The universal geography : earth and its inhabitants

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•.'It1,10,I•aTHE NOBTH-EAST ATLANTIC,surface of the Great Belt, he mode bis way by the islands of Laaland andFalater to Zealand, diotating peaoe under the walls of Copenhagen, Jiui in[809 the capital of Sweden was in its turn threatened bj a Russian expeditionwhich orossed the Baltic al the Qvarken [elands, the narrowest part of ihc GulfEiI'mii. I iIksi
THE BALTIC. 21No mountains of floating ice are seen in the Baltic, as in the polar seasbut here and there detached masses rising from 14 to 16 feet above thesurface present a faint image of the fragments of glaciers met with in the watersto the south of Spitsbergen and Greenland. These masses, like those of thoglacial epoch, are occasionally charged with stones and other detritus, thus on asmall scale continuing the transport of erratic boulders, at one time of suchimportance in the geological history of Scandinavia, Finland, and Germany.Scientific records quote a great number of facts bearing witness to this displacementof rocks borne southwards by tho broken masses of ice. Blocks of granite,weighing many millions of pounds, have been thus transported from the coast otFinland to Ilogland Island.*The law of decreasing temperature observed in the Atlantic prevails also inthe Baltic, at least in summer. But the transition is here much more rapid, theinland sea being but slightly affected by the action of the warm currents whichtemper the waters of the northern seas. The lower strata vary in temperature,as in the Atlantic, and are usually very near freezing point. Thus the plummetreaching the bottom in a depth of 50 to 100 fathoms in a very short space traversesliquid strata varying at least 18°.The Baltic is nowhere as deep as the Skager Eak. Between Copenhagenand Bornholm the line never reaches a depth of 32 fathoms ; east of Bornholm,and in the same latitude, it falls to 66 ; but the average is about 44, withno more than 8 fathoms on the Stolpe and some other submarine banks.Farther north, where the Baltic is widest, the depth increases with itsarea. The greatest depression discovered by the Pomcrania in 1871 lies betweenGotland and "Windau, where a depth of 126 fathoms was reached, previous butincorrect soundings having given 200 fathoms. All the harbours, both in thesouth and north, are shallow, being inaccessible to vessels drawing over 16to 20 feet. Still, as a whole, the Baltic is deeper than the North Sca.t Itsbed has, so to say, not yet been levelled, still presenting numerous inequalities,in this respect resembling tho beds of the countless fresh-water lakes in Swedenand Finland.There are no appreciable tides in the Baltic. South of the Straits navigationtakes no account of them, though naturalists are able to verify their presencein the Mecklenburg and Pomeranian ports, determining their rise to withina fraction of an inch. Thus in the harbour of WIsmar the difference betweenebb and flow is estimated at about 3 5 inches. The variation diminishescontinually eastwards, at last escaping the most careful observations. Suchfaint oscillations are as nothing compared with the changes produced by theatmospheric currents. The strong and continuous west winds cause the waterto fall from 4 to 5 feet X in Kiel Harbour, and on the low shores of the Baltic the* Von Baer ; Forchhammer ; Ant. von Etzel, " Die Ostsee."t Area of the Baltic 13S,230 square miles.Mean depth (Meyer)207 feet.Approximate contents29,544, 506 cubic yards.% Mbbius, ''Das Thierleben am Boden der dcutschen Ost und Nord See."VOL. V. 1)
Page 1 and 2: pp-i'"**•••%.
Page 7: LIBRARYOF THEr ry of Illinois.
Page 10 and 11: CITYUOAD.
