries by the Reuss and the Limmat, and extends north to the Rhine. It is for the most part hilly and fertile. The products include wine and salt (300,000 cwts. ). There are cotton-mills (265,000 spindles), dye and print works. Straw-plaiting occupies about 30,000 operatives during winter. Much has been done for education. The principal towns are Aargau, Zofingen, Baden, and Reinach. 468 SWITZEELAND. bitants) is not a large town, but its inhabitants are distinguished for their culture, and many industries requiring skill, intelligence, and even a scientific training, such as the manufacture of instruments, are carried on. Eighteen centuries ago, Vindonissa, at the triple confluence of the Aar, the Limmat, and the Reuss, was the great strategical centre of the country. It was upon this town that the Roman roads converged which crossed the Alps from Italy, and the legions stationed there were favourably placed for supporting those which held the frontiers of the Rhine and of the Danube. But its very importance led to the destruction of this stronghold. Several times captured towards the close of the Empire, there now remain but a few insignificant ruins, and only its name survives in that of the Fig. 324.— The Lake of the Fovr Cantons (Vif.rwaldstattek See). Scale 1 : .SOO.OOa T Eof.P. 5 Miles. village of Windisch. The wars of the Middle Ages prevented the recon- struction of this ancient city, but several towns have sprung up in its vicinity, such as Bnigff, at the mouth of the Boetzberg tunnel ; SchinznarJi, famous on account of its sulphurous waters ; and Baden, the hot springs of which were highly appreciated by the Romans. It is certainly curious that no large town should have arisen in so favourable a locality. On a hill which rises to the south are the ruins of the feudal castle of Habsburg, the ancestral home of the imperial family of Austria. If we trace the Reuss to the point where it issues from the Lake of the Four Cantons, we reach Luzern (14,524 inhabitants), the political and commercial THK FOREST CANTONS 409 metropolis of primitive Switzerland, and the capital of a large canton.* Its position, at the lower end of the lake and upon its effluent, is analogous to that of Geneva, Ziirich, and Constanz. AnoUier river, the Little Emnie, joins the Reuss about a mile below Luzern. Turretcd walls surrounding the town, an old lighthouse, or fucenuj, the blue and swift waters of the Reuss, the lake, and the view of the mountains which enclose it, render Luzern one of the most attractive cities of Switzerland. The number of strangers who pass through it every summer is very great. Luzern, the most Catholic city, was the capital of the Swiss " Sonderbund," or " Separatist League," which fought between 1845 and 1847 in favour of the pretensions of the Jesuits. Its most remarkable monument is a lion carved out of the solid rock, from a design bj' Thorwaklscn, and recalls the time when the Switzers sold themselves as soldiers to the sovereigns of Europe. Though favour- ably situated, Luzern has little commerce or industry, but, like Ziirich, it expects great things from the completion of the tunnel through the St. Gotthard. ScmjMuh, the village rendered famous through the battle fought there on the 9th July, 1386, lies to the north-west of Luzern, on a small lake. Kitssnacht and Wdggis are villages on the Lake of the Four Cantons, and at the foot of the Rigi. In the three other Forest Cantons t the towns are few in number, and even the capitals are hardly more than villages. Altorf, or Altdorf (■2,7"24 inhabitants), is still the simple village as in the legendary age of William Tell ; Stanz (2,070 • LtizfTH (in French Lu(tr»t).—kiea, 579 square miles : population (1870), 132,338, (1876) 133,316. In 1870 there were 128,338 Catholics and 3,823 Protestants. The canton includes three distinct regions, viz. the Gail, in the north, the centre of which is occupied by the Lake of Sempach ; the country adjoining the Lake of the Four Cantons, together with the valley of the Reuss : and the mountain valleys drained by the Little Emmc and its tributaries. The most important of these valleys is known as Enllibuch. Its inhabitants depend almost wholly upon dairy-farming for their subsistence, and, like their neighbours in the valley of the Great Enmio, they are expert wrestlers. The mount.iins bounding these v.alleys rise to a height of 7, HO feet, and are covered with turf and aromatic herbs. There are no glaciers in tho canton. Agriculture and dairy-fanning are the principal occupations. The soil, almost throughout, is fertile. There arc extensive forests. + The Forest Cantons, or Vicrwaldstatte, are Luzern, Schwyz, TTri, and Unterwalden. Luzern has been noticed above. Schwyz (Schwitz, hence Switzcr and Switzerland). — Area, 351 square miles; population (1876), 4!