■<;i>ffy LIBRA RY OF THE U N I VERSITY or 1 LLl NOI5 v2>IO -imw — ^m OF THE BULGAEIAXS. Christian f.c-T ViaJia . Christian Ir.dics from Skodra. llchammedans from Viddir. A native of Koyatepe. THE EARTH AND ITS INHABITANTS THE UNIVERSAL GEOGRAPHY Bv KLISEE RECLUS % XI EDITED Br E. G. RAVENSTEIN, F.R.G.S., F.S.S., Etc. ^ VOL. I. SOUTHERN EUROPE (GREECE, TURKEY IX EUROPE, RUMANIA, SERVIA. ITALY, SPALN AND PORTUGAL) ^ ^ ,^m 1 f'- ~^ ''"^K] w ^ ILLUSTRATED BY NUMEROUS ENGRAVINGS AND MAPS LONDON J. S. VIRTUE & CO., Limited, 294, CITY ROAD LONDON : PI1INT2D Bt J. 8. VIKTUK AND CO., LIMITED. CITY ROAD. CONTENTS. lo ■4 1 ^ TT r- HI. tv^lV V cJ c) c>~ I. TT, O Til O a? cJ. 1. . TT. .<1 III. (J IV. C V. cJ VI. .b- VII. rAGE I Intuoductoky Remahks EUROPE. Extent and Boixhaiues N.\TuitAL Divisions and Mountain.^ The SLvuiTiME Kecions . Climate Lmiaiutants THE lIEDITEKUAyEAN. Hyukology Anlmal Liie, F18HEU1ES, and Salt-i'ans CoMMEKtE AND NAVIGATION . GKEECE. Genehal Aspects . COXTINENTAL GkEECE The Mokea, ok Peloponnesus The Islands of the iEoEAN Sea . The Ionian Isles . The Phesent and Futl'ue of Gkeece . govhknment and political divisions . TURKEY IN EUROPE. General Aspects 87 C'UETE AND the IsLANKS OF THE AlUHI lEI.AGO TrKKEV OF THE GllEEKS (ThUACIA, JIalE llONIA, AND ThF.SSALv) AllCANIA AMI ICl'iUIS 90 ll.i V. The Illyrian Alps, Bosnia, and IIehze- OOVINA l'-f> VI. BlLGAUIA 131 A'll. Present Position and Pkospects of TlKKEY 145 VIII. G0VEUN.MENT AND Administuation . 150 RUMANIA 1.5.5 SERVIA AND MONTENEGRO . . 172 ITALY. I. Geneual Aspects 183 II. The Basin of the Po: Piemont, Lom- BAllDY, VeNETIA, AND EmILIA . . 189 HI. LlOUKIA AND THE RlVIEIlA OF GeNOA . '230 IV. Tuscany 239 V. The Roman Apennines, the Valley of the Tiheu, the Marches, and the Abruzzos 2-57 VI. Southepjj Italy : Naples . . . 28G VII. Sicily 309 VIII. Sardinia 338 IX. The Present and Future of Italy . 35'2 X. Government AND Administration . 358 V CORSICA 3G3 SP.UN. I. General A'^pects 370 II. The Castiles, I, eon, and Estremaduha 377 HI. ASDALISIA 391 CONTENTS. PAGE I IV. The Mediteueanean Slope : Murcia j AND Valencia 414 V. The Bale.iric Islands .... 423 I VI. The Valley of the Ebko : Akagon and Catalonia 427 VII. Basoue Provinces, Navakra, and Lo- GRoSo 439 VIII. Santander, the Asturias, and Galicia . 448 IX. The Present and Future of Spain . 460 X. Government and Administration . 465 PORTUGAL. I. General Aspects ..... 469 II. Northern Portugal .... 473 III. The Valley of the Tagus . . . 482 IV. Southern Portugal .... 490 V. The Present and Fut'.re of Portugal 496 VI. Government and Administration . 498 INDEX 501 LIST OF ILLUSTPvATIOXS. MArS PEIXTED IX COLOUES. 1. Ethnographical Map of Europe . .18 2. Turkty-in-Eiuxppc and Greece . . .85 3. The Bosjihurus and Constantinople . 98 4. Ethnographical Map of Turkey . .148 P.«08 5. luUy 183 6. The Delta of the Po 210 7. The Bay of Xaples 288 8. Spain and Portugal 385 PLATES. Peasants from the En\-irons of Athens Tufact pagi 53 Const;intinople and the Golden Horn, from the Heights of E>-ub 99 i AlUuiians 118 Wi;Jthy .\mauts 124 Turkish Muleteers in the Uerzegorina . . 127 Tirnova 133 Bulg^irians 1 38 JIussuhiuui of Adrianople, and Mussulman Lady | of I'riiirend 147 ' Wallachians (Valakhs) 162 I Belgrade 174 Tlic Pennine Alps, as seen from the Becca di Nona (Pic Carrel), 10,380 feet . . 195 i Venice 207 ' The Palace at Fcrrara ... . 228 Verona 229 Peaijunts of the Abruzzos 2.58 Xaples Tofaeepaijc 300 Capri, seen from Massa Luliixns^^^ . . . 302 Amalfi 304 La Valetta, M:Uta 337 Peasants of Toledo, OistUe . .390 Roman Bridge at Alcantara .391 Gorge de los Gaitanes, Detilc of Guadiilhorce . 399 Peas;ints of Cordova, And:ilusia .... 406 Gibraltar, as seen from the " Lines " . . .414 Peasants of La Hucrta, and Cigarrera of Valen- cia 419 Women of Ibiza, Balc;iric Isles . . .425 Monserrat, Catalonia . . . . .431 Barcelona, seen from the Castle of Monjuich . 437 Gorges of Pancoibo ...... 440 Los Pas.'.g« 447 Oporto 478 Lisbon 4S4 LIST OF ILLUSTKATIONS. ILLUSTEATIONS IN TEXT. EUROPE. 1. The Natural Boundary of Europe . . 7 2. The Relief of Eui-ope 8 3. Development of Coast-lines relatively to Area 11 4. The Isothermal Zone of Europe . . .17 THE MEDITERRANEAN. 5. The Depth of the Mediterranean . . 24 6. The Strait of Gibraltar . . . .26 7. Principal Fisheries of the Mediterranean . 30 8. Ste:imer Routes and Telegraphs . . .34 GREECE. Matnote and Svahtan . . . .42 Foreign Elements in the Population of Greece -14 Mount Parnassus anu Delphi . .46 Lower Acarnania 49 Thermopylaj 50 Lake Copais ...... 52 The Acropolis or Athens . . .54 Athens and its Long Walls . . .55 Ancient Athens 56 Mount Taygetvs 58 Lakes Phenoa and Stymphalus . . .60 The Plateau of Mantinea . . . .62 Bifurcation of the Gastuni . . . .63 The Valley of the Eurotas .... 67 Euripus and Chalcis 70 Nea Kaimeni ...... 72 Corfu 76 The Channel of Santa JIaura . . .77 Argostoli 79 TURlvEY IN EUROPE. The Gokge of Hagio Rumeli . . .91 Ci-ete, or Candia . . . . .93 The JEgenn Sea 95 Geological Map of the Peninsula of Con- stantinople 99 The HelK'spont, or Dardanelles . . . 105 Mount Athos 108 Mount Olympus HO Mount 01)-mpus and the Valley of Tempo 111 Southern Epirus 117 Suhterranean Beds of the Affluents of the Narenta 128 Mount Vitosh 132 39. Delta of the Danube 137 40. Comparative Discharge of the Mouths of the Danube 138 41. Commercial Highways converging upon Constantinople . . . . .150 42. The Turkish Empire 151 RUMANIA. 43. The Rumanians . 44. The Rivers Shil and Olto . 45. The Danube and Yalomitza 156 158 161 4C. Ethnological Map of MoldaWan Bessarabia 164 47. Bucharest 169 SERVIA jVND MONTENEGRO. 48. Confluence of the Danube and Save . .174 49. Montenegro and the Lake of Skodi-a . . 180 ITALY. 50. Rome and the Roman Empire . . . 186 .51. Monte Viso 189 52. Grand Paradis 191 53. Plain of Debris between the Alps and Apennines . . . . . .192 54. Slope of the VaUey of the Po . . . 193 55. Mud Volcanoes of the Northern Apennines 194 56. Ancient Glaciers of the Alps . .195 57. Serra of Ivrea and Ancient Glacier Lakes of the Dora 196 58. Ancient Lakes of Verbano .... 197 59. Lake Como 198 60—62. Sections of Lake Como . . .199 63. Villa Seubelloni 201 64. Beech and Pine "Woods of Ravenna . . 203 65. Shingle Beds of the Tagliamento, &c. . 205 66. Old Bed of the Piave 206 67. Lagoons of Venice 207 68. Colonies of the Roman Veterans . . 209 69. The Po between Piaeenza and Cremona . 211 70. German Conununes of Northern Italy . 216 71. Monte Rosa 217 72. The Lagoons of Comacchio . . . 220 73. The Fisheries of Comacchio . . . 221 74. Mouth of the Adige Valley . . .223 75. The Passages over the Alps . . . 224 76. ITie Lakes and Canals of Mantua • .227 77. Palmanova 229 78. Junction of the Alps and Apennines . . 231 79. Genoa and its Suburbs .... 234 80. Genoa 235 LIST OF ILLUSTRilTIONS. Slope 81. The Gulf of Siwzia . 82. The Golfolino of the Au\o 83. Defiles of the .iVrno . 84. Monte Argentaro 85. Val di Chiana . 86. The Lake of Bientina 87. The Malarial Kegions 88. Flouenxe .... 89. The Uarbour of Leghorn . 90. The Lake of Bolsona . 91. La Montagna d'Albano 9'2. Ancient Lake of Fucino 93. Lake of Trasiineno . 94. C.iMP.lGXA OF ItOMB . 9-5. Pontine JLarshes 96. Ancient Lakes of the Tiber and Topino 97. Cascades of Terni . 93. The Delta of the Tiber 99. Peas.vsts of the Kcman Campagxa 100. Rome 101. The Hills of Rome . 102. Ci\-ita Vecchia .... 103. Valleys of Erosion on the Western of the Apennines . lot. Rimini and San Marino lOo. Monte Gargano .... 106. ^Vshes of the Campania 107. Ercption of Mount Vesuvius 108. Educational Map of Italy . 109. Pompeii ..... 110. The Marshes of Salpi 111. Harbour of Brindisi in 1871 112. Harbour of Taranto . 113. Strait of Messina 1 14. Profile of Mount Etna 115. Lava Stream of Catania 1 16. Subsidiary Cones of Mount Etna 117. The Maccalubas and Girgenti 118. Palermo akd Monte Pellegrixo 119. Trapani and Marsala 120. Sj-racuse 121. Temi'LE of Concord at Gibgenti 122. The Central Portion of the iEoIian Islands 123. The Mediterranean to the South of Sicily . 124. The Port of Malta . 125. The Sea to the South of Sardinia 126. Strait of Bonifacio 127. LaGiara . 128. District of Iglcsias 129. Cagliari . 130. Port of Terranova 131. Navigation of Italy 132. Commercial Routes of Itiily 133. Submarine Plateau between Coraic Tuscany PAOK . 237 . 240 . 241 . 243 . 244 . 245 . 247 . 252 . 255 , 260 261 263 264 265 267 269 270 271 272- 276 278 281 283 285 287 289 292 297 301 305 307 308 310 311 313 314 317 324 326 328 329 332 334 336 339 340 345 348 350 351 355 356 FIO. PAOB 134. Profile of the Road from Ajaccio to Bastia 305 ise. Bastia 368 SPAIN. 136. Table-lands of Iberian Peninsula . . 371 137. Dehesiis near Madi'id ..... 375 138. Density of Population .... 376 139. Profile of RjiUway from Bayonne to Cadiz 379 140. SieiTas de Gredos and dc Gata . . .380 141. Defile of tub Tajo . . . .382 142. Steppes of New Castile . . . .384 143. Salamanca 388 144. The Alcazar of Segovia . . . 389 145. Toledo 390 146. Madrid and its Environs . . . .392 147. Aranjuez 394 148. Basins of the Guadiana and 6uadalqui\-ir . 395 149. The Pass of Despenaperros . . . 396 150. The Sierra Nevada . . . .397 151. The Mouth of the Guadalquivir. . .399 152. The Steppes of Ecija 402 153. Zones of Vegetation on the Coast of Anda- lusia 403 154. The Mines of Iluelva 406 155. The Aliiambra 408 156. Cadiz and its Roadstead . . . .411 157. Gibraltar 413 158. Steppes of Miircia 416 159. The Palm Grove of Elche . . .418 IGO. The Palm Grove of Elche and the Iluertas ofOrihuela 419 161. Ruins of the Dyke above Lorca . . 420 162. Peasants op Murcia .... 421 163. The Harbour of Cartagena . . . 423 164. ITie Grao de Valencia . . . .424 165. The Balearic Islands 426 166. View of Ibiza 427 167. The Pytiuses 42S 168. Port Miihon 430 169. The Delta of the Ebro .... 435 170. The Steppes of Aragon .... 436 171. The Environs of Barcelona .440 172. The Sand-banks of Mataro . . .441 173. Andorra 443 174. Jaizquibel 445 175. Azcoitia and Azpeitia .... 447 176. The Environs of Bilbao .... 441 177. St. Sebastian 450 178. St. Sebastian 451 179. (iuctaria 452 180. Guernica 453 181. Pass of Reinosa 454 LIST OF ILLUSTRATIONS. 182. Penas do Europa 4oU 183. Ilias of La Corufia and Ferrol . . . 458 184. Santona and Santander . . . .40 185. Oviedo and Gijon 462 186. Tower of Hercules .... 463 187. Kia de Vigo 464 188. Railroads of the Iberian Peninsula . . 465 189. Foreign Commerce of the Iberian Peninsula 466 190. Diagram e.xhibiting the Extent of the Caa- tilian Language 467 PORTUGAL. 191. Rainfall of the Iberian Peninsula 192. Portuguese Types (Peasants) 193. The Valley of the Limia, or Lima 194. Dunes of A voire 195. Oporto and the Paiz do Vinho . 470 472 475 476 478 196. Sao Joiio da Foz and the Mouth of the Douro 480 197. COIMBRA 482 198. The Estuary of the Tejo (Tagus) . .483 199. Peniche and the Berlingiis . .485 200. Mouth of the Tejo 486 201. Zones of Vegetation in Portugal . . 488 202. Castle of Penka de Cintra . . . 489 203. Monastery of the Knights of Christ at Thomar 491 204. Estuary of the Sado 492 205. Serra de Monchique and Promontory of Sagres 493 206. Geology of Algarve 494 207. Faro and Ta^-ira 496 208. Geographical Extent of the Portuguese Language 497 209. Telegraph from Lisbon to Rio de Janeiro. 498 A UNIVEESAL GEOGEAPHY. IXTKODUCTOEY EEMAEKS* TR earth is but as an atom in space, a star amongst stars. Yet, to us \i-ho inhabit it, it is still without bounds, as it was in the time of our barbarian ancestors. Nor can we foresee the period when the ^ybole of its surface will be known to us. We have been taught I by astronomers and geodesists that our planet is a sphere flattened at the poles, and physical geographers and meteorologists have applied their powers of inductive reasoning to establish theories on the direction of the winds and ocean currents within the polar regions. But hitherto no explorer has succeeded in reaching the extremities of our earth, and no one can tell whether land or sea extends beyond those icy barriers which have frustrated our most determined efforts. Thanks to the struggles of indomitable seamen, the pride of our race, the area of the mysterious regions around the north pole has been reduced to something like the hundredth part of the earth's surface, but in the south there still remains an unknown region of such vast extent, that the moon, were she to drop upon our planet, might disappear within it without coming into contact with any part of the earth's surface already known to us. And the polar regions, which present so many natural obstacles to our explorers, are not the only portions of the earth not yet known to men of science. It may be Inmiiliating to our pride as men, but we feel constrained to admit that among the countries not j-et known to us there are some, accessible enough as far as natural obstacles are concerned, but closed against us by our fellow-mcu ! There are peoples in this world, dwelling in towns, obeying laws, and ha'i-ing customs comparatively polished, but who choose to live in seclusion, and are as little known to us as if they were the inhabitants of some other planet. Their frontiers are closed by war and its horrors, by the practice of slavery, by religious • Hou2eau, " Histotre du Sol de I'Europe." — Carl Eitter, Lags dcr HaupsUdle Europa'e." vol.. I. -. B 'Europa." — Kohl, "Die Googiaphjsche 2 INTEODUCTOEY EEMAEKS. fanaticism, and even commercial jealousy. "We have heard of some of these peoples by vague report, but there are others concerning whom we absolutely know nothing. And thus it happens that in this age of steam, of the printing press, of incessant and feverish activity, we still know nothing, or very little, of the centre of Africa, of a portion of Australia, of the interior of that fine and no doubt most fertile