Page 12: ivCONTEXTS.PAOBChap. II. Finland 20
Page 18 and 19: LIST OF ILLUSTRATIONS.ILLUSTRATIONS
Page 20 and 21: MonasteryLIST OF ILLUSTRATION'S.PAG
Page 22 and 23: 2 THE NORTH-EAST ATLANTIC.islands,
Page 24 and 25: 4 TIIE NOKTH-EAST ATLANTIC.The velo
Page 26 and 27: 6THE NOETH-EAST ATLANTIC.boat manne
Page 28 and 29: 8 THE NORTH-EAST ATLANTIC.the norma
Page 30 and 31: 110 THE NORTH-EAST ATLANTIC.pole to
Page 32 and 33: 12 THE NORTH-EAST ATLANTIC.Mohn has
Page 34 and 35: 14 THE NORTH-EAST ATLANTIC.opposing
Page 36 and 37: 1GTHE NOETH-EAST ATLANTIC.constant
Page 38 and 39: 18 THE NOETH-EAST ATLANTIC.THE BALT
Page 42 and 43: 22 THE NORTH-EAST ATLANTIC.water-li
Page 44 and 45: ISLANDS OF THE NORTH ATLANTIC.I.—
Page 46 and 47: 2GISLANDS OF THE NORTH ATLANTIC.The
Page 48 and 49: 28 ISLANDS OF THE NORTH ATLANTIC.pe
Page 50 and 51: 80 ISLANDS OF THE NORTH ATLANTIC.re
Page 52 and 53: 32 ISLANDS OF THE NORTH ATLANTIC.ov
Page 54 and 55: 34 ISLANDS OF THE NORTH ATLANTIC.no
Page 56 and 57: 36 ISLANDS OF THE NORTH ATLANTIC.ar
Page 58 and 59: 33 ISLANDS OF THE NORTH ATLANTIC.Th
Page 60 and 61: 10 ISLANDS OF THE NORTH ATLANTIC.en
Page 62 and 63: 42 ISLANDS OF THE NORTH ATLANTIC.fo
Page 64 and 65: 44 ISLANDS OF THE XOETH ATLANTIC.Mi
Page 66: Sudur-Umdaemid46 ISLANDS OF THE NOR
Page 69 and 70: SCANDINAVIA.CHAPTER I.jEEPER though
Page 71 and 72: THE TIiNINSULA OP JYLLAND. 49Katteg
Page 73 and 74: THE PENINSULA OF JYLLAND. 51the mud
Page 75 and 76: THE DANISH ISLANDS. 53a number of l
Page 77 and 78: THE DANISH ISLANDS. 55— consist o
Page 79 and 80: INHABITANTS—PREHISTORIC REMAINS.
Page 81 and 82: INHABITANTS—PREHISTORIC REMAINS.
Page 83 and 84: TOPOGRAPHY. 61Topography.All the im
Page 86 and 87: •COPENHAGEN .THESOUfS t- i i- 6 B
Page 89 and 90: COPENHAGEN.G3sea, and the land rout
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COPENHAGEN. 65and a model of its ki
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SOCIAL CONDITIONS—OCCUPATIONS. 67
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SOCIAL CONDITIONS—OCCUPATIONS.G9e
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ADMINISTRATION—COLONIES. 71Assemb
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CHAPTER II.THE SCANDINAVIAN PENINSU
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nrsiCAL features of noeytay. 75with
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,RARY
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78 SCANDIXAYTA.o-laciers -were cons
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80 M'AXDINAVIA.opening like crevice
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B2SCANDINAVIA.other equally dangero
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JJ50GEDALSF0SSEN, IN THE DISTRICT O
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M SI AXDIXAYIA.insular masses. The
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THE SCANDINAVIAN FIOEDS. £5tills s
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GLACIAL ACTION"—THE ASAR. 87Glaci
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GLACIAL ACTION—THE ASAE, 89in 184
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GLACIAL ACTION—THE ASAR. 01The be
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UPHEAVAL OF THE LAND. 93rather than
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LAKES. 96tops and headlands are now
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LAKES. 97to the Baltic, and no more
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EIYEKS. 99streams as the llhone or
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EIVEKS. 101amount of their rainfall
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CLIMATE. 103by engineers at 225,000
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CLIMATE. 105Cape ; in summer and wi
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CLIMATE. 107Even in the coldest win
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FLORA. 109of new species. The perfu
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FAUNA.Illwant of cheap fuel. In the
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EARLIEST INHABITANTS. 113later or p
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THE SWEDES AND NORWEGIANS. 115the p
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THE SWEDES AND NORWEGIANS. 117were
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TYPES AXD COSTUMES IN LAPLAND.