*, 216, nearly all Catholics. l"he canton extends from the Lake of the Four Cantons to that of Ziirich, and may be described as a platform 2,700 feet in height, above which rise the naked rocks of the Slythenand other mountain summits. The Rigi lies almost wholly within the limits of the cantons, a plain and the small Lake of Lowerz separating it from the rest of the canton. The valleys are fertile, tho most important amongst them beiag those of the Sluota, which flows into the Lake of the Four Cantons, and of the Sihl, a tribu- tary of the Lake of Ziirich. Cattle-breeding and dairy-farming are the principal occupations. Silk and cotton mills have been established by Ziirich manufacturers. ITie only places of impoi-tancc arc Schwyz and Gcrsau. rn'.— Area, 415 square miles ; population (1876), 16,900, all Catholics. Tho canton extends from tho southern bay of the I>ake of the Four Cantons up to the St. Gotthard and Furka Passes, and thus includes the valley of the Reuss, known at its head as Crseren Tlial, and all its tributary valleys, with the famous Mayenthal. Cattle-breeding and dairy-farming support the majority of the inhabitants. Com is grown on about 14,000 acres ; forests cover about 42, and glaciers 44 square miles. Altdorf and Andermatt are the principal villages. 'ITie Great St. Gotthard railway will traverse this canton throughout its length. UiiUncalden extends from the southern shore of tho Lake of the Four Cantons, and includes the valleys of the Samer Aa and of the Engelberg Aa, the one extending up to the Briinig Pass, the other to tho foot of the snow-clad Titlis. Since 1100 Untenvalden has formed two cantons, one "nid" ("below"), the other " ob dem Wald " (" above the forest "), whose combined area is 296 square miles, with a population (1876) of 27,002 inhabitants, nearly all of whom are Roman Catholics. The country is distinguished for its picturesque scenery. Its meadows and pastures are luxuriant, and cheese (20,000 cwts. annually), fruit, walnuts, spirits, and cidor arc exported. ITie princiiml villages are Stanz aud iNiruun. 470 SWITZERLAND. inhabitants) and Sarnen (3,720 inhabitants), the capitals of the two half-cantons of TJnterwalden, are merely villages. Brunncn, on the lake and the Axenstrasse, is one of the most-frequented places on the St. Gotthard road, with large storehouses. Gcrsau (2,274 inhabitants), formerly the capital of an inde- pendent republic, is visited now by a few foreign valetudinarians in search of a sheltered abode. Schwyz (6,154 inhabitants), at the foot of the Mythen, is a larger place than either of the above, but the number of inhabitants assigned to it in the census includes those of several of the villages in the vicinity. It lies close to the Lake of Lowerz, beyond which is Goldmi, built on the debris resulting from the great landslip which took place in 1806, and buried four villages. Einsiedlen, the native place of Paracelsus, consists of a few detached hamlets, the most considerable amongst which has for its centre a famous old abbey, annually visited by 150,000 pilgrims and tourists. The printing-office there, which limits itself to the production of religious books, is one of the largest establishments of that kind in Europe. The great boast of the monks at the abbey is to have collected, in the ninth century, the most ancient copies then existing of the monu- mental inscriptions of Eome and Pavia. The gorge of Morgarten, to the south- west of Einsiedlen, recalls the decisive victory achieved by the Confederated Swiss in 1315 over the iron-clad knights of Austria — a victory which insijired them with confidence in themselves. Zug (4,277 inhabitants), on a lake named after the town, is the capital of a small canton of great antiquity, but not otherwise remarkable. Cham, a village on the same lake, has a paper-miU, a cotton-mill, and the extensive establishment of the Anglo-Swiss Condensed Milk Company.* Zurich'^ (56,695 inhabitants), the principal town of north-eastern Switzerland, * Zur/. — Area, 92 square miles ; population (1876), 21,775, nearly all Roman Catholics. The canton includes the country to the west, north, and east of the Lake of Zug, together with the valley of the Lorze, the effluent of the Aegeri Lake. lis surface is hilly and fertile. Agriculture and dairy-farming are the principal occupations, hut there are also cotton-mills. Zug is the capital. The canton joined the Con- federation in 1352. t Zurich. —kiea., 666 square miles ; population (1870), 284,786, (1876) 294,994. In 1870 there were 263,790 Protestants, 17,972 Catholics, and 504 Jews. The canton includes the greater portion of the Lake of ZUrich, together with the land on hoth sides of it, and extends to the Rhine in the north. The principal valleys are those of the Limmat, of the Glatt, of the Toss, and of the Thur, all of them tributary to the Rhine. In addition to the Lake of Ziirich there are the Greifensee and the Lake of Phiiffikon, hoth in the raUej' of the Glatt. The Schnebelhorn (4,248 feet), on the