island of New Guinea, and of vast table-lauds in the centre of Asia. Nay, even the country which most men of learning love to look upon as the cradle of our Aryan ancestors is known to us but very imperfectly. As regards most covmtries which have been visited by travellers, and figure more or less correctly upon our maps, a great amount of further research is required before our knowledge of their geography can be called complete. Years wiU pass ere the erroneous and contradictory statements of our explorers con- cerning them have been set right. A prodigious amount of labour must be performed before their climate, their hydrography, their plants and animals, can be thoroughly known to us. Minute and S3'stematic researches have to be conducted to elucidate the slow changes in the aspects and physical phenomena of many countries. The greatest caution vdll have to be exercised in distinguishing between changes due to the spontaneous action of natural causes and those brought about by the hand of man. And all this knowledge we must acquire before we can boast that we know the earth, and all about it ! Nor is this all. By a natural bent of our mind, all our studies are carried on with reference to Man as the centre of all things. A knowledge of our planet is, therefore, imperfect as long as it is not joined to a knowledge of the various races of man which inhabit it. The earth which man treads is but imperfectly known, man himself even less so. The first origin of races is shrouded in absolute darkness, and the most learned disagree with reference to the descent, the amalgamation, the original seats, and migratory stages of most peoples and tribes. What do men owe to their surroundings ? What to the original seats of their ancestors, to inborn instincts of race, to a blending mth alien races, or to influences and traditions brought to bear upon them from beyond ? We hardly knowj and as yet only a few rays of light begin to penetrate this darkness. Unfortunately our erroneous views on many of these questions are not due solely to ignorance. Contending passions and instinctive national hatreds too frequently obscure our judgment, and we see man as he is not. The far-off' savages assume the shape of dim phantoms, and our near neighbours and rivals in the arts of civilisation appear repulsive and deformed of feature. If we would see them as they really are, we must get rid of all our prejudices, and of those feeUngs of contempt, hatred, and passion which still set nation against nation. Our fore- fathers, in their wisdom, said that the most difficult thing of all was to know one's self Surely a comprehensive study of manldnd is more difficult stiU. We are thus not in a position at present to furnish a complete account of the earth and its inhabitants. The accomplishment of this task we must leave to the future, when fellow-workers from aU quarters of the globe will meet to write the grand book embodying the sum of human knowledge. For the present an rXTEODUCTOUY KE5IAEKS. 8 indiA-idual author must rest content with giving a succinct account of the Earth, in which the space occupied by each country shall be proportionate to its impor- tance, and to the knowledge we possess with respect to it. It is natural, perhaps, that each nation should imagine that in such a description it ought to be accorded the foremost place. Every barbarous tribe, however small, imagines itself to occupy the very centre of the earth, and to be the most perfect representative of the human race. Its language never fails to bear witness to this naive illusion, born of the very narrowness of its horizon. The river which irrigates its fields is called the "Father of Waters," the mountain which shelters its camp the "Navel," or "Centre of the Earth;" and the names by which primitive races designate their neighbours are terms of contempt, for thej- look down upon them as their inferiors. To them they are "mute," "deaf," "unclean," "imbecile," "monstrous," or "demoniac." The Chinese, one of the most remarkable peojjles in some respects, and certainly the most important of all as far as mere numbers go, are not content with having bestowed upon their country the epithet of " Flower of the Centre," but are so fully convinced of its superiority as to have fallen into the mistake (very excusable under the circum- stances) of deeming themselves to be the " Sons of Heaven." As to the nations thinly scattered around the borders of their " Celestial Empii'e," they know them merely as "dogs," "swine," "demons," and "savages." Or, more disdainful still, they designate them by the four cardinal points of the compass, and speak of the "unclean" tribes of the west, the north, the east, and the south. If in our description of the Earth we accord the first place to civilised Europe, it is not because of a prejudice similar to that of the Chinese. No ! this place belongs to Europe as a matter of right. Europe as yet is the only continent the whole of whose surface has been scientifically explored. It possesses a map approximately correct, and its material resources are almost fully known to us. Its population is not as dense as that of India or of China, but it nevertheless contains about one-fourth of the total population of the globe ; and its inhabitants, whatever their failings and vices, or their state of barbarism in some respects, still impel the rest of mankind as regards material and mental progress. Europe, for twenty-five centuries, has been the focus whence radiated Ai'ts, Sciences, and Thought. Nor have those hardy colonists who carried their European languages and customs beyond the sea succeeded hitherto in giving to the New World an importance equal to that of "little" Europe, in spite of the virgin soil and vast area which gave them scope for unlimited expansion. Our American rivals may be more active and enterprising than we are — they certainly are not cumbered to the same extent by the traditions and inheritances of feudal times — but they are as yet not sufiiciently numerous to compete with us as regards the totality of work done. They have scarcely been able hitherto to ascertain the material resources of the country in which they have made their home. " Old Europe," where every clod of earth has its history, where every man is the heir of a hundred successive generations, therefore still maintains the fii-st place, and a comparative study of nations justifies us in the belief that its moral B 2 4 lM'x>ULiUCruKY REMARKS. ' ascendancy and industrial preponderance will remain with it for many years to come. At the same time, we must not shut our eyes to the fact that equality wUl obtain in the end, not only between America and Europe, but also between these two and the other quarters of the world. The intermingling of nations, migrations which have assumed prodigious proportions, and the increasing facilities of intercourse must in the end lead to an equilibriiun of population being established throughout the world. Then wUl each country add its proper share to the wealth of mankind, and what we caU civilisation will have "its centre everywhere, its periphery nowhere."' The central geographical position of Europe has undoubtedly exercised a most favourable influence upon the progress of the nations inhabiting it. The superiority of the Europeans is certainly not due to the inherent virtues of the races from which they sprang, as is vainly imagined by some, for in other parts of the ancient world these same races have exhibited far less creative genius. To the happy conditions of soil, climate, configuration, and geographical position the inhabitants of Europe owe the honour of halving been the first to obtain a knowledge of the earth in its entirety, and to have remained for so long a period at the head of mankind. Historical geographers are, therefore, right when they insist upon the influence which the configuration of a country exercises upon the nations who inhabit it. The extent of table-lands, the heights of mountain ranges, the direction and volume of rivers, the vicinity of the ocean, the indenta- tion of the coast-Hne, the temperature of the air, the abundance or rarity of rain, and the correlations between soil, air, and water — all these are pregnant with effects, and explain much of the character and mode of life of primitive nations. They accoimt for most of the contrasts existing between nations subject to different conditions, and point out the natural highways of the globe which nations are constrained to foUow in their migrations or warlike expeditions. At the same time, we must bear in mind that the influence exercised upon the history of mankind by the general configuration of land and sea, or any special features of the former, is subject to change, and depends essentially upon the stage of culture at which nations have arrived. Geography, strictly speaking, confines itself to a description of the earth's surface, and exhibits the various nations in a passive attitude as it were, whilst Historical Geography and statistics show man engaged in the struggle for existence, and striving to obtaia the mastery over his surroundings. A river, which to an uncultured tribe would constitute an insurmountable barrier, becomes a commercial high-road to a tribe further advanced m culture, and in process of time it may be converted into a mere canal of irrigation, the course of which is regulated by man. A mountain range frequented by shepherds and huntsmen, and forming a barrier between nations, may attract, m a more civilised epoch, the miner and the manufacturer, and in course of time wUl even cease to be an obstacle, as roads wiU traverse it in all directions. Many a creek of the sea, which afforded shelter of yore to the small vessels of our ancestors, IS deserted now, whilst the open bays, which vessels dreaded formerly, have been protected by enormous breakwaters, and have become the resort of our largest ships. INTEODTJCTORY EEMAEKS. 6 Innumerable changes such as these have been effected by man in all parts of the world, and they have revolutionised the correlations existing between man and the land he lives in. The configuration and height of mountains and table-lands, the indentation of the coasts, the dispo>;ition of islands and archipelagos, and the extent of the ocean — these all lose their relative influence upon the history of nations in proijortion as the latter emancipate themselves and become free agents. Though subject to the condition of his dwelling-place, man may modify it to suit his own purpose ; he may overcome nature as it were, and convert the energies of the earth into domesticated forces. As an instance we may point to the elevated table-lands of Central Asia, which now separate the countries and peninsulas surrounding them, but which, when they shall have become the seats of human industry, will convert Asia into a real geographical unit, which at present it is only in appearance. Massy and ponderous Africa, monotonous Australia, and Southern America with its forests and waterfalls, will be put on something like an equality ■with Europe, whenever roads of commerce shall cross them in all directions, bridging their rivers, and traversing their deserts and mountain ranges. The advantages, on the other hand, which Europe derives from its backbone of mountains, its radiating rivers, the contours of its coasts, and its generally well- balanced outline are not as great now as they were when man was dependent exclusively upon the resources furnished by nature. This gradual change in the historical importance of the configuration of the land is a fact of capital importance which must be borne in mind if we would understand the general geography of Europe. In studying space we must take account of another element of equal value — time. EUROPE. I. — Extent and Boundaries. HE dwellers on the eastern shores of the jrediterranean Sea mnst liave learnt, in the course of their first warlike and commercial expeditions, to distinguish between the great continents ; for within the nucleus of the ancient world Africa is attached to Asia by a narrov/ band of arid sand, and Europe separated from Asia Minor by seas and channels difficult to navigate on account of dangerous currents. The division of the known world into three distinct parts coidd not fail to impress itself upon the minds of those infant nations, and when the Greeks had attained a state of maturity, and historical records took the place of myths and oral traditions, the name of Europe had probably been transmitted through a long series of genera- tions. Herodotus naively admits that no mortal could ever hope to find out the true meaning of this name, bequeathed to us by our forefathers ; but this has not deterred our modern men of learning from attempting to explain it. Some amongst them consider that it was applied at first to Thrace with its "large plains," and subsequently extended to the whole of Europe ; others dei'ive it from one of the surnames of Zeus with the " large eyes," the ancient god of the Sun, specially charged with the protection of the continent. Some etymologists believe that Europe was designated thus by the Phoenicians, as being the country of " white men." We consider it, however, to be far more probable that its name originally meant simply "the West," as contrasted with Asia, "the East," or " country of the rising sun." It is thus 'that Italy first, and then Spain, bore the name of Hesperia ; that Western Africa received the name of El Maghreb from the Mohammedans, and the plains beyond the Mississippi became known in our own times as the " Far West." But, whatever may be the original meaning of its name, Europe, in all the myths of the ancients, is described as a Daughter of Asia. The Phoenicians were the first to explore the shores of Europe, and to bring its inhabitants into contact with those of the East. When the Daughter had become the superior of her EXTENT AND BOHSDAEIES. 