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120 SCANDINAVIA.dependent for his s
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122 SCANDINAVIA.churches, all with
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121 SCAHDINAYIA.the houses are main
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126 SCANDINAVIA.the point where the
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128 SCANDINAVIA.Saugesund guards th
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130 SCANDINAVIA.Spitzbergen and the
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132 SCANDINAVIA.Canal, whose sluice
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13-1 SCANDINAVIA.between the three
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13sSCANDINAVIA.Stockholm, capital o
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-ID>J)AV.ENVIRONS.*"-,;"3j~Zi^^n^"^
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138 SCANDINAVIA.and shipping are al
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140 SCANDINAVIA.temple where human
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112 SCANDINAVIA.mining district. Bu
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114 SCANDINAVIA.eruigratiori, which
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146 SCANDINAVIA.also yearly adds ma
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1-18 SCANDINAVIA.by regular parcell
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150 SCANDINAVIA.rodskjaer, each of
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152 SCANDINAVIA.which that of Ammeb
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15JSCANDINAVIA.between Christiania
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156 SCANDINAVIA.The Swedish system,
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View158 SCANDINAVIA.the exact relat
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1G0SCANDINAVIA.to pass a part of th
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162 SCANDINAVIA.and bailiffs {foged
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164 SCANDINAVIA.The Swedish Church
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106 SCANDINAVIA.The militia of the
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THE EUROPEAN ISLANDS OF THE ARCTIC
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170 THE EUROPEAN ISLANDS OF THE AEC
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SPITZBEEGEN. 171Jurassic, and even
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SPITZBERGEN. 173vicissitudes in the
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SPITZBERGEN. 175changes of temperat
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SPITZBEKOEN. 177captured ; but Nord
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WICHE'S LAND. 179to certain unauthe
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the expedition.But from this point
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RUSSIA IN EUROPE.CHAPTER I.GENERAL
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GEOLOGICAL FEATURES. 185that have b
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LAKES AND RIVERS. 187St. Petersburg
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CLIMATE. 189Climate.— Vegetation.
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* Mean temperature in degrees Fahre
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INHABITANTS. 193groups, Uralo-Fiuni
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OEIGIXES OF RUSSIA. 195fifths of th
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THE VARANGIANS. 197the Novgorod Sla
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NOVGOROD IN HEB GLORY. 199the north
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POLISH ASCENDANCY.2C1historic highw
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GROWTH OF RUSSIA. 203herself be one
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SEABOARD AND BOUNDARIES.where could
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CHAPTER II.ALTHOUGH forming part of
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GLACIALFINLAND :ACTION. 209elevatio
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FINLAND: LAKES. 211It looks as if a
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FINLAND: LAKES. 213it has retained
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FINLAND: CLIMATE. 215Climate.— Ve
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FINLAND: INHABITANTS. 217with the R
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FINLAND: TOrOGEAPHY. 219Forsby, on
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FINLAND : NATURALRESOURCES. 221of S
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FINLAND: POTOLATION. 223Industry is
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FINLAND : GOVERNMENT.225one iu twen
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CHAPTER III.THE BALTIC PROVINCES.(E
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TEE BALTIC PROVINCE*. 229drainage i
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TIIE BALTIC PROVINCES. 231and geolo
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THE BALTIC PROVINCES. 233composed t
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THE BALTIC PK0YENCE8. 235vessels, a
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THE BALTIC ITiOVlXCES. 237capital o
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THE LALTIC rKOVIXCE*. 239approaches
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CHAPTER IV.poland (polska).Historic
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POLAND. 243successors soon lost mos
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POLAND. 245in appearance. It was ev
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'•',|',.jl"n -''
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248 RUSSIA JN EEBOrE.Like all civil