frontier of St. Gallen, is the highest summit within the boundaries of the canton, the whole northern half of which is undulating, with fertile fields, rich meadow lands, and wooded hilln. Agriculture ia carried on with great care, and the use of agricultural machines general. The land is much subdivided. About 12.5,000 acres are under the plough; 116,000 acres consist of meadows ; 13,000 acres are planted with vines ; and 128,000 acres are covered with forests. Market gardening is carried on with greater success than elsewhere in Switzerland. The breeding of cattle and dairj'-farming are of great importance. The mineral kingdom supplies coal, peat, gypsum, marl, and building stones. Manufacturing industries flourish. The cotton manufacture employed, in 1871, 660,136 spindles, 6,265 power-looms, and 9,536 operatives. The manufacture of silk gives occupation to 18,000 operatives, most of whom work at home. About £2,000,000 worth of .silk stuff's are exported annually, j-ielding a profit of no less than £720,000. The woollen and linen industries were of greater importance than they are now. The machine shops and foundries (3,563 operatives) are the most important in Switzerland. There are likewise potteries, paper-mills, chemical works, saw, oil, and gypsum mills. Straw-plaiting is principally carried on in the Rafzerfeld. Much has been done to promote the education of the people, perhaps more than in any other canton of Switzerland. The principal towns are Ziirich, Winterthur, Wadensweil, Uster, and Horgen. The canton joined the Confederation in 1351, fifteen years after its Patrician Government had been overthrown by the people. . . J\*V>J' ' ■' \'A'T lf r ' U5RASY <3F THE UNIVERSIIY of ILLINOIS, OLABUS. 171 at the foot of the Uotlibcrg, and at the lower end of its lake, where the rivers Limiuat and Sibl effect their junction, is far more accessible than Luzern, and commands some of the most imiwrtant natural bi;^h-roads. ITence its strategical iiuportauce. It was at Zurich, on the Jird N'ondcniiaire of the year VIII., that Massena saved Franco by annihilating the Russian army marching upon Basel. The city of Zwingli is but little inferior to that of Calvin, as regards the number of its inhabitants, but it is far superior to it in the facilities which are offered by its numerous educational institutions, its Polytechuicum, its university, its museums and libraries. Ziirich makes great efforts to deserve the epithet of " Athens of Switzerland," which its citizens have bestowed upon it. Scheuchzer, the tirst man who studied the physical geogniphy of the Alps in a scientific spirit, was a native of Zurich, as was also Lavater, the famous physiognoiuist. It is a manufacturing town, too, with silk and cotton mills, foundries, and machine shops. Steam-engines constructed at Zurich have been exported even to England and to America. ^lore than half the corn trade of Switzerland is conducted by Ziirich houses, its leather fairs are well attended, and the visits of commercial travellers are more frequent than in any other town of Switzerland. Zwingli preached in the old parish church, a basilica of the twelfth century. The silk and cotton industry enriches also many of the neighbouring towns and villages as far as the canton of Zug. Wahl (5, 0-55 inhabitants) and Usfer (5,808 inhabitants), to the east of Ziirich, on the river Aa, which connects the Pftiffikon with the Qreifen Lake, are busy manufacturing centres. The river Aa, which supplies motive power to the numerous mills of these towns, is popularly known as the " river of millions." Wintcrthur (9,404 inhabitants), next to Ziirich the most important town of the canton, is the modern representative of the Roman station of Vitodurum. It is ambitiously termed the Liverpool of Switzerland, because it imports so much cotton. There are, however, few towns of equal size which can boast of more varied industries, or of a larger number of educational and other public institutions. Its foundries and machine shops are more especially noteworthy. Giants* (in French Glaris, 5,516 inhabitants) is the capital of a canton and a busy manufacturing and commercial centre, but in the mountain country of the Grisons,t which lies beyond it, there are no manufactures, and Chtir (in French • Glarut.— Area, 267 square miles ; population (1876), 36,129. In 1870 there were 28,238 Protcstanta and 6,8S8 Catholics. The canton includes the valley of the Llnth, as far as the Walon Lake, and is quite Alpine in its character, glaciers covering 6 per cent, of its surface. Formerly a land of herdsmen, it haa become a manufacturing country, cotton and woollen mills and hosiery manufacture emjiloying more hands now than dairy-farming or agriculture. The battles of Naeft-ls (1352 and 1388) resulted in the liberation of the canton from the yoke of Austria. t Graubundcn (Grisons).