7 Motber in civilisation, and Greek voyagers were following up the explorations begi'n by the mariners of Tyre, all the known countries to the north of tho Mediterranean were looked upon as dependencies of Europe, and that name, which was originally confined to the Thraco-Hellenic peninsula, was made to include, in course of time, Italy, Spain, the countries of the Gauls, and the hyperborean Fig. 1. — Thb Xatural Bousdart of Eubope. Sciile 1 : 21,9(»,00a >s^>-^ { r- ■ - r^^. The zone of depression extending from the Black Sea to tho Gulf of Obi is shaded. The darker sh.. to the north of the Caspian shows the area depressed below the level of the Mediterranean. oO 3Ijles. regions beyond the Alps and the Danube. Strabo, to whom were known already the most varied and fruitful portions of Europe, extends it eastward as far as the Palus ilax)tis and the Tanais.* • Modem Sea of Azof and Eirer Don. 8 EUEOPB. Since that epoch the limits between Europe and Asia have been shifted hy geographers still flirther to the east. They are, however, more or less con- ventional, for Europe, though bounded on three sides by the ocean, is in reality but a peninsula of Asia. At the same time, the contrasts between these two parts of the world fully justify scientific men in dividing them into two continental masses. But where is the true line of separation between them ? Map-makers generally adopt the political boundaries which it has pleased the Eussian Government to draw between its vast European and Asiatic territories, and others adopt the summits of the Ural Mountains and of the Caucasus as the boundary Fig. 2. — The Relief op Europe. According to Houzeau, Bcrghaus, Kiepcrt, Olsen, and others. Scale 1 : CO.OOO.OOn IM/Mrf vp toBoOteet abovx-Scd level ^BS^a tfss than CSOfcet in depUi . S29 Liad depress^ hehwltn^ of Utediterraneai^ E3Jij nsor. than liOO [rtt m depLh between the two continents ; and although, at the first glance, this delineation appears more reasonable than the former, it is in reality no less absurd. The two slopes of a mountain chain can never be assigned to different formations, and they are generally inhabited by men of the same race. The true line of sepa- ration between Europe and Asia does not consist of mountains at all, but, on the contrary, of a series of depressions, in former times covered by a channel of the sea which united the Mediterranean with the Arctic Ocean. The stejjpes of the Manych, between the Black Sea and the Caspian, and to the north of the Caucasus, are still covered in part with salt swamps. The Caspian itself, as well as Lake Aral and the other lakes which we meet with in the direction of the Gulf of Obi, are the remains of this ancient arm of the sea, and the intermediate regions still bear the traces of having been an ancient sea-bed. There can be no doubt that vast changes have taken place in the configuration NATUEAL DIVISIONS AND MOUNTAINS. 9 / of Europe, not only during more ancient geological periods, but also within comparatively recent times. "We have already seen that a vast arm of the sea formerlv separated Europe from Asia ; it is equally certain that there was a time when it was joined to Anatolia by an isthmus, which has since been converted into the Bosphorus of Constantinople ; Spain was joined to Africa until the waters of the Atlantic invaded the Mediterranean ; Sicily was probably connected with ilaiiritania ; and the British Islands once formed a portion of the mainland. The erosion of the sea, as well as upheavals and subsidences of land, has effected, and still effect, changes in the contours of our coasts. Numerous soundings in the seas washing Western Europe have revealed the existence of a submarine plateau, which, from a geological point of view, must be looked upon as forming an integral portion of our continent. Bounded by abyssal depths of thousands of iiithoms, and submerged one hundred fathoms at most below the waters of the ocean, this pedestal of France and the British Islands must be looked upon as the foimdation of an ancient continent, destroyed by the incessant action of the waves. If the shallow portions of the ocean, as well as those of the Mediterranean Sea, were to be added to Europe, its area would be increased to the extent of one-fourth, but it would lose, at the same time, that wealth in peninsulas which has secured to Europe its historical superiority over the other continents. If we supposed Europe to subside to the extent of one hundred fathoms, its area would be reduced to the compass of one-half. The ocean would again cover her low plains, most of which are ancient sea-beds, and there would remain above the waters merely a skeleton of plateaux and mountain ranges, far more extensively indented by bays and fringed by peninsulas than are the coasts existing at the present time. The whole of Western and Southern Europe would be converted into a huge island, separated by a wide arm of the sea from the plains of interior Eussia. From an historical as well as a geological point of view, this huge island is the true Europe. Eussia is not only half Asiatic on account of its extremes of temperature, and the aspect of its monotonous plains and interminable steppes, but' is likewise intimately linked with Asia as regards its inhabitants and its historical development. Russia can hardly be said to have belonged to Europe for more than a hundred years. It was in maritime and mountainous Exirope, with its islands, peninsulas, and valleys, its varied features and unexpected contrasts, that modem civilisation arose, the result of innumerable local civilisa- tions, happilv im^ited into a single current. And, as the rivers descending from the mount-ains cover the plains at their foot with fertile soU, so has the progress accomplished in this centre of enlightenment gradually spread over the other continents to the very extremities of the earth. II. — Natural Divisioxs axd MorxxAiNS. The Europe alluded to includes France, Germany, England, and the three Mediterranean peninsulas, and constitutes several natural divisions. The British Islands form one of these. The Iberian peninsula is separated scarcely less 10 EUEOPB. distinctly from the remainder of Europe, for between it and France rises a most formidable range of mountains, the most difficult to cross in all Europe ; and immediately to the north of it a depression, nowhere exceeding a height of 650 feet, extends from the Mediterranean to the Atlantic Ocean. The geographical imity of Europe is represented to the full extent only in the S3'stem of the Alps, and in the mountains of France, Germany, Italy, and the Balkan peninsula which are connected with it. It is there we must seek the framework of continental Europe. The Alps, whose ancient Celtic name probably refers to the whiteness of their snowy summits, stretch in an immense curve, more than 600 miles in length, from the shores of the Mediterranean to the plains of the Danube. Thej' consist in reality of more than thirty mountain masses, representing as many geological groups, and joined to each other by elevated passes ; but their rocks, whether they be granite, slate, sandstone, or limestone, form one continuous rampart rising above the plains. In former ages the Alps were higher than they are now. This is proved by an examination of their detritus and of the strata disintegrated by natural agencies. But, whatever the extent of detrition, they still rise in hundreds of summits beyond the line of perennial snow, and vast rivers of ice descend from them into every upland valley. Looked at from the plains of Piedmont and Lombardy, these glaciers and snow-fields present the appearance of sparkling diadems encircling the mountain svunmits. In the eastern portion of the Alpine system — that is to say, between the Mediterranean and Mont Blanc, the culminating point of Europe — the average height of the mountain groups gradually increases from 6,500 to more than 13,000 feet. To the east of Mont Blanc the Alps change in direction, and, beyond the vast citadels represented by Monte Rosa and the Bernese Oberland, they gradually decrease in height. To the east of Switzerland no summit exceeds a height of 13,000 feet, but this loss in elevation is fully made up by increase of breadth. And whilst the general direction of the principal axis of the Alps remains north-easterly, very considerable mountain chains, far exceeding the central mass in breadth, are thrown off towards the north, the east, and the south-east. A line drawn across the true Alps from Vienna has a length of no less than 250 miles. In thus spreading out, the Alps lose their character and aspect. "We no longer meet with grand mountain masses, glaciers, and snow-fields. Towards the north they gradually sink down into the valley of the Danube ; towards the south they branch out into secondary chains, resting upon the arched plateau of Turkey. But, in spite of the vast contrasts ofiered by the true Alps and the moimtains of Montenegro, the Hfemus, the Rhodope, and the Pindus, all these mountain chains nevertheless belong to the same orographical system. The whole of the Balkan peninsula must be looked upon as a natural dependency of the Alps ; and the same applies to Italy, for the chain of the Apennines is nothing but a continuation of the Maritime Alps, and we hardly know where to draw the line of separa- tion between them. The Carpathians, too, must be included among the NATUEAL DIVISIONS AND MOUNTAINS. 11 mountain chains forming part of the system of the Alps. They have been gradually separated from them through the continuous action of water, but there can be no doubt that, in former times, the semicircle of mountains known as the Little Carpathians, the Beskids, the Tatra, the Great Carpathians, and the Transyl- vanian Alps was joined, on the one hand, to the Austrian Alps, and on the other to spurs descending from the Balkan. The Danube has forced its waj' through these mountain ramparts, but the passages, or "gates," are narrow; they arc strewn with rocks, and commanded by what remains of the ancient partition ranges. The configuration of the Alps, and of the labyrinthine mountain ranges branching ofE from them towards the east, could not fail to exercise a most powerful influence upon the history of Europe and of the entire world. The only high-roads known to barbarians are those traced out by nature herself, and they were consequently able to penetrate into Europe only bj' sea, or through the vast plains of the north. Having penetrated to the westward of the Black Sea, their progress was first stopped by the lakes and difficult swamps of the Danubian valley ; and, when they had surmounted these obstacles, they found themselves face to face with a barrier of high mountains, whose intricate wooded valleys and declivities led up to the inaccessible regions of eternal snow. The Alps, the Balkan, and all the other advanced chains of the Alpine system constituted an advanced defensive barrier for "Western Europe, and the conquering nomad tribes who threw them- selves against it did so at the risk of destruction. Accustomed to the boundless horizon of the steppes, they did not venture to climb these steep hills — thev turned to the northward, where the vast plains of Germania enabled successive swarms of immigrants to spread over the countrj'with greater ease. And as to the invaders, whom blind rage of conquest impelled to engage in the defiles of these mountains, they found themselves caught as in a trap ; and this accounts for the varietj' of nations, and of fragments of nations, whose presence has converted the coimtries of the Danube into a sort of ethnological chaos. And as the debris carried along bj' the current is deposited in the eddy of a river, so were these fragments of nearly every nation of the East accumulated in raotlej' disorder in this comer of the continent. To the south of this great mountain barrier the migrations between Europe and Asia could take place only by sea — a high-road open to those nations alone who were sufficiently advanced in civilisation to have acquired the art of building ships. Whether pirates, merchants, or warriors, they had raised themselves long ago above a state of primitive barbarism, and even their voyages of conquest added something to the stock of human knowledge. Moreover, owing to the difficulties of navigation, they migrated only in small bodies. At whatever point thej' settled they came into contact with populations of a different race from their own, and this intercourse gave birth to a number of local civilisations, each bearing its own stamp, and nowhere did their influence preponderate. Every island of the Archipelago, and every valley of ancient Hellas, differed from its neighbours as regards social con- dition, dialect, and customs, but they all remained Greek, in spite of the Phoenician and other influences to which they had been subjected. It is thus owing to tho 12 EUEOPB. configuration of the mountain cuains and coast-lines that the civilisation which developed itself gradually in the ^lediterranean countries to the south of the Alps was, upon the whole, more spontaneous in its nature, and offered more variety and greater contrasts, than the civilisation of the far less advanced nations of the north, who were moving from place to place on vast plains. The wide range of the Alps and of their advanced chains thus separated two distinct worlds, in which historical development went on at a different rate. At the same time, the separation between the two slopes of the Alpine system was by no means complete. IN'owhere in the Alps do we meet with cold and uninhabited plateaux, as in the Andes and