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230 RUSSIA IX EUROPE.some of the la
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25 2 KtTSSIA IN EUEOPE.In the "Wart
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254 RUSSIA IN EUEOPE.Few cities of
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CHAPTER V.UPPER DVINA AND NIEMEN BA
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258 RUSSIA IN EUROPE.The Niemen, wh
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260 RUSSIA IX EUROPE.and representi
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262 RUSSIA IN EUROPE.breathing a de
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2G4 RUSSIA IX BUEOPE.labourers rece
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266 RUSSIA IN EUROPE.Jesuits was on
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CHAPTER VI.DNIEPER AND DNIESTER BAS
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'.;.270 RUSSIA IN EUEOPE.on the sur
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272I1; -ssl A IN EUROPE.Water Syste
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271 RUSSIA IX EUROPE.Nearly all its
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27GRUSSIA IN EUEOPE.nowhere an abso
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27KPITSSIA IN EUROPE.side of the li
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280 RUSSIA IX EUROPE.Iii the coast
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2S2RUSSIA IN EUROPE.and beyond it t
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284 . RUSSIAIX EUROPE.Russians may
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28GRUSSIA IN EUKOPE.Topography.The
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288 RUSSIA IX EUROPE.Lug, a tributa
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,;290 RUSSIA IX ETTBOEE.names corre
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292 RUSSIA IN EUROPE.In the ninth c
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201 KUSSIA IN EUEOPE.whence thev so
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29 C RUSSIA IX EUROrE.thousands of
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298 RUSSIA IN ETJEOrE.and in the st
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800 RUSSIA IN EUROPE.provinces, and
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:v.".-'.•302 RUSSIA IN EUROPE.and
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304 EUSSIA IX EUROl'E.enemies from
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306 RUSSIA IN EUROPE.Fanatics are e
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308 RUSSIA IN EUROrE.was one of the
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310 RUSSIA IX ETJEOPE.rate the over
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812 RUSSIA IN EUROPE.opposite bank
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8URUSSIA IN EUEOrE.Ilaji-Bey liman,
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316 RUSSIA TX EUBOPEThe quality of
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318 RUSSIA IX EUROPE.the Moldavian
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:;-nEUSSIA IN EUEOPE.oi' (lie river
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322 EUSSIA IN EUROPE.fallin g from
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324 RUSSIA IN EUROPE.jslaiddown at
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826 i;l SSIA IX EUROPE.of the same
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328 BUSSIA IN EUROPE.history is pre
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330 RUSSIA IN EUROPE.woven stuffs,
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B32RUSSIA IN EUEOPE.Byzantine coins
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334 Bl SSIA IN EUEOPE.Nevertheless
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ST. PETEESBTJEG. 335On the shores o
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.;& 'i;J illVinlSii
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ST. PETERSBURG. 337including the hu
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ST. PETERSBURG. 339Palace, contains
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CHAPTER VIII.LANDS DRAINING TO THE
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ARCTIC RUSSIA. 843stretching southw
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ARCTIC RUSSIA.3Urunning north-west
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ARCTIC RUSSIA. 347from 40 to TO fee
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TIIK WHITE SEA. 349which it is dist
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THE SAMOYEDS. 851Russian plains sou
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ZIRYANIANS. 853or Ch tides, as the
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ONEGA. 155in the first half of the
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AKCHANGEL. :;:,7chief centre of tra
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NOVAYA ZEMLYA. 359frequented by the
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NOVAYA ZEMLYA. 363Government survey
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theCHAPTER IX.VOLGA AND URAL BASINS
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THE VOLGA. 365and rafts are then ab
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THE VOLGA DELTA.3G7narrow peninsula
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Tin: VOLGA DELTA. 369thirds of that
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TUE CASriAX SEA. 371light navigatio
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LACUSTRINE AND SALT STEPPES OF THE
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THE SOUTHERN URALS. 375their operat
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THE SOUTHERN HEALS. 877other plains
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THE GEEAT RUSSIANS. 879the spring f
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THE GREAT RUSSIANS. 881the subject.