— .rVrea, 2,774 square miles; population (1870), 91,782, (1876) 92,906. In 1870 there were 51,887 Protestants and 39,843 Roman Catholics. The canton is the largest in Switzerland, but very thinly inhabited. It includes the valley of the Upper Rhine ; the valley of the Upper Inn, or Engadin, separated from the former by the Albula Alps ; and the valleys of Calanca and Misocco, on the southern slope of the Alps, and tributary to the Ticino. Only about 5 per cent, of the area is cultivated (barley is grown up to 5,810 feet, wheat up to 4,740 feet). Wine is grown around Chur and on the Italian elopes. Sericulture and the breeding of snails (for exportation to Italy) are likewise of some importance. The mines supply lead, copper, silver, and iron, and there are quarries of marble, alabaster, and pot-stones. Amongst the 6fty mineral springs are Tarasp and St. Jloritz. In the tenth century the Grisons were annexed to the Gorman Empire, and numerous eccleaiattical 472 SWITZEELAND. Coire, in Italiau Coira, in Romaic Quoira, 7,552 inhabitants) is the only town deserving the name. It is, above all, a place of trafBc, for the roaas which run over the Alpine passes of the Spliigen and the Bernardino into Italy, and those which cross the Julier, Albula, and Fluela Passes into the Engadin, diverge from it. The cathedral is a remarkable building, said to date back to the eighth century, and there are also the remains of a Roman tower (]Mars in Oculis). Other places of interest are Ilanz, the capital of the Grey League, and Discntis, with one of the oldest abbeys in Christendom, founded in the seventh century by Sigisbert, the Scotch apostle, but burnt, together with its invaluable library, in 17C9, by the French, both on the Rhine, and Samaden, St. Moritz, and Tarasp, in the Engadin. The latter two are famous watering-places. Sf. Morifz, in the Upper Engadin, 609 feet above the sea, has acidulous and ferruginous springs, whilst Tarasp (4,912 feet), in the Lower Engadin, and its neighbourhood, abound in springs of nearly every kind, including mofettas, or gas springs. At both places huge hotels have been constructed for the accommodation of visitors. The villages in the Engadin are generally wealthy, many of the inhabitants having made their fortunes abroad as pastrycooks or coffee-house keepers. Descending the Rhine, wo pass from the Grisons into the canton of St. Gallon.* On our left we perceive Ragatz, a famous bathing town, suj)plied from the springs of Pf affers, higher up in the Tamina valley, which here debouches upon the plain of the Rhine. The only Swiss town in that plain is Altstdttcn (7,575 inha- bitants). But long before we reach it a road and railway branch off towards the west at Sargans, and, passing to the south of the Walen Lake, conduct to the curious old city of Rapperswyl, on the Lake of Ziirich, here crossed by a wooden bridge. St. Galkn (16,675 inhabitants), the venerable capital of the canton, lies to the west, beyond the Alps of Appenzell, in a valley tributary to the Lake of Constanz. One thousand years ago, in the age of the Carlovingians, the abbey of St. Gall was the most famous school of learning in the world. A monk there and secular lords ruined the wealth of the country by their continual quarrels. The people at various times rose against them, and destroyed the 183 castles which they had built. In 1393 the inhabitants of the Lower Rhine valley, of the Albula valley, and of the Engadin, formed the League of God's House (Lia Ca De), at the head of which was the Church of Chur. In 1424 the inhabitants dwelling along the two head-streams of the Rhine and on the Italian slope formed the Grey League (Lia Grischa, in German Graubundeii, in French Grisons), thus named on account of the grey dress usually worn. In 1428 — 36 the small villages to the east of Chur, in the Praetigau (Landquart valley"), the Schanfigger valley (Scana \-ieus), and the Davos valley formed the League of the Ten Courts (Lia dellas desch dretturas). In 1473 these three leagues combined and joined the Swiss Confederation. Of the inhabitants 30 per cent, speak German, 14 percent. Italian, and 56 per cent. Romaic dialects. These latter, however, in addition to their patois, speak in most instances either German or Italian. * Sf. Gallen (St. Gall).— Area, 780 square miles; population (1876), 196,834. In 1870 there were 116,060 Roman Catholics and 74,.573 Protestants. The canton includes the valley of the Rhine down to the Lake of Constanz, the flourishing old county of Toggenburg, drained by the river Thur, to the north of the depression through which the Rhine formerly took its course, and which extends from Sargans, in the east, to the Lake of Zurich in the west. Within it lie Lake Walen and the vale known as Gaster. The southernmost portion of the canton is exceedingly rugged, and partly covered with glaciei-s. Dairy- farming and agriculture are of importance ; and there are productive coal and iron mines, slate and other quarries. The manufacturing industry is mostly confined to the old county of Toggenburg. It supplies cottons, lace, embroidery, linen, and silk. The principal towns are St. Gallen, Altstatten, Wattwyl, Rorschach, Wallenstadt, and Rapperswyl. TIIUROAU. 