in Tibet, whose enormous extent forms almost insurmountable barriers. The Alpine masses are cut up everywhere into mountains and valleys, and the climate of the latter is sufficiently mild to enable man to exist in them. The mountaineers, who easily maintained their independence, owing to the protection extended to them by nature, first served as intermediaries between the peoples inhabiting the opposite lowlands. It was they who eflfected the rare exchanges of produce which took place between the North and South, and who opened the first commercial high-roads between the summits of the moun- tains. The direction of the valleys and the dee 3I3' cut mountain passes even then indicated the grand routes by which the Alps would be crossed, at a future period, for the purposes of commerce or of war. That portion of the Alps which lies between the mountain masses of Savoy and of the Mediterranean would natu- rally cease first to form an obstacle to military expeditions. The Alps there are of great height, it is true, but they are narrower than anywhere else ; besides which, the climate on the two opposite slopes is similar, and assimilates the mode of life and the customs of the people dwelling there. Far more formidable, as a natural barrier, are the Alps to the north-east of Mont Blanc, for they constitute a climatic boundary. The other mountain ranges play but a secondary or local part in the history of Europe, when we compare them with the Alps. Still, the influence which they have exercised upon the destiny of nations is no less evident. The table-lands and snow-fields of the Scandinavian Alps form a wall of separation between Norwegians and Swedes. The quadrangular mountain fort of Bohemia, in the centre of Europe, which shelters the Chechians, is almost entirely enclosed by Germans, and resembles an island fretted by the waves of the ocean. The hills of "Wales and of Scot- land have afforded a shelter to the Celtic race against the encroachments of Anglo-Saxons, Danes, and Normans. The Bretons, in France, are indebted to their rocks and landcs for the fact of their not having yet become wholly French ; whilst the table-land of Limousin, the hills of Auvergne, and the Cevennes con- stitute the principal cause of the striking contrast which still exists between the inhabitants of Northern and of Southern France. The Pyrenees, next to the Alps, constitute the most formidable obstacle to the march of nations in Europe ; they would have remained an insurmountable rampart down to our own time, were it not easy to pass round them by their extremities abutting upon the sea. THE MAUITIME KEGIONS. 18 III. — The Maritime Kegions. The valleys which radiate in all directions from the great central masses of the Alps are admirably adapted for imparting to almost the whole of Europe a remarkable unity, whilst they offer, at the same time, an extreme variety of aspects and of physical conditions. The Po, the Rhone, the Rhine, and the Danube traverse countries having the most diverse climates, and yet they have their sources in the same mountain region, and the fertilising alluvium which they deposit in their valleys results from the disintegration of the same rocks. Minor valleys cut up the slopes of the Alps and of their dependent chains, and carry towards the sea the waters of the moimtains and the triturated fragments of their rocks. Running waters are visible, wherever we cast our eyes. There are neither deserts, nor sterile plateaux, nor inland lakes and river basins such as we meet with in Africa and Asia. The rivers of Europe are not flooded as are those of certain portions of South America, which deluge half the country with water. On the contrary, in the scheme of her rivers Europe exhibits a certain degree of moderation which has favoured the work of the settler, and facilitated the rise of a local civilisation in each river basin. Moreover, although most rivers are suffi- ciently large to have retarded migration, they are not sufficiently so to have arrested it for any length of time. Even when roads and bridges did not exist, barbarian immigrants easily made their way from the shores of the Black Sea to those of the Atlantic. But Europe, in addition to the advantages due to its framework of mountains and the disposition of its river basins, enjoys the still greater advantage of possess- ing an indented coast-line. It is mainly the contours of its coasts which impart to Europe its double character of unity and diversitj', which distinguish it amongst continents. It is "one" because of its great central mass, and "diversified" because of its numerous peninsulas and dependent islands. It is an organism, if we may say so, resembling a huge body furnished with limbs. Strabo compared Eui'ope to a dragon. The geographers of the period of the revival of letters compared it to a crowned virgin, Spain being the head, France the heart, and England and Italy the hands, holding the sceptre and the orb. Russia, at that time hardly known, is made to do duty for the ample folds of the robe. The area of Europe is only half that of South America, and one-third of that of Africa, and yet the develoj)ment of its coast-lines is superior to that of the two continents taken together. In proportion to its area the coasts of Europe have twice the extent of those of South America, Australia, and Africa ; and although they are to a small extent inferior to those of North America, it must be borne in mind that the arctic coasts of the latter are ice-bound during the greater portion of the year. A glance at the subjoined diagrams will show that Europe, as compared with the two other continents washed by the Arctic Ocean, enjoys the immense advantage of possessing a coast-lino almost wholly available for purposes of navigation, whilst a large portion of the coasts of Asia and America is altogether useless to man. And not only does the sea penetrate into the very heart of 14 EUEOPE. temperate Europe, cutting it up into elongated peninsulas, but these peninsulas, too, are fringed with gulfs and miniature inland seas. The coasts of Greece, of Thessaly, and of Thrace are thus indented by bays and gulfs, penetrating far into the land; Italy and Spain likewise possess numerous bays and gulfs; and the peninsulas of Northern Europe, Jutland and Scandinavia, are cut up by the waters of the ocean into numerous secondary peninsulas. 3. — Development op Coast-lines iuslatively to Area. SOUTH AMERICA NORTH AMERICA Europe. 4,00.5,100 3,758,300 Asia. 17,308,400 15,966,000 18,600 17,610 1 : 2-5 34,110 28,200 1 : 2-5 Africa. 11,542,400 11,293,030 16,480 16,480 1 : 1-4 N. America. 9,376,850 7,973,700 S. America. 6,803,570 6,731,470 30,890 26,510 1 ; 31 16,390 10,390 1 : 1-8 2,934,500 10,570 14,400 1: 1-7 Total area, square miles . Mainland „ Development of coast-liue, miles Accessible coasts .... Ratio of the geometrical to the actual contour . . . The shaded circles I'cpresent the various continents ; the outer circle represents the actual extent of coast-line. The blank space between the two concentric cii-cles represents graphically the diflerence between the smallest possible or geometrical contour of a country having the area of the respective continents, and the actual contour as exhibited in the existing coast-lines. Europe, beiug in reality only a peninsula of Asia, hardly admits of this comparison. The islands of Europe must be looked upon as dependencies of that continent, for most of them are separated from it only by shallow seas. Candia and the islands scattered broadcast over the JEgean Sea, the Archipelagos of the Ionian Sea, and of Dalmatia, Sicily, Corsica and Sardinia, Elba, and the Baleares, are in reality but prolongations, or maritime out-stations, of neighbouring peninsulas. To the islands of Sealand and Fycn, at the entrance to the Baltic, Denmark owes THE JIAErrnTE EEGION. 15 most of her commercial and political importance. Great Britain and Ireland, wliich actually formed a portion of the European continent in a p;ist age, cannot be looked upon otherwise than as dependencies of it, although the isthmus which once joined them has been destroyed by the waters of the ocean. England has actuallv become the grand commercial emporiiun of Europe, and plays now the same part in the world's commerce that Greece once played in that of the more restricted world of the Mediterranean. It is a remarkable fact that each of the European peninsulas should hare enjoyed in turn a period of commercial preponderance. Greece, the " most noble individuality of the world of the ancients," came fii'st, and when at the height of her power governed the ilediterranean, which at that time meant nearly the whole imi verse. During the Middle Ages Amalfi, Genoa, and Venice became the com- mercial agents between Europe and the Indies. The discovery of a passage round the Cape and of America diverted the world's commerce to Cadiz, Seville, and Lisbon, on the Iberian peninsula. Subsequently the merchants of the small Dutch Republic seized a portion of the heritage of Spain and Portugal, and the wealth of the entire world was floated into the harbours of their sea-bound islands and peninsulas. In our own days Great Britain, thanks to its favourable geo- graphical position, in the very centre of great continental masses, and the energy of its people, has become the great mart of the world. London, the most populous city of the world, is also the great centre of attraction for the treasures of man- kind; but there can be no doubt that sooner or later it will be supplanted, in consequence of the opening of new commercial high-roads, and changes in the political preponderance of nations. Perhaps some city of the United States will fake the place of London ia a future age, and thus the American belief in the westward march of civilisation will be verified ; or we may possibly return to the East, and convert Constantinople or Caii'o into the world's emporium and centre of intercourse. But, whatever may happen in the future, the great changes which have taken place in the relative importance of the peninsulas and islands of Europe in the short span of twenty centuries, sufficiently prove that geographical features exercise a varying influence at different epochs. That which at one time was looked upon as a great natural advantage may become, in course of time, a serious disadvantage. Thus the numerous inlets and gulfs enclosed by mountain chains, which favoured the rise of the cities of Greece, and gave to Athens the dominion of the Mediterranean, now constitute as many obstacles to their connection with the existing system of European communications. That which in former times constituted the strength of the country has become its weakness. In primitive times, before man ventured upon the seas, these bays and gulfs formed insur- mountable obstacles to the migration of nations ; at a later date, when the art of navigation had been acquired, they became commercial high-roads, and were favourable to the development of civilisation ; and at the present time they are again obstacles in the way of oui- road-builders and railway engineers. 16 EUEOPE. IV. — Climate. The influence exercised by the relief of the land and the configuration of the coasts varies in different ages, but that of cliraate is ijermanent. In this respect Europe is the most favoured region of the earth, for during a cycle of unknown length it has enjoyed a climate at once the most temperate, the most equable, and the most healthy of all continents. Owing to the inland seas which penetrate far into the land, the whole of Europe is exposed to the modifying influence of the ocean. With the exception of Central Russia, no part of Europe is more than 400 miles from the sea, and, as most of the mountains slope from the centre of the continent towards its circum- ference, the influence of the sea breezes is felt throughout. And thus continental Europe, in spite of its great extent, enjoys the advantages of an insular climate throughout, the winds passing over the ocean moderating the heat of summer and tempering the cold of winter. The continuous north-easterly movement of the waters of the Atlantic likewise has a favourable effect upon the climate of Europe. After having been heated by a tropical sun in the Gulf of Mexico, the gulf-stream issues through the Strait of Florida, and, spreading over the Atlantic, takes its course towards the coasts of Europe. This enormous mass of warm water, equal in volume to twenty million rivers as large as the Rhone, brings the warmth of southern latitudes to the western and northern shores of Europe. Its influence is felt not only in the maritime countries of Western Europe, but to some extent as far as the Caspian and the Ural Mountains. The currents of the air exercise as favourable an influence upon the climate of Europe as do those of the ocean. The south-westerly winds predominating on the coasts pass over the warm gulf-stream, and, on reaching Europe, they part with the heat stored up by them between the tropics. The north-westerly, northerly, and even north-easterly winds, which blow during a portion of the year, are less cold than might be expected, for they, too, have to cross the warm waters of the gulf- stream. And lastly, there is the Sahara, which elevates the temperature of a portion of Europe. The increase in temperature due to the combined influence of winds and ocean currents amounts to 40°, 60°, and even 60°, if we compare Europe with other parts of the world lying under the same latitudes. Nowhere else, not even on the western coast of North America, do the isothermals, or lines of equal annual temperature, ascend so high towards the arctic regions. The inhabitants of Europe, though they may live 900 to 1,200 miles farther away from the equator, enjoy as mUd a climate as do those of America, and the decrease of temperature on going northward is far less rapid than in any other part of the globe. This uniformity of temperature constitutes one of the most characteristic features of Europe. The whole of it lies within the temperate region bounded by the isothermal lines of 32° F. and 68° F., whilst in America and Asia that privileged zone has only half this extent. CLIMATE. 