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THE GREAT RUSSIANS. 883the mingled
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RELIGIOUS SECTS OF GREAT RUSSIA. 38
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RELIGIOUS SECTS OF GREAT RUSSIA. 38
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RfBINSK. 389industrial centres in X
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TYTES AM) COSTUMES IN THE GOVEKNMEK
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OROL— TULA. 391the artisan classe
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MOSCOW. 393Vitebsk and Smolensk, th
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MOSCOW. 395that " Moscow is celebra
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RIAZAN-KASIMOV. 397monastery. It is
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NIJNI-NOVGOROD. 399paint as many as
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NIJNI-NOVGOBOD. 401The district whe
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THE MORDYINIANS. 403down the Volga
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CHEREMISSIANS—CHUVASHES. 405conne
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KAZAN TATARS. 407Bulgarliks. Differ
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PENZA. 4091875. The kindred Voguls
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BOLOAE. 411history of the Russian s
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SLA.TOUST—VIATKA. 4131721. Thanks
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THE KAIMUK8. 415some Turki tribes,
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SIMBIRSK—SAMAEA. 417enthusiasm in
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DUBOVEA—SAREPTA—-TZAROV. 419the
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THE URAL COSSACKS. 421place having
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THE DON. 423been levelled by the ac
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THE SEA OF AZOV. 425basin.Since 186
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iTHE SEA OF AZOV. 427especially is
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THE SEA OF AZOV. 429the salt consum
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'THE DON COSSACKS. 431Inhabitants.
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THE DOX COSSACKS. 433families, Saxo
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VOEONEJ—KHARKOV. 435as Kozlor and
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GKUGUYEV—SLA.VANSK—SLAYANOSEBBS
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EOSTOV—AZOV-TAGANROG. 439head of
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;«,
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CHAPTER XLTHE CRIMEA.HE Crimean pen
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THE CRIMEA. 443times facilitated co
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TIIE CRIMEA. 445and according to th
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THE CRIMEA. 447a reaction which lus
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SEBASTOPOL. 449The famous siege of
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KAFFA—KERTCH. 451often commanding
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POPULATION. 453surprisingly from pr
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POPULATION. 455far inferior to that
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POPULATION. 457The Russians, as is
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AGRICULTURE. 459who are obliged to
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TEE MIE, OR COMMUNE. 461taiuly rece
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THE MIE, OE COMMUNE. 463both " vill
Page 579 and 580:
MINING AND MANUFACTURES.4G5a more f
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COMMEKCE. 46775,680,000 gallons of
Page 583 and 584:
RAILWAYS.4G9long. Yet, nofcwithstan
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EDUCATION. 471Education.In educatio
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GOVERNMENT AND ADMINISTRATION. 473s
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GOVERNMENT AND ADMINISTRATION. 475m
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-•>THE CHURCH—THE ARMY. 477"whi
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THE AKMY AND NAVY. 479Some of the R
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Hibrring,Aalborg,j(suburbYiborg,APP
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AITENDIX. 483EL—COMMERCE.Shipping
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APPENDIX. 485Area axd Population -o
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APPENDIX. 487VI.—MANUFACTORIES NO
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INDEX.Aa River. Kurlfmd, 229Livonia
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INDEX.1U1Frithiof Glacier, 173Frost
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INDEX. 493Mezen, 358Gulf, 343River,
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INDEX. 495Skj&lfjanaifli6t, 34SkjSr
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,'.J'4T"^L._,.'•;--£'in **£%^SS
Page 616:
"VUNIVERSITY OF ILUNOIS-URBA3 0112
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