478 compiletl the famous chroulclo wLii-li recounts the achievements of Charlemagne ; and Gerniau becauK' a fixed Lmguage there long before Luther translated the Bible. This famous old abbey was suppressed in 18l»t>, but its library, with its 1,506 precious codices and 21,000 volumes, has been carefully preserved. In addition to it there exists a town library of 28,000 volumes. The founder of the abbey, St. Gall, an Irishman, lies buried in the abbey church. The town, in sjjite of its great elevation above the sea (:i,'.Hio feet), has grown into a manufacturing centre since the thirteenth century. Formerly the linen manu- facture predominated, but now embroidered muslins form the staple produce, and the vast meadows surrounding the town and its suburbs have been converted into bleaching grounds. The manufacturers of St. Gall are a pushing race, and maintain agents in all parts of the world. The valley of Toggenburg, which is drained by the Thur, and has Watticyl (5,494 inhabitants) for its capital, lies to the west of that town, and forms one continuous street of factories, and one-eighth of all the cotton stuifs manufactured in Switzerland are produced there. Uerismi (9,727 inhabitants), the largest town of the canton of Appenzell, belongs to the manufacturing district of St. Gall. As to Appenzell itself (3, govie) / tTicino (Tcssin) Vaud (TVaadt) tValais (Wallis) . Ncuchatcl "I (Xcucnburg) J JGenfeve (Genf, ) Genera) / Total • Total Area. Sq.51. 6.56-9 2659-9 679-5 415-4 350-8 18.33 11-2-2 266-9 92-3 644-4 Glaciers. tq.M. lU-4 44-3 0-5 3-9 1-4 13-9 0-04 0-4 2-9 138-7 131 4-3 375-2 710-0 luhnbitonts. Lakes. Dec. 31, 1870 July 1, 1876 Inhnb. to rrcrailing Sq M. (Census). (Estimated), a Sq. M. Nationality. 29-2 284,786 294,994 443 German 47-4 606,455 628,670 236 Germ., French 25-2 132,3;!8 133,316 230 German 7-8 16,107 16,900 41 21-0 47,705 49,216 141 4-4 124 2-7 13-1 451 0-1 0-04 0-2 29-6 6-8 3-3 50-4 25-6 156-6 6-7 36-9 11-6 635-1 14,415 11,701 35,151 20,993 110,832 74,713 47,760 54,127 37,721 48,726 11,909 191,015 91,782 198,875 93,300 119,620 2.31,700 90,887 97,284 93,196 2^69,095 15,009 11,993 36,179 21,775 113,952 77,803 51,515 65,548 38,925 48,879 11,907 196,834 92,906 201,567 95,074 121,768 212,439 100,490 102,843 99,352 2,759,854 82 107 134 236 177 259 3,680 280 344 488 195 252 34 373 250 lU 195 50 331 920 173 French, Germ. German ( Germ. .Romaic, ( It.ilian German German Italian French ( French, Germ., ( Italian French French t Catholic cantons. VOL. II. X Mixed Catholics and Frotestants. K K 494 SWirZEELAXr. their representatives. The legislative powers are vested in the people and their representatives, and measures of paramount importance must be referred to the voters, without whose approbation they cannot pass into laws. Every citizen may propose a law, and if he can obtain the support of one- thirteenth of the electors of his eaaton he mav take the opinion of the cantonal authorities upon it. In this macnsr the whole of Switzerland has been converted into a huge parliament, of which every Swiss citizen is a member. The central authority, up to l&i8, was exercised by the Tagsatzung, or Diet, which alternately sat at Zurich, Luzem, and Bern. Each canton or half-canton was represented bv a Delegate, compelled to vote in accordance with the instructions furnished by his constituency. The large and wealthy cantons had no more to sav than the small ones, and the half-cantons had virtually but a consultative vote, for by a legal fiction two half-votes were not considered to count as a fuU vote, and a bill was not considered to have been carried if 11 A votes had been recorded in its favour. The small cantons actually governed the country. These evils were put a stop to by the Constitution adopted on the 12th September, 1848, on the conclusion of the Separatist war, which converted a loose federation of sovereign cantons into a Federal state. In virtue of this Federal pact, amended in a spirit of centralization in 1874, no canton is permitted to form political alliances with other cantons or with foreign states. All sovereign powf rs have been delegated to the Xational Assembly. It alone can conclude treaties or declare war ; the military forces, towards which each canton contributes a contingent, only obey its orders ; it coins money and superintends weights and measures ; it carries on the postal and telegraph services, and levies the customs duties. The Federation likewise watches over the rights and pri^-ileges of the citizens, and interferes whenever a canton attempts to violate the law. Religious liberty is guaranteed, and elementary education throughout Switzerland is to be compulsory, secular, and