17 This remarkable uniformity in the climate of Europe is exhibited not only in its temperature, but likewise in the distribution of its rains. The seas vrashiuj the shores of Europe supply all parts of it with the necessary amount of moisture. There is no rainless district, nor, with the exception of a portion of the maritime region of the Caspian and a small corner of Spain, anj' district where droughts occasionally entail the entire loss of the harvest. Eains full not only regularly every year, but in most countries they occur in every season, the only exception being the coimtries of the Mediterranean, where autumn and winter are the real rainy seasons. Moreover, in spite of the great diversity in the physical features of Europe, the amount of rain is scarcely anywhere excessive, whether it descends as a fine drizzle, as in Ireland, or in heavy showers, as in Provence and on the Fig. 4. — The Isotrebhal Zoke or Eubope. Scale 1 : 60,000,000. >U>65ofl. 6i<>lo3?8on. JiSo to 63«o fl. orrr 656o ft. southern slope of the Alps. The annual rainfall scarcely ever exceeds thirty-nine inches, except on the flanks of certain mountain ranges which aiTest the passage of currents charged with moisture. This uniformity and moderation in the rain- fall exercise a regulating influence upon the course of the rivers, for even the smallest amongst them, at all events those to the north of the Pyrenees, the Alps, and the Balkan, flow throughout the year. They rise and fall generally within narrow limits, and inundations on a vast scale are as rare as is want of water for purposes of irrigation. In consequence of this regularity, Europe is able to derive a greater advantage from its waters than other continents where the amount of precipitation is more considerable. The Alps contribute much towards main- VOL. I. c IS ETJEOPE. taining a regular flow of the rivers ; tie excess of humidity which falls to their share is stored up in the shape of snow and ice, which descend slowly into the Talleys, and melt during the heat of summer. This happens just at a time when the rivers gain least from rain, and lose most by evaporation, and some amongst tiem woidd drv up if the ice of the mountains did not come to the aid of the waters descending from the sky. It is thus that a sort of balance is established in the economy of European rivers. The climate of Europe is thus characterized by uniformity as a whole, and by a compensatoiT action in its contrasts. Regularity and freedom from excess, sucii as are not known in other continents, mark its ocean currents, its winds, its temperature and rains, and the course of its rivers. These great advantages have benefited its inhabitants in the past, and will not cease to do so in the future. Though small in extent, Europe possesses by far the largest area of acclimation. Man mav migrate from Russia to Spain, or from Ireland to Greece, without exposing himself to any great risk of life. The inhabitants of the Caucasus and the Urol Mountains were thus able to cross the plains and mountains of Europe, and to establish themselves on the shores of the Atlantic. Soil and climate are equally propitioiis to man, and enable him to preserve his physical and intellectual powers wherever he goes. A migratory people might found new homesteads in any part of Europe. Their companions of travel — the dog, the horse, and the ox — would not desert them on the road, and the seed-corn which they carry with them would yield a harvest wherever confided to the earth. T. IXHABITAXTS. A STTDT of the soil and a patient observation of climatic phenomena enable us to appreciate the general influence exercised by the nature of the country upon the development of its inhabitants ; but it is more diiBcult to assign to each race or nation its due share in the progress of European civilisation. !No doubt, in their struggles for existence, diflerent groups of naked and ignorant savages must have been acted upon difierently, according to their numbers and physical strength, their inborn intelligence, their tastes and mental tendencies. But who were those primitive men who first turned to account the natural resources of the country in which they dwelt ? We know not ; for, if we go back for a few thousand years, every fijct is shrouded in darkness. We know nothing even as regards the origin of the leading nations of Europe. Are we the " sons of the soil," and the " shoots of oak-trees," as told in the poetical language of ancient tradition, or are we to look upon the inhabitants of Asia as the ancestors to whom we are indebted for our languages, and for the rudiments of our arts and sciences ? Or did those inunigrants from a neighbouring continent settle down amongst an indigenous population? Xot many years ago the Asiatic origin of European nations was accepted as an established fact, and the original seats of our forefathers were pointed out upon the map of Asia, Rut now most men of science are agreed to ETHNOGRAPHICAL MAP F E~DHDP1 l^'.GBa^-euslem.FR G.S BASK. CATCASIAN' \ KAMITO-SE.\aTH: ■ TNDO-(;F.RMA^■K" t C? LIMITED ^: INTIABITANTS. 10 seek our ancestors upon the very soil ^vhich we, their descendants, still occupv. Caverns, the shores of oceans and lakes, and the alluvial beds of our rivers have yielded the remains of human industry, and even human skeletons, which clearly prove that long before these supposed immigrations from Asia there existed in Europe tribes who had alre;idy made some progress in human industry. Even in the childhood of history there existed tribes who were looked upon as aborigines, and some of their descendants — as, for instance, the Basks — have nothing in common with the invaders from the neighbouring continent. Nor is it universally admitted that the Aryans — that is, the ancestors of the Pelasgians, the Greeks, the Latins, Celts, Germans, and Slavs — are of Asiatic origin. Similarity of language niaj- justify our belief in the common origin of the Aryans of Europe, the Persians, and the Hindoos, but it does not prove that their ancestral home should be looked for somewhere near the sources of the Oxus. Many men of learning * look upon the Ajyans as aborigines of Europe, but certainty on this point does not exist. Xo doubt, in prehistoric times, intermigrations between the two continents were frequent ; but we hardly know what directions they took, and can speak with certainty only of those migrations of peoples which are related by history. Wo thus know that Europe sent forth to other continents Galatians, Macedonians, and Greeks, and more recently inniunerable emigrants of all nationalities, and received in turn Huns, Avares, Turks, Mongols, Circassians, Jews, Ai-menians, Moors, Berbers, and members of many other nations. Leaving out of consideration the smaller families of nations, as well as the members of races who have not attained a national existence, Europe may be described as consisting of three great ethnological divisions, the principal boundary between which is formed by the Alps, the Carpathians, and the Balkan. The first of these great families of European nations, the members of which speak Greco-Latin languages, occupies the southern slopes of the Balkan and of the Alps, the Iberian peninsula, France, and a portion of Belgivun, as well as a few detached territories within the limits of the ancient Eoman empire, altogether surrounded by alien nations. Such are the plains of the Lower Danube and a portion of Transylvania, which are inhabited by the Rumanians, and a few secluded Alpine valleys inhabited by " Romans." On the other hand, fragments of two ancient nations have maintained their ground in the midst of Latinised populations, viz. the Celtic inhabitants of Brittany, and the Basks of the Pyrenees. Generally speaking, however, all the inhabitants of South-western Eui-ope, whether of Celtic, Iberian, or Ligurian race, speak languages derived from the Latin, and whatever diffeieaces existed originally between these various populations, this community of language has more or less obliterated them. The Teutonic nations form the second great group. They occupy nearly the whole of Central Europe to the north of the Alps, and extend through Holland and Flanders to within a short distance of the Straits of Dover. Denmark and the great Scandinavian peninsula, as well as Iceland, belong to the same group, and • Latham, Beufey, Cuno, Spiegel, and others. c 2 20 EUEOPE. the bulk of the inhabitants of the British Islands are likewise generally included in it. The latter, however, should rather be described as a mixed race, for the aboriginal Celtic population of these islands, which now exists pure only in a few remote districts, has amalgamated -with Anglo-Saxon and Danish invaders, and the language of the latter has become mixed with meditcval French, the resulting idiom being almost as much Latin as Saxon. The development of national characteristics has been favoured by the isolation in which the inha- bitants of the British Islands found themselves, and they differ essentially from continental neighbours — the Scandinavians, Germans, and Cclto-Latins — in lan- guage and customs. The Slavs, or Slavonians, form the third group of European nations. They are less numerous than the Greco-Latins, but the territories they occupy are fiir more extensive, for they spread over nearly the whole of Russia, over Poland, a large portion of the Balkan peninsula, and about one-half of the Austro-Hungarian monarchy. All the great plains to the east of the Carpathians are inhabited by Slavs, either pure or mixed with Tartars and Mongols. To the west and south of the mountains the race is split up into numerous small nations, and in the valley of the Danube these come into contact with Rumanians, as well as with Turks and Magyars, the two latter being of Asiatic origin, and these separate the Slavonians of the north from the Slavonians of the south. In the north, Finns, Livonians, and Lithuanians interpose between the Slavonians and the Germanic nations.* Race and language, however, arc not always identical. Members of one race frequently speak the language of another, and race and linguistic boundaries, therefore, differ frequently. As for the political boundaries, they scarcely ever follow those natural features which would have been selected had their settlement been intrusted to the spontaneous action of the different nations. They hardly ever coincide with the boundaries of races or of languages, except in the case of a few high mountain ranges or of arms of the sea. On many occasions the countries of Europe were arbitrarily split up in consequence of wars or diplomatic arrange- ments. A few peoples only, protected by the nature of their country as well as Population of Europe, about 305,000,000 :— Greeo-Latin. Greeks . . . 2,600,000 Albanians 1,250,000 Italians . 27,700,000 French . 39,700,000 Spaniards and For tuguese 20,210,000 Rumanians . 8,400,000 Itliaetians ("Romans") 42,000 99,902,000 Finns Osmanli . Jilagyars . Tartars . Calmucks Gennanic. Germans . . 63,400,000 Dutch and Flemish 6,720,000 Scandinavians . 5,640,000 Anglo-Saxons . 30,600,000 96,360,000 4,700,000 Celts . 1,300,000 Basks 6,770,000 Letts, &c. 2,500,000 Armenians 100,000 Gipsies . Circassians Included above are 4,500,000 Jews. Slavonic, Russians Poles . Czechians, ciu. .Servians Slovenes Bulgarians . 59,000,000 11,800,000 6,750,000 5,750,000 1,200,000 3,100,000 87,600,000 1,600,000 700,000 2,900,000 280,000 690,000 400,000 INHABITANTS. 