gratuitous. If 30,000 citizens or ei»ht cantons require it, each bill carried by the National Assembly must be submitted to a popular vote. This is called a Referendum. Bern has been chosen capital of the country, and is the seat of the Jfational Assembly, or Bundes-Versammlung, which consists of two chambers. The State Council fStanderath) is composed of forty-four members, chosen by the cantons and half-cantons, the former being represented by two, the latter by one member. The National Council (Xationalrath) consists of 135 representatives of the people, chosen in direct election at the rate of one deputy for every 20,000 souls. A general election of representatives takes place every three years. Every citizen of the Republic who has attained the age of twentj- years is entitled to a vote ; and any voter, not being a clergyman, may be elected a deputy. The chief executive authority is deputed to a Bundesrath, or Federal Council, consisting of seven members, elected for three years by the Federal Assembly. The President and Vice- President of the Federal Coimcil are the first magistrates of the Republic. Both GOVERNMENT A.\l> AHMIXISTRATIOX. 495 are elected liy tbo Federal Assembly for the term of one year, and are not re-eligible till after the expiration of another year. The seven members of the Federal Council— each of whom has a salary of X'480 per annum, while the President has t'.j40 — act as ministers or chiefs of the seven administrative depart- ments of the llepublie. The eleven members of the Federal Tribunal are elected for six years by the Federal Assembly. It decides on all matters in dispute between the cantons, or between cantons and the central Government, and acts in general as a High Court of Appeal. Its seat is Lausiinne. The constitution of 1874 abolished corporal punishment and the penalty of death, and transferred all legislation on commercial matters and copyright to the National Assembly. There is no standing army, but all citizens are called upon to render military service between the ages of twenty and forty-four, or to pay an exemption-tax should they be physically unfit. The BtiiHlcs-Auszitg (field force, absurdly called elile in the French cantons) consists of all men up to thirty-two, and each canton is required to furnish a force equal to at least 3 per cent, of its population, and in addition a reserve of half that strength. The Landwchr (militia) includes all men who have passed through the Auszug. Most of the expenses connected witli the army are borne by the Federation.* The cantons le\-y the recruits, appoint the officers, and carry on tlie adminis- tration of their contingents. The Federal authorities furnish the instructors, and exercise a general control. All legislation on militarj' matters emanates from them. The army, though not a standing one, nevertheless weighs hea%-ily upon the Federal and cantonal budgets, and a deficit has become almost chronic since the middle of the present century. The first Federal loan was contracted in 1867, and fresh loans will have to be contracted in future every year unless the cantons are called upon to cover the deficiency in the public revenue. This, however would be a dangerous experiment, for most of the cantons raise their revenues by direct taxes, and would resent any increase of the heavy burden they are obliged to bear even now. The Federal revenue is derived chiefly from customs, for the Post and Telegraph Offices yield but a small surplus. A portion of the revenue is • Federal army (December, 1876) : — Acszio. Staff Infantry, 107 battalions Cavalry, 24 squadrons and 12 troops Artillery, CD batteries and train . Engineers. 8 battalions Hospital Corps .... Administrations .... Permanent Instructorb Each man undergoes six to eight weeks' setting-up drill, and as long as he remains in the Auszug he annually attends a week's or a fortnight's training, according to tbe branch of the army to wliich he belongs. Lamiwehb. 620 Stuff .... HO 98,188 107 battalions 81,617 2,046 24 squadrons and 12 troops 2,279 1.5,530 23 batteries and train 7,421 2,2S5 8 battalions 1,484 8S7 — 292 604 187 — 12{>.fi:Jo 93,515 496 SWITZEELAND. paid over to the cantons. These latter derive their chief revenue from a property tax of one and a half per miUe.* * Eevenue and expenditure of the Confederation : — 1S74 1875 1876 1878 Revenue. £1,873,792 1, .580,640 1,659,496 1,642,600 Expenditure. £991,295 1,570,640 1,704,880 1,684,920 The military expenditure amounted to £580,239 in 1876, as compared with £127,439 in 1872. The public dcht of the Eepuhlic amounts to £1,170,000. As a set-off against the debt there exists a so-called " Federal fortune," including lauded property and invested capital. It is valued at £1,271.33.', hut only yielded £11,736 in 1876. The cantonal debts probably amount to £400,000. Taxation, inclusive of what is levied by the cantons, is sufficiently onerous to excuse a great amount of grumhUng. INDEX. Aar, 427, 429, 430 Aar, Canal of the, 465 Aargiiu, 466 Abbc\-iUe, 334 Abizc, lU Adour, 4o AJiiln, 406 AgJe, 118 Agdc, Capd", 110 Agen, 67 Agiiillon, 67 A him, 200 Aigueperso, 196 Aigucs-Mortts, 103, 121 Aiguillier, 182 Aiguillon, 218 Ain, loO, 133 Ain DeiMirtment, 157, 3S6 Airo, 68, 337 Aisne Department, 310, 389 Aix, 127 Aixe, 200 Aix-les-liains, 145 Ajol, Valley of, 353 Alais, 120 Albcres, 23 Albert, 332 Albertrille, 145 Albi, 192 Albigeois, 191 Albula, 431 Aldorney, 209 AJpn(;on, 275 Al.-sia, 162, 167 Alet, 115 Al.tsch Glacier, 400, 422 Allaasac, 198 AUevard, 142 AUier, 201, 223 AUier Department, 201, 38 Alprs-5Iaritime8, 134 Alpilli-8, 77 Alps, French, 78 Alturf, 469 AlUtatten, 472 Amberieu, 157 Ambert, 197 AmbletcoBC, 336 Amboise, 236 Amiens, 332 Amplepui*, 173 Ancenis, 243 VOL. II. AndelvB, 315 Andoiinatt, 393 Androzieux, 204 Andiize, 120 Angers, 239 Angouleme, 212, 213 Anianc, 1 1 8 Aniche, 339 Anneey, 140 Annocy, Lake of, 90 Annonav, 124 Antibes," 134 Autifer, 290 Appcnzell, 473 Aps, 123 Apt, 139 Aran, 31 Arbois, 159 Arbreale, 173 Are, 77 Arc, Pont d", 96 Areachon, 42, 72 Arcis-sur-Aubc, 291 Arcueil, 307 Ardk-he, 95 Arddche Department, 122, 385 Ardennes, 349 Ardennes Department, 350, 390 Ardres 337 Argeles, Glacier of, 36 Argens, 107, 130 Argcntan, 276 Argentat, 197 Argentcuil, SCO Argenton, 233 ArgoWe, 467 Ariegp, 55 Arlanc, 197 Aries, 63, 128 Annagnac, 65 Armentiires-sur-Lys, 340 Armissan, 117 Arques, 321 Arras, 337 AiTeau, 60 Ar8-en-R6, 217 Arve, 88, 90 Asnieres, 307 Aspc, 02 Aspres, 53 Attigny, 352 Aubapie, 127 L I, Aubo, 281 Aube Department, 291, 388 Aubcnas, 122 Aubirvilliers, 307 Aubin, 191 Aubusson, 200 Aiuli, 65 Aude, 27, 28, 106, 115 Aude Department, 115, 38A Audineourt, 160 Angst. 407 Amnale, 321 Aunic, 210 Auray, 258 Aure, 00 Aun-. Kiver, 273 Aurillac, 194 Auriol, 127 Auterive, 58 Authion, 224 Autnn, 169 Auvergne, 181 Auxerre, 290 Auxonne, 165 Avallon, 290 Aveuches, 458 Aventicum, 458 Avcsnes, 337 AvcjTon, 06 AvcjTon Department, 190, 3S8 A^Hgnon, 137 Arize, 294 A\Tanches, 275 Ax, 55 Axenstrassc, 470 Ay, 294 Azincourt, 334 Baccarat, 354 Baden, 4GS Bagneres-de-Bigorre, 60 Bagneres-de-Luchon, .'36, 67 BagiioUes, 276 Bagniils-8nr-C(^zc, 121 Bailleul, 342 Balanic, 119 Bfile, 465 Banduls, 131 Baiai836 RoiiKs6, 134, 136, IJT Bajiaume, 3:)7 Barbttste, 67 Barbczieux, MH 498 INDEX. Barcelonnette, 140 Bareges, 02 Barfleiir, 274 Bar-le-Duc, 350 Bar-sur-Aube, 291 Bar-sur-Seine, 291 ]5asel, 465 Basques in the Pj-renees, 37 Basses-Alpes, 140, 386 Basses-Pyrenees, 62, 384 Bussin, 276 Bastide, La, 193 Batz, 229, 231 Baume-los-Dames, 161 Baux, 129 Bavai, 338 Bayeux, 276 Bayonne, 63 Bazas, 09 Beam, 45, 62 Beaiicaire, 121, 122 Beauce, 233 Beaufort-en-Vallee, 239 Beaugency, 234 Beaujcu, 173 Beaujolais, 173, 188 Beaumont, 65 Beaune, 167 Beauregard, 235 Beauvais, 314 Bedarieux, 117 Begles, "2 Belfort, 162 Belpoeh, 115 BeUac, 200 BeUegarde, 53, ISl Belle^-iUc, 173 Belley, 157 Bellinzona, 453 Berck-sur-Mer, 331 Bcrgerac, 199 Bergues, 342 Bern, 461 Bern, Canton, 460 Bemay, 316 Bemina, 406 Berro, 112 Berthoud, 463 Besancjon, 161, 162 Besseges, 120 Bethune, 337 Bex, 454 Bezenet, 201 Beziers, 117 Biarritz, 64 Biel, 463 Bienne, 464 Bicnne, Lake of, 426 Bifevre, Plateau of, 94 BQlom, 197 Bize, 117 Blamont, 354 Blanc, 233 Blanquefort, 73 Blanzy, 170 Blaye, 73 Blois, 234 Blumlisalp, 401 Bocage, 276 Bodensee, 473 Boen, 205 Bohain, 311 BiUene, 139 Bonaguil, 67 Bonfol, 467 Bonneval, 86 Bonneville, 147 Bordeaux, 69, 70 Bom, Pays de, 41, 69 Bort, 197 Bosco in Ticino, 448 Bosmoreau, 200 Bouchcs-du-Rhone, 124, 385 Bougival, 308 Boulogne, 307, 335 Boulogne HiUs, 323 Bourbon-Lancy, 170 Bourbon-rArchambault, 204 Bourbonno-les-Bains, 291 Bom-bourg, 342 Bourg, 73, 157 Bourgancuf, 20O Bom-g-de-Peage, 142 Bourg-d'Oisans, 143 Bourges, 232 Bourget, Lake of, 91, 92 Boiirgoin, 144 Bourg St. Andeol, 123 Bourgueil, 237 Bouscat, Lc, 72 Boussac, 2Ul Bouxnnes, 342 Bouzigues, 119 Brantonie, 199 Brassac, 197 Bray, 287 Brehat, 202 Bresse, La, 353 Bressuire, 220 Brest, 200 Brctagne, 246 Breteuil, 316 Brian(;on, 139 Briare, 234 Brides, 145 Brie, 297 Brie-en-Comte, 298 Brieg, 454 Brienne, 291 Brienz, 464 Brieuz, Lake of, 427 Briev, 355 Brignolles, 133 Brigue, 451 Brionne, 316 Brioude, 190 Brittany, 246 Brive, 198 Brugg, 468 Brunnen, 470 Bugue, Lc, 199 Burgdorf, 463 Burgundy, 148 Bussang, 353 Bussy-le-Grand, 107 Buzan(;ais, 233 Cadillac, 69 Caen, 277 Cagots, 63 Cahors, 193 Calais, 336 Calanda, Mount, 404 Calas, 189 Caluirc, 172 Calvados Department, 276, 388 Camargue, 101 Cambrai, Ii38 Camembert, 276 Campan, 60 Cancale, 265 Canigou, 25 Cannes, 135, 138 Cantal, 181, 194, 386 Cap-Breton, 68 Capvern, 62 Carcanieres, 55 Carcassonne, 116 Carentan, 247 Carhaix, 261 Carignan, 351 Carlat, 194 CarUtte, 26, 28 Carmaux, 191 Caronte, 113 Carpentras, 138 Cassel, 342 Cassis, 127 Casteljaloux, 67 Castelmoron, 07 Castclnaudary, 115 Castel-Sarrasin, 05 Castets, 09 Castillon, 