21 hv ihcir valour, have maintained tbcir independence since the age of great migra- tions, but many more have been swept away by successive invasions. Many others, again, have alternately seen their frontiers expand and contract more than onco even during a generation. The so-called " balance of European powers," founded as it is iipon the rights of war and ambitious rivalries between nations, is necessarily unstable. Nations eminently fit to lead a common political existence are torn asunder on the one side, whilst the most heterogeneous elements are thrown together on the other. In those political arrangements the nations themselves are never consulted, but their wishes and inclinations must nevertheless prevail in the end, and the artificial edifice raised by warriors and statesmen will come to the ground. A true " balauce of jjower " will only be established when every nation of the continent shall have become the arbiter of its own destinies, when every pretended right of conquest shall have been siirrendered, and neighbouring nations shall be at liberty to combine for the management of the afiuirs they have in common. Our arbitrarj- political divisions, therefore, possess but a transitory value. They cannot altogether be ignored ; but in the following descriptions we shall, as far as possible, adhere to the great natural divisions as defined by mountains and valle^-s, and by the distribution of nations having the same origin and speaking the same language. But even these natural boundaries lose their importance in countries like Switzerland, inhabited by nations speaking diS'erent languages, but held together by the strongest of all ties — the common enjoyment of freedom. From an historical point of view a description of Europe should commence with the maritime countries of the Mediterranean. It was Greece which gave birth to our European ci\'ilisation, and which at one time occupied the centre of tlie known world. Her poets first sang the praises of venturesome navigators, and her historians and philosophers collected and classified the information received with respect to foreign countries. In a subsequent age, Italy, in the very centre of the Mediterranean, took the place of Greece, and for fifteen centuries maintained herself therein : Genoa, Venice, and Florence succeeded Eome as the leaders of the civilised world. During that period the surrounding nations gravitated towards the Mediterranean and Italy ; and it was only when the Italians themselves enlarged the terrestrial sphere by the discovery of a new world beyond the ocean that this preponderance passed away from them, to remain for a short time with the Iberian peninsula. Greece had been the mediator between Europe and the ancient civilisations of Asia and Africa ; Spain and Portugal became the representatives of Europe in America and the extreme Orient ; historical develop- ment in its progress had followed the axis of the Mediterranean from east to west. It will be found natural, imder these circumstances, when we describe the three Mediterranean peninsulas in the same volume, particularly as they are peopled almost exclusively by Greco-Latin nations. France, though likewise Latinised, nevertheless occupies a distinct position. It is a Mediterranean country only as respects Provence and Langucdoc, the rest of its territory sloping towards the Atlantic. Its geographical position and history have made France the great 22 EUROPE. European thoroughfare iipon which the nations of the Mediterranean rnd of the Atlantic meet to exchange their products and to fight their battles. Ideas are imported into France from all parts of Europe, and she is called upon to act the part of an interpreter between the nations of the North and of the South. Next to France we shall describe the Germanic countries of Europe, the British Islands, and Scandinavia ; and lastly, the immense empire of Russia. THE MEDITERRANEAN. I. — Hydrology. TlEECE and its insular satellites prove sufficiently that the unstable floods of the IMediterranoan have exorcised a greater influence upon the march of history than did the solid land upon which man trod. Western civilisation would never have seen the light had not the waters of the Mediterranean washed the shores of Egypt, Phoenicia, Asia Minor, Hellas, Italy, Spain, and Carthage. The western nations would have remained in their primitive barbarism if it had not been for the Mediterranean, which joined Europe, Asia, and Africa ; facilitated the intercourse between Aryans, Semites, and Berbers ; and rendered more equable the climate of the surrounding countries, thus facilitating access to them. For ages it appeared almost as if man- kind could prosper only in the neighbourhood of this central sea, for beyond its basin only decaj'ed nations were to be met with, or tribes not yet awakened to mental activity. " Like frogs around a swamp, so have we settled down on the shores of this sea," said Plato ; and the sea he refers to is the Mediterranean, It is thereiore deserving of description quite as much as the inhabited countries which surround it. Unfortunately many mysteries still remain hidden beneath its waves. * From an examination of the coasts, as well as from tlic traditions of the people inhabiting them, we learn that the Mediterranean has varied frequently in its contours and extent. The straits which connect its waters with those of the ocean have frequently changed their position. At a time when peninsulas like Greece, and even islands like JIalta, formed part of continental masses — and that they did so in a comparatively "recent geological epoch is proved by their fossil fauna — the waters of the Mediterranean covered largo portions of Africa, of Southern Russia, and even of Asia. The researches of Spratt, Fuchs, and others have satisfactorily proved that towards the close of the miocene age a vast frcsh- • W- H. Smith, "The Jlediterranean." — Bureau de la Halle, "Geographie Physique do la Mcr Noire et de la Mediterranee." — Bottger, " Das Mittelmcer." 24 THE MEDITERRANEAN. water laks stretclied from the banks of the Aral, across Eussia, the plains of the Danube and the Archipelago, as far as Syracuse in Sicily. Then came the briny waters of the ocean. There was a time when the Black Sea and the Caspian connected the Archipelago with the Gulf of the Obi. At another epoch the gulfs of the Syrtes penetrated far inland, and a large portion of what is now the Libyan and Saharan desert was then covered with water. The Strait of Gibraltar, which was torn asunder by Hercules according to the traditions of the ancients, is in reality but of recent origin, and has taken the place of a more ancient strait which joined the Mediterranean to the Red Sea and Indian Ocean : this strait has been restored by human hands, and is known now as the Suez Canal. The coast-lines of the Mediterranean are undergoing perpetual change, owing to the upheaval or subsidence of the countries surrounding it. The Nile, the Po, the Rhone, and other rivers incessantly enlarge the alluvial plains at their mouths, and still further encroach upon the sea. Actually the Mediterranean, with its subordinate Fig. 5.- -The Depth of the Meditekbaxean. Fi-om a Chart by M. Delesse. seas from the Strait of Gibraltar to the Sea of Azof, covers an area about thirty times that of the British Islands. This area is small if we compare it with the immense development of the coasts and the wealth in peninsulas, which impart an aspect of life and independence to at least one-third of the ancient world. The Mediterranean, though it takes precedence of all the oceans, in consequence of the part it has played in history, nevertheless only covers an area one-seventieth that of the Pacific* It is broken up, moreover, into several separate seas, some of them so small in extent that the na\'igator hardly ever loses sight of the land. In the Area of the Mediterranean basin : — (Europe Africa : : : , Mediterranean Sea 683,500 square miles. 232,000 „ 1,737,500 „ 1,153,300 „ 3,806,300 nYDEOLOGY. 25 cast wc have the Bl:ick Sea, with its two dependencies, the Seas of Azof and of Sfarmara. The Aigean Sea, or Archipelago, with its numerous islands, extends between the deeply indented coasts of Greece, Asia Minor, and Crete. Tho Adriatic stretches towards tho north-west, between the Balkan peninsula and Italy ; and the Mediterranean proper is divided into two separate basins, which might appropriately bo called the riicrnician and Carthaginian Seas, or the Greek and Roman Mediterraneans. Each of these basins is again subdivided, tho one by Crete, tho other by tho two islands of Sardinia and Corsica. These various subdivisions of the Mediterranean differ in area, and still more in depth. The Sea of Azof almost deserves the name of " Swamp," which was bestowed upon it by the ancients, for if a ship sinks in it the masts remain visible above the water. The Black Sea has a maximum depth of over 1,000 fathoms, but the narrow strait which joins it to the Sea of Marmara is shallower than many a European river. The cavity filled by the Sea of Marmara is far inferior to that of many an inland lake ; and the Dardanelles, like tho Bosphorus, are hardly wider than a river. In the Archipelago and tho eastern basin of the Mediterranean proper the depth corresponds with the protuberance of the land. Abyssal dejjths and "pits" of 260 and even of 540 fathoms are to be found in close proximity to the scarped mountain islands of the Cyclades, whilst on the low coasts of Egj'pt the water deepens only gradually, until in the centre of the Levantine Sea it attains a depth of 1,750 fathoms. The maximum depth — 2,170 fathoms — is attained between Crete and ilalta. If the whole of the waters of the Mediterranean were to be collected into an aqueous si^here, the latter would have a diameter of 90 miles ; if it fell down upon the earth, it would not even wholly cover a country like Switzerland. The Ionian Sea is scjDarated from the Adriatic by a submarine ridge rising in the Strait of Otranto, and bounded on the west by a shoal or submarine isthmus, already referred to by Strabo, which joins Sicily to Tunis. This isthmus forms the true geological boundary between the western and eastern basins of the Mediterranean, which are connected here by a narrow breach only, the depth of which hardly exceeds 100 fathoms. The western of these basins is the smaller and shallower of the two, but nevertheless it attains a depth of 1,100 fathoms in the Tyrrhenian, and of 1,360 fathoms and even 1,6-10 in the Balearic Sea, and is separated from the waters of the Atlantic by a submarine ridge lying outside tho Strait of Gibraltar, and joining Europe to Africa.* This subdivision of the Mediterranean into separate basins, divided from each other by shoals or submarine ridges, by islands and promontories, sufficiently explains the contrasts between the phenomena of the open ocean and those observed here. In the Mediterranean, it is well known, the tides are almost everywhere irregular and uncertain. To the east of the Narrows of Gibraltar, in the sea extending between Andalusia and Morocco, the tides are hardly felt at all, and Western basin. • Area . . . 365,200 Greatest depth, fathoms 1,640 Average depth, „ . 640 Eastern basin. Adriatic. ArcbipeLigo. Bkck Sea. Mediterranean. 602,000 60,200 60,600 185,300 1,163,300 2,170 605 640 1,070 2,170 960 110 320 320 640 2G THE MEDITEEEANEAN. they are, moreover, interfered with to such an extent by currents that it is exceed- ingly difficult to determine their amplitude, or the establishment of the various ports. Nevertheless the rise and fall of the tidal wave are suificiently marked to have attracted the attention of Greek and Italian navigators. On the coasts of Catalonia, France, Liguria, Naples, Asia Minor, Syria, and Egypt the oscillation is hardly perceptible, but on those of Eastern Sicily and of the Adriatic the tide sometimes rises three feet, and, if accompanied by storms, may even attain a height of ten feet in certain localities. The Straits of ^lessina and of Euripo (Euboea) have their regidar tides, and in the Gulf of Gabes the waters rise and fall with the same regularity as in the open ocean. In the Black Sea, however, no tidal movements Fig. 6. — The Strait of Gibraltar. According to Eobiquet, Eandcgger, and others. Scale 1 : 750,000. J)eptYi less ihan no fathoms Depth no to 170 fathoms ^^ Dfpth i-jo to 55o fathom E^S Depth over SSo fathoms 25 Miles. whatever have been discovered hitherto. It is nevertheless probable that more careful observations will lead to the discovery of a feeble tide, for it is believed that this phenomenon exists even on Lake Michigan, which has only one-iifth the area of the Black Sea. The Mediterranean differs not only from the open ocean with respect to the feebleness and irregularity of its tides, but it is likewise without a great stream- current keeping in constant circulation the whole body of its waters. The currents which have been observed in various divisions of the Mediterranean can be ascribed only to local causes. An Italian geographer of the last centurj^, Montanari, has HYDEOLOGT. 27 advanced an liypotliesis of a great circuit current wLich entered the !Mcdi!jrr.iiioan through the Strait of Gibraltar, and, after having washed the shores of Africa as far as Egypt, returned to the west along those of Asia and Europe ; but careful obsei"vers have vainly endeavoured to discover its existence. They have met only with local currents, produced by an indraught of the waters of tho Atlantic, by winds, by the floods of rivers, or by an excess of evaporation. One of these currents sets along the coasts of Slorocco and Algeria from west to east ; anolhcr flows along the Italian coast of the Adriatic from north to south ; and a third from the mouth of the Rhone in the direction of Cette and Port Vendres. In fact, the configuration of the sea-bottom, and particularly the shoal between Sicilj' and Tunis, precludes the existence of any but surface currents in the Mediter- ranean. Amongst the local currents the existence of which has been most clearly established are those which convey the waters of the Sea of Azof into the Black Sea, and those of the latter into the Archipelago. The Don more than makes up for the loss by evaporation in the Sea of Azof, and its surplus waters find an exit through the Strait of Kerch into the Black Sea. Similarly the waters of the Dniester, tho Dnieper, the Bion, and of the rivers of Asia Minor, and, above all, of the Danube, which by itself conveys a larger volume of water into the Black Sea than all the others combined, are discharged through tho Bosphoiiis and the Dardanelles into the Archipelago. On the other hand, the Archipelago returns to the Black Sea, by means of a submarine coimter-current and of lateral surface currents, a certain quantity of salt water for the fresh water which it receives in excess. This exchange accounts for the salineness of the waters of the Black Sea. The volume of fresh water discharged into it hy the Danube and other rivers is so large that in the course of a thousand years its waters would become perfectly fresh, if there did not exist these compensatory highly saline counter- currents. Analogous pnenomena take place at the other extremity of the Mediterranean. Evaporation there is excessive, owing to the neighbourhood of the burning sands of the deserts, the winds from which blow freely over the sea, absorbing the vapours and dispersing the clouds. The loss by evaporation amounts to at least seven feet in the course of a year, and as the annual rainfall is estimated to amount to twentj' inches only, and the volume of water discharged annually by all the tributary rivers of the Mediterranean, if uniformly spread over its surface, would hardly exceed ten inches in depth, there exists thus an excess of evaporation amounting annually to more than four feet ; and this excess has to be made good by an inflow of the waters of the Atlantic, which takes place through the Strait of Gibraltar, whose volume far exceeds that of the Amazon in a state of flood. This inflow of the waters of tho Atlantic is felt, as a current, as far as the coasts of Sicily, and, like all other currents, it is bounded by lateral currents flowing in a direction contrary to that of the main current. During ebb the insetting Atlantic current takes up the whole of the strait, but when the tide rises the Mediterranean resists more successfully the pressure of the ocean, and this struggle gives birth to 23 THE MEDITEEEANEAN. two counter-currents, one of which skirts the coast of Europe, the other that of Africa between Ceuta and Cape Spartel ; the latter is the larger and more powerful of the two. In addition to these, there exists a submarine current, which convej's the highly saline and heavier waters of the Mediterranean out into the Atlantic. The quantity of salt held in solution in various parts of the Mediterranean differs widely, as the submarine ridges and shoals which divide it into separate basins do not permit its waters to mingle as freely as in the open ocean. Owing to the excess of evaporation, the quantity of salt is greater on the whole than in the Atlantic, and this is the case more particularly on the coast of Africa. But in the Black Sea it is far less, and near the mouths of some of the largo rivers which enter that sea the water is almost fresh.* The temperature of the Mediterranean is affected bj^ the same causes which produce its varying salineness, viz. the existence of shoals and banks, which separate it into distinct sub-basins. In the open ocean the currents convey to all latitudes largo bodies of water, some of them heated by a tropical sun, others cooled by contact with the ice of the polar regions. But these layers of unequal density are regularly superimposed one upon the other, owing to the differences in their temperature : the warm water remains on the surface, whilst the cold water descends to the bottom. In the Mediterranean an analogous superimpositlon exists only to a depth of 110 fathoms, which is the depth of the Atlantic current, flowing into it through the Strait of Gibraltar. If a thermometer be lowered to a greater depth it will indicate no further decrease of temjDerature, and the immense body of water, remaining almost still at the bottom of the Mediterranean, has an equable temperature of about 56° F. Observations made at depths A-arying between 110 and 1,G40 fathoms have always exhibited the same result. Professor Carpenter believes, however, that the abj'ssal waters of some of the volcanic regions have a somewhat higher temperature, which may be due to the presence of lava in a state of fusion. II. — Animal Life. Fisheries and Salt Pans. Another remarkable feature of the abyssal waters of the Mediterranean consists in their poverty of animal life. No doubt there is some life ; the dredgings of the Porcupine and the telegraph cables, which, on being brought to the surface, were found to be covered with shells and polypes, prove this. But, comjjared with those of the ocean, the depths of the Mediterranean are veritable deserts. Edward Forbes, who explored the waters of the Archipelago, arrived at the conclusion that their abyssal depths were entirely devoid of life, but he was wrong when he assumed an exceptional case like this to represent a universal law. Carpenter thinks that this absence of life in the depths of the Mediterranean is due to the great quantity of organic remains which is carried into it by the rivers. These remains absorb the oxygen of the water, and part with their carbonic acid, which is detrimental to • Quantity of salt held in solution in the Atlantic, 36 parts in 1,000 ; in the Mediterranean (mean), 38 parts ; in the Black Sea, 16 parts. ANIMAL LIFE. 29 auiiual life. In niimerous instances tho water of the Mediterranean contains only one-fourth tlie normal quantity of the former gas, but fifty per cent, in excess of the latter. To the presence of these organic remains the Mediterranean is probably indebted for its beautiful azure colour, so different from the black waters of most oceans. This blue, then, which is justly celebrated by poets, would thus be caused by the impurity of the water. M. Delesse has shown that the bottom of nearly the whole of the Mediterranean is covered with ooze. The regions of the Mediterranean immediately below the surface abound in animal life, particularly on the coasts of Sicily and Southern Italy; but nearly all i^pecies, whether fish, testacea, or others, are of Atlantic origin. The Mediterranean, in spite of its vast extent, as far as its fauna is concerned, is nothing but a gulf of the Lusitanian Ocean. Its longitudinal extension and the similaritj- of climate in its various portions have favoured the migration of animals through the Strait of Gibraltar as far as the coasts of S}Tia. At the same time, animal life is most varied near this point of entrj', and the species met with in the western basin are generally of greater size than those which exist in the eastern. A very small pro- portion of non -Atlantic species recalls the fiict that the Mediterranean formerly communicated with the Red Sea and the Indian Ocean. But amongst a total of more than eight hundred molluscs there are only about thirty which have reached the seas of Greece and Sicily through the ancient straits separating Africa from Asia, instead of through the Strait of Gibraltar.* The diminution in the number of species in an easterly direction becomes most striking when we reach the narrow channel of the Dardanelles and the Bosphorus. The Black Sea, in fact, differs essentially from the Mediterranean proper as regards temperature. It is refri- gerated by north-easterly winds sweeping over its surface, to the extent even of portions of it becoming now and then covered with a thin coating of ice, adhering to the coast. The Sea of Azof has frequently disappeared beneath a thick crust of ice, and even the whole of the Black Sea has been frozen over in winters of exceptional severity. The cold surface waters, together with those conveyed into the Black Sea by large rivers, descend to the bottom, and prove most detrimental to animal life. Echinodermata and zoophytes are not-met with at all in the Black Sea; certain classes of molluscs, already rare in the Levantine Sea and the Archipelago, are likewise absent ; and the total number of species of molluscs is only one-tenth of what it is in the Mediterranean. Fish are numerous as far as individuals go, but their species are few. In fact, the fauna of the Black Sea appears to resemble that of the Caspian, from which it is cut off", rather than that of the Greek seas, with which the Sea of Marmara connects it. In addition to the species which have found a second home in the Mediterranean, there are some that must still be looked upon as visitors. Such are the sharks, which extend their incursions to the seas of Sicily, to the Adriatic, and even to the coasts of Egypt and Syria. Such, also, are the larger cetacea — whales, rorquals, and sperm whales — whose visits, however, are confined now to the Tyrrhenian • There are found in the Mediterranean 444 fpecies offish (Gooiwin Auslcn), 850 species of moUusc3 (Jefircys), and about 200 species of foiaminiferse. yO THE MEDITEEEANEAX. basin, and become less frequent from century to century. The tunny -fisb of the Mediterranean are also visitors from tbe coasts of Lusitania. First-rate swimmers, they enter througli the Strait of Gibraltar in spring, ascend the whole of the Mediterranean, make the tour of the Black Sea, and return in autumn to the Atlantic, after having accomplished a journey of some 5,600 miles. In the opinion of the fishermen the tannics go upon their travels in three immense divisions or shoals, and it is the central shoal which visits the coasts of the Tyrrhenian Sea, and consists of the largest and strongest fish. Each of the three divisions appears to be composed of iudividu.ils about the same age. For mutual protection they swim in troops, for they are preyed upon by enemies innumerable. Dolphins and other fish of prey follow their track, but their great destroyer is man. In the summer the tunny fisherj^ or ionnaro, is carried on in numerous bays of Sicih', Sardinia, Naples, and of Provence. Enormous structures consisting of nets Fig. 7.— The Pkincipal Fisheries of the Mediteuranean. Scale 1 : 38,300,000. > Cr. S" !5" So» 35° enclose these bays, and they are ingeniously arranged so as to close gradually around the captured fish, which, passing from net to net, find themselves at last in the " chamber of death," where they are massacred. Millions of pounds of flesh are annually obtained from these floating " slaughter-houses," yet the tunny appears year after year in multitudes, and on the same coasts. There may have been a slight decrease in the number, but their closely packed masses still invade the " Golden Horn " of Byzance and other bays, as they did when first they attracted the attention of Greek naturalists. Next to the tunny fisheries those of the sardines and anchovies are most important. Sea-urchins and other products of the sea are eaten by the inhabitants of the coasts, particularly in Italy, but there is no part of the Mediterranean where animal life is so abundant and so prodigious in quantity as on the celebrated banks of Newfoundland, or on the coasts of Portugal or of the Canaries. A large number of fishing-boats are engaged, not in the capture of fish, but in COMMERCE AND NAVIGATION. 81 the collection of articles of dress or of tbo toilet. The purple-shell fisheries on the coasts of Phoenicia, the Peloponnesus, and Greece are no longer carried on, but hundi-eds of bouts are employed annually during the fine season in fishing for coral or sponges. Coral is found most abundautlj- in tlie western portion of the Mediterranean, and the Italian fishermen do not confine themselves to their own shores — to Sicily, Najilcs, and Sardinia — but also yisit the Strait of Bonifacio, the sea off St. Tropez, the vicinity of Cape Crcus in Spain, and the waters of Parbary. Ordinary sponges are collected in the Gulf of Gabes, and at the other extremity of the Mediterranean, on the coasts of Syria and Asia Minor, and in the straits winding between the Cyclades and Sporades. Sponges are usually found at a depth of from 12 to 150 feet, and can be gathered b}' divers ; whilst coral occurs at far greater depths, and has to be wrenched ofi" with an iron instrument, which brings up its fragments, mixed with ooze, seaweeds, and the remains of marine animal- culrc. This industry is still in a state of barbari.sm : those devoted to it are not as yet sufficiently acquainted with the sea and its inhabitants to enable them to carry on the sponge and coral fisheries in a rational manner. Yet this they must aim at : they must learn how to deprive Proteus, the ever-changing deity, of his dominion over the inhabitants of the deep. Next to the fisheries, the preparation of sea salt constitutes one of the leading industries of the Meditei-rancan coast-lands. But this industrj', too, is frequently carried on in a primitive way, and only in the course of the ^oresent century have scientific methods been introduced in connection with it. The Mediterranean is admirably suited for the production of salt, for its waters have a high temperature, they hold a very largo quantity of salt in solution, the rise and fall of the tides are inconsiderable, and flat seashores alternate with steep coasts and promontories. The most productive salt marshes of the Mediterranean are probably those on the Lagoon, or Etang de Thau, near Cette, and on the littoral of Hyeres ; but consider- able ones may also be met with on the coasts of Spain, in Italj^ in Sardinia, Sicily, Istria, and even on the "limans" of Bessarabia, bordering upon the Black Sea. The annual production of salt is estimated at more than a million tons, and exceeds, therefore, the entire tonnage of the commercial marine of France.