73 Castrcs, 193 Catcau-Cambresis, 338 Catogne, 410 Caudorun, 72 Caudi-y, 338 Caxines, 116 Caussade, 66 Causse of Mejean, 175, 176 Cauterots, 02 Caux, 288 Cavaillon, 138 Cayeux, 334 Cazaubon, 05 Cazeres, 68 Celts, 10 Cenis, Slont, 85 Cento Valli, 394 Cerdagne, La, 28 Ceiet, 63 Cerons, 09 Cette, 118 Cevennes, 174 Chabeuil, 142 Chablais, 146 Chagny, 108 Chaise-Dieu, 190 Chalabre, 115 Chalin, 162 ChaUes, 145 Chalonnes, 239 Chalons-sur-Mame, 293 Chalons-svir-Saone, 108 Chains, 200 Chamagne, 353 Chambery, 145 Chamboi^ 201 Chambon, Le, 204 Ch:imbord, 236 Chamonix, 87, 147 Champagne, 284 Champagney, 164 Champagnole, 159 Champtoce, 239 Channel Islands, 206 Channel Tunnel, 328 C'hantenav, 243 ChantiUyi 313, 314 Chantonnav, 221 Charente, 206, 207,213 Charonte Department, 212, 387 Charente- 1 nferieure, 214, 3i)7 Charenton, 307 Charite, 231 CharleviUe, 351 Charollais, 188 CharoUes, 170 Chartres, 235, 236 INDEX. 499 Chartrcuso, 143 Churtnusf, Unindo, 82, 87 Chuasirou, Muut, 415 Chati-aubriaut, 245 Chatcuu-Chinon, 232 0>ut«au-ilu-Loir, 241 Chatiaudua, 234 Oiatcau-CJontier, 242 ChaU'auneuf, 234 Chitoaunfuf-l£andon, 189 Cliateaurenault, 237 Chiteauroux, 233 Chatcau-'lTiiirry, 311 CbaU-Mon, 196 ChaU'lIerault, 219 Cliatillon, 167, 2o3 Chatix>. 233 Ojauffailli-s, 170 Cliauinont-en-Ua«ign_v, 292 Ckaunv, 312 Chaussado, La, 231 Cham-igny, 219 Chaux, lo'o Cliaux-di-Fonds, 460 Chavagruai', 194 ChazflU-s-sur-Lyon, -'05 Chenoncoaux, 236 Chtr Department, 232, 387 Chirbourjf. 273 Chessy-Us-XIints, 173 Chinon. 237 Choisv-leltoi, 307 Cholet, 239 • 'homdrac, 124 Chrishooa, 466 Chur, 471 Churfirsten, 405 CinteiraUlle, 58 Ciotat, 127 Cirev, 354 Ci\-rav, 218 Clairsic, 07 Cluirvaux, 159 Oaniecv. 232 Clermont, 195, 314, 350 Clennont-l'Hcxault, 118 Horv, 234 Clksun, 243 Cloves, 236 Clunv, 169 Clusis. 147 Coire, 471 Coiron, 122 CoUioure, 53 Combourg, 265 Commentry, 201 Comnienv, ^J50 Compi;-^e, 312, 314 Concamc-au, 259 Condc-8ur-Xoireau, 278 Condon, 65 Confolens, 212 Conftanz, Lake of, 432 Corbeil, 309 Corl.ie, 332 Corbiere--*, 29 C<.rde^ 192 Comouaille, 250 Correze Department, 197, 386 Cosne, 231 Costabona, 53 Cote-d'Dr, 104 Cotcntin, 246, 270 Cotos, 73 C'6tcs-du-\ord Department, 261, 388 CdUi St. Aadii, 143 Coition Alps. 78 Couehes-lcs-Minea, 169 Coulmiers, 234 Coulonimiers, 298 Couronne, La, 214 Coursan, 116 Coutanees, 274 Cninsae, 191 Cr.ion, 242 CVapponne's Canal, 99 Crjiu of Crapponne, 99 t'reev, 334 (.Vil, 314 Crest, 142 Creiise De[>artmont, 200, 386 Cn-usot, Le, 109 Croisie. 231, 245 Crussol, 124 Cuers, 132 Cuire, 172 Culoz, 91 Cusset, 202 Damctal, 318 Dauphinc, 80 Dax, 68 Deeazeville, 191, 192 Decizc, 231 Denain, 338 Dent du Midi, 396 Deols, 233 Devil's Bridge, 483 Di'voluv, 83 Diablerets, 402 Die, 14? Dieppe, 320 Dieu-le-Fit, 142 Digne, 140 Diifoin, 170 Dijun, 165 Dinan, 203 Disentis, 472 Dives, 279 Dol, 265 DGle, 1.59 Dol-er-Verchant, 15 Domlies, 156 Domfront, 276 Donmie, 199 Doniremv, 353 Douzv, 231 Dorat, 200 Durdogni', 187 Dordogne Department, 198, 386 Dure, Mont, 183 DoiLii, 339 Douamenez, 2C0 Doubs, 151, 154 Duubs at St. Ursannc, 4 1 2 Doiibs Department, 159, 380 Doue-la-Fontaine, 239 Doullens, 334 Dourdan, 309 Hover, .^trait of, 328 Drae, 92. 94 Draguignan, 133 Dranse, 423 Drf ux, J36 Drnme, 94 Drome Department, 111 Dunkirk, 343 Dun-le-Koi, 232 Durance, 97 Eauzc, 65 Kliene Fluh, 481 iCbreiiil, 202 Keluse, L", 90, 151 Kinsii-dUn, 470 Klbiuf, 317 Klne, 53 Kirilirun, 139 Knj,iidin, 406, 472 Kngliien, 309 Entlebueh, 468 Kntre-deux-Mere, 09 K|>emay, 294 KpiiiHo, 109 isjiinal. .•)62, 363 Knlns 226 I'.niir, 242 Kspalion, 191 Kspiuouze, 174, 176 Ivssonnc, 309 Kstngel, 66 Ktuin, 350 Etanipes, 309 Ktuples, 334 Ktretat, 318 Ku, 321 Kure Department, 314, 3S9 Eure-et-Loir, 236, 387 Evaux, 201 Evien, 147 Evreux, 316 Evron, 242 EjTiioutiers, 200 FasTies, 349 Falaiso, 279 FaueiiniV, 146 Faueiiles, 345 Faulhom, 401 Fa verges, 146 Feeamp, 319 Felletiu, 200 Felsberg, 404 Ffere-Champenoise, 294 Fernev, 157 Ferric-res, 298 Ferti- Bernard, 241 Ferte-.Macc, La, 276 Ferte sous- Jouarrc, 298 Feurs, 204 Fi;,'iac, 193 Finistire Department, 258, 388 Fimiiny, 204 I-leniings in Prance, 329 Fkrs, 276 neuranee, 65 Florae 189 Fuhn, 436 Foix, 55 Fontainebleau, 297, 298 FonUnav, 290 Fontenay-le-Comt«, 220 Fontenov-lc-Chiteau, 354 FonteWelle, 129 Fontcvrault. 239 Forcalquier, 140 Funst Cantons, 469 Fore/., 188 Forigny, 276 Fougeres, 205 FougiToUes, 164 Fouillouse, 204 Four Cantons, Ijiko of, 429, 468 Fourchambault, 231 Fourmies, 337 Fnintlu-Conitf', 14S Frjinqiii, 109 Fniii.'ufeld, 473 500 INDEX. Freiburg, 458 Froil, 123 Frcjua, 133 Frejus, Pass of, 85 French national character, 20 Fresnay-Ie-Vicomte, 241 Fresnoy-le-Grand, 314 Frevent, 334 Fribourg, 458, 459 Frontignan, 119 Fronton, 58 Frouard, 354 Fumay, 351 Funiei, 07 Fuveau, 127 GaiUac, 193 GaiUon, 315 Gallargues, 120 Ganges, 118 Gannat, 202 Gap. 140 Gard, 96, 98 Gard, Department of, 119, 385 Gardanne, 127 Garde-Freinet, 132 Gardon, 96 Garonne, 48, 71