* But this quantity, large as it is, is infinitesimal if we compare it with the saline contents of the sea, and science will enable us one daj' to raise a far more abundant treasure from its sterile depths.f III. CoMMEnCE AND NAVIGATION. Whatever advantages may be yielded by fisheries and salt-works, they shrink into insignificance if we compare them with the great gain — material, intellectual, • The production of suit on the coasts of the Mediterranean is thus distributed among its coast- lands ;— Spain, 200,000 tons ; France, 250,000 tons ; Italy, 300,000 tons ; Austria, 70,000 tons ; Eussia, 120,000 ; other countries, 200,000 tons. Total, 1,140,000 tons, valued at £480,000. t The annual produce of the fisheries has been estimated at £3,000,000, of the coral fisheries at £640,000, of the sponge Cbhcries at £40,000. Total, £3,080,000; 82 THE MEDITEEEANEAN. and moral — wliich mankind lias derived from the navigation of this inland sea. It has repeatedly been pointed out by historians that the disposition of the coasts, islands, and peninsulas of the Mediterranean of the Phoenicians and Greeks admi- rably favoured the first essays in maritime commerce. Many causes have con- tributed to make this sea the cradle of Euiopean commerce: the faint summits of distant lands visible even before the port has been quitted ; numerous nooks along the coasts where a safe refuge may be foimd in case of storms ; regular land and sea breezes ; an equability of climate which makes the sailor feel at home wherever business takes him ; and, moreover, a great variety of productions resulting from the diverse configuration of the Mediterranean coast-lands. And this commerce, does it not lead to a peaceful intercourse between peoples on neutral ground, and to mutual enlightenment, brought about by an interchange of ideas ? Every coast-line which facilitates the intercourse between nations is, therefore, of immense value as a means of developing civilisation. Civilisation for many centuries marched from the south-east towards the north- west, and Phosnicia, Greece, Italy, and France have successively become great centres of human intelligence. This historical phenomenon is due to the configura- tion of the sea, which has been the vehicle of migratory nations. In fact, the axis of civilisation, if this expression be allowed, has become confounded with that axis of the Mediterranean which extends from the coast of Syria to the Gulf of Lions, on the coast of France. But the Mediterranean has ceased to be the only centre of gravitation of Europe, which sends its merchantmen now to the two Americas and the farthest East ; and civilisation no longer marches in that general line from east to west, but rather radiates in all directions. Civilising streams depart from England and Germany towards Northern America, and from the Latinised countries of Europe towards Southern America. Their direction is still westerly, but they have been deflected towards the south, to meet the conditions imposed by climate and the geographical configuration of land and sea. It is interesting to trace the changes which have occurred in the historical importance of the Mediterranean. As long as that sea remained the great highway between nations, the commercial republics were content to extend this highway towards the east, by establishing caravan routes to the Gulf of Persia, to India, and to China. In the Middle Ages Genoese factories dotted the coasts of the Black Sea, and extended thence through Trans-Caucasia as far as the Casjjian. European travellers, and particularly Italians, at that time crossed Western Asia in all directions ; and many a route hardly known in our days was then frequented almost daily. But for several centuries direct commercial intercourse with Central Asia has dwindled down to small proportions. The Mediterranean had ceased to be a great ocean highway. Our navigators, no longer dreading a boimdless sea, took their ships into every part of the ocean. The diflicult and perilous land routes were abandoned, the once busy markets of Central Asia became solitudes, and the Mediterranean itself a veritable blind alley, as far as the world's commerce was concerned. This condition of affairs lasted for many years, but since the middle of this century our relations with the East have COMMEECE AXD NAVIGATIOX. 83 been renewed, and the lost ground is rapidly being recovered. "Within the last year a great commercial revolution has been effected through the oiiening of one of the ancient gates of the Mediterranean, and the Suez Canal has become tho great highway of steamers between "Western Europe, the Indies, and Australia. Possiblj', at no distant future, a similar canal will enable our merchantmen to proceed from the BlacK Sea to the Caspian, and perhaps even tj the Amu and the Syr, in the very heart of the ancient continent. It is thus that the great centres of intercommunication, or vital points of our planet, as we should like to call them, become shifted in the course of time. Port Said, an improvised town on a desert shore, has thus become a centre of attraction for travellers and merchandise, whilst the neiglibouring cities of Tyro and Sidon have dwindled down into miserable villages, with nothing to indicate the proud position they held in the past. Carthage, too, has perished, and Venice decayed. Many a thriving place on the shores of the Mediterranean has been reduced to insigniticance through the silting up of its harbour, the employment of larger vessels, the loss of independence, or through political changes of all kinds. But in nearly every instance some neighbouring town has taken the place of these decayed harbours, and most of the great routes of commerce have maintained their original directions, and their terminal points, as well as intermediate stations, have remained in the same localities. There are, moreover, certain places which ships are almost obliged to frequent, and where towns of importance arise as a matter of course. Such are the Straits of Gibraltar and of Messina ; such, also, are places like Genoa, Trieste, and Saloniki, which occupy the bottom of gulfs or bays penetrating far into the land. Ports offering the greatest facilities for embarking merchandise intended for foreign countries, such as Marseilles and Alexandria, are likewise natural centres of attraction to merchants. One town there is in the Mediterranean which enjoys at one and the same time every one of the geographical advantages which we have pointed out, for it is situated on a strait connecting two seas and separating two continents. This town is Constantinople, and despite the deplorable maladminis- tration under which it suffers, its position alone has enabled it to maintain its place amongst the great cities of the world. The ports of the Mediterranean no longer enjoy a monopoly of commerce as they did for thousands of years, but the number of ships to be met with in that inland sea is, nevertheless, proportionately far greater than what we meet with on the open oceans. The commercial marine of the Mediterranean numbers thirty- seven thousand vessels, of a capacity of two million seven hundred and ninety-six thousand tons, without counting lishing-boats. This is more than one-fourth of the entire commercial marine of the world, as respects the number of ships, and one-sixth of it as regards tonnage. This inferiority of tonnage is due to the small vessels of ancient types which still maintain their ground in Greece and Italy, and ■which possess certain advantages for the coasting trade. To this marine of the Mediterranean should be added the vessels belonging to foreign ports, which visit it for purposes of trade, and amongst which those of VOL. I. V 81 THE MEDITEEEANEAN. England take the most prominent rank. The Government of Great Britain has even taken care to secure itself a place amongst the Mediterranean powers. It has occupied Gibraltar, at the western entrance to this basin, and taken possession of Malta, which commands its centre ; and although the eastern entrance, formed by the Suez Canal, is not in its possession, its garrisons on Perim and the rock of Aden are able at any moment to close up the only approach to it which leads from the Indian Ocean through the Red Sea. The share which England takes in the commerce of the Mediterranean is considerable, but it is surpassed by far by that of France and Italy. A sovereign who aspired to the dominion of the world once spoke of the inland sea extending from the Strait of Gibraltar to Egypt as a " French lake ; " but with equal justice might it be called a Greek, a Dalmatian, or Spanish lake, and with still greater an Italian lake. The pirates of Barbary were, in reality, the last " masters " of the Mediterranean : their swift vessels presented themselves unexpectedly before the Fig. 8. — Steamer Eoutes and Telegraphs in the Mediterranean. Scale 1 : 45,000,000. coast towns, and carried off their inhabitants. But since their predatory fleets have been destroyed, the Mediterranean has become the common property of the world, and the meshes of an international network of maritime highways become closer from year to year. The merchantmen no longer pursue their voyages in company as they did in former times, discharging their cargo from port to port, for a single vessel may venture now into any portion of the Mediterranean in safetj'. Still there remain the dangers of reefs and of storms. The art of naviga- tion has made vast progress ; most of the capes, at least on the coasts of Europe, are lit up by lighthouses ; the approaches to the ports are rendered easy by Kghtships, buoys, and beacons ; but shipwrecks are nevertheless of frequent occurrence. Even large vessels founder sometimes, without leaving a stray plank behind to indicate the place of their disappearance. Steamers travelling along prescribed routes are now gradually taking the place of sailing vessels, and where they cross at frequent intervals they may be COMMERCE AND NAVIGATION. 35 likened to ferry-boats crossing a river. The regularity and speed of these steam ferries ; the facilities which they afford for the conveyance of luercliandiso ; the increasing number of I'aihvays which convey the produce of the interior to the seaports ; and lastly, the submarine telegraphs, which have established instantaneous means of commimication between the principal ports, all contribute towards the growth of Mediterranean commerce. This commerce, including imports and exports, and the transit through the Suez Canal, actually amounts to about £353,000,000, a year.* This may not be much for a maritime population of a hundred millions, but a perceptible increase is taking place from year to year. We should also bear in mind that, face to face with the busy peninsulas of Europe, there lies torrid Africa, an inert mass, avoided by the sailors of our own age as much as it was by those of ancient Greece. Its coasts are hardly ever visited, with the exception of those portions which extend from Orun to Tunis, and from Alexandria to Port Said. It is matter of surprise, too, that certain localities which formerly attracted crowds of vessels, such as Cyrenaica, Cyprus, and beautiful Crete, at the very entrance to the Archipelago, should still remain outside the ordinary track of our steamers. • Shipping and commerce of the Mediterranean (estimated) : — CojIMEKCIAL SIaUIXE. SaU-vessels. Stcameis. Tonnage. E.VTErED AKD Cleaked. Tons. Valce of Expobts AXD iMTOlilS. £ Spain (Mediterranean) 2,500 100 250,000 5,000,000 24,000,000 Franco ., 4,000 230 300,000 6,000,000 80,000,000 Italy IS.SOO 140 1,030,000 21,000,000 104,000,000 Austria .... 3,000 92 380,000 8,000,000 1?,000,000 Gneco .... 5,400 20 502,000 8,500,000 8,000,000 Turkey in Europe and A^ia 2,200 10 210,000 25,000,000 24,000,000 Rumania .... — 1,300,000 8,000,000 Russia (Mediterranean) 500 50 50,000 2,000,000 24,000,000 Egjpt 100 25 15,000 4.100,000 20,000,000 Malta and Gibraltar . 200 13 39,000 12,000,000 23,000,000 Algeria .... 170 — 10,000 2,000,000 16,000,000 Tunis, Tripuli, &c. . 500 680 10,000 500,000 4,000,000 37,370 2,796,000 95,300,000 353,000,000 T) 2 GREECE. I. — Gener.u. Aspects. REEOE, within its confined political boundaries, to the south of the Gulfs of Arta and Volo, is a country of about nineteen thousand square miles, or at most equal to the ten-thousandth jDart of the earth's surface. Within the vast empire of Russia there are many dis- tricts more extensive than the whole of Greece, but there is nothing which distinguishes these from other districts which surround- them, and their names call forth no idea in our mind. The little country of the Hellenes, however, so insignificant upon our maps — how many memories does it not awaken ! In no other part of the world had man attained a degree of civilisation equally har- monious in all respects, or more favourable to individual development. Even now, though carried along within an historical cycle far more vast than that of the Greeks, we should do well to look back frequently in order to contemplate those small nations, who are still our masters in the arts, and first initiated us into science. The city which was the " school of Greece " still remains the school of the entire world ; and after twenty centuries of decay, like some of those extinct stars whose luminous rays yet reach the earth, still continues to enlighten us. The considerable part played by the people of Greece during many ages must imdoubtedly be ascribed to the geographical position of their country. Other tribes having the same origin, but inhabiting countries less happily situated — such, for instance, as the Pelasgians of Illyria, who are believed to be the ancestors of the Albanians — have never risen above a state of barbarism, whilst the Hellenes placed themselves at the head of civilised nations, and opened fresh paths to their enterprise. If Greece had remained for ever what it was during the tertiary geological epoch — a vast plain attached to the deserts of Libya, and run over by lions and the rhinoceros — would it have become the native country of a Phidias, an .Jilschylos, or a Demosthenes ? Certainly not. It would have shared the fate of Africa, and, far from talring the initiative in civilisation, would have waited for an impulse to be given to it from beyond. GENERAL ASPECTS. 87 Greece, a sub-peninsula of the peninsula of the Balkans, was even more completely protected by transverse mountain barriers in the north than was Thracia or Macedonia. Greek culture was thus able to develop itself without fear of being stifled at its birth by successive invasions of barbarians. Mounts Olvmpus, Pelion, and Ossa, towards the north and east of Thessaly, consti tutcd the first line of formidable obstacles towards Macedonia. A second barrier, the steep rant^ of the Othrys, runs along what is the present political boundary of Greece. To the south of the Gulf of Lamia a fresh obstacle awaits us, for the range of the (Eta closes the passage, and there is but the narrow pass of the Thermopylae between it and the sea. Having crossed the mountains of the Locri and descended into the basin of Thebae, there stiU remain, to be crossed the Fames or the spurs of the Cithiseron before we reach the plains of Attica. The " isthmus " beyond these is again defende