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SAKHALIN, or SAGHALIEN

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Originally appearing in Volume V24, Page 54 of the 1911 Encyclopedia Britannica.
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SAKHALIN, or SAGHALIEN , a large elongated See also:island in the See also:North Pacific, lying between 450 57' and 540 24' N., off the See also:coast of the See also:Russian Maritime See also:Province in See also:East See also:Siberia, divided between the Russian and See also:Japanese empires. Its proper See also:Ainu name, Karafuto or Karaftu, has been restored to the island by the Japanese since 1905. Sakhalin is separated from the mainland by the narrow and shallow Strait of Tartary or Mamiya Strait, which often freezes in See also:winter in its narrower See also:part, and from See also:Yezo (See also:Japan) by the Strait of La Perouse. The island is 600 m. See also:long, and 16 to ro5 broad, with an See also:area of 24,560 sq. m. Its See also:orography and See also:geological structure are imperfectly known. Two, or perhaps three, parallel ranges of mountains See also:traverse it from north to See also:south, reaching 2000 to 5000 ft. (Mt. Ichara, 486o ft.) high, with two or more wide depressions, not exceeding 600 ft. above the See also:sea. Crystalline rocks See also:crop out at several capes; Cretaceous See also:lime-stones, containing an abundant and specific See also:fauna of gigantic See also:ammonites, occur at Dui on the See also:west coast, and See also:Tertiary conglomerates, sandstones, marls and See also:clays, folded by subsequent upheavals, in many parts of the island. The clays, which contain layers of See also:good See also:coal and an abundant fossil vegetation, show that during the See also:Miocene See also:period Sakhalin formed part of a See also:continent which comprised north See also:Asia, See also:Alaska and japan, and enjoyed a comparatively warm See also:climate. The See also:Pliocene deposits contain a mollusc fauna more See also:arctic than that which exists at the See also:present See also:time, indicating probably that the connexion between the Pacific and Arctic Oceans was broader than it is now. Only two See also:rivers are worthy of mention.

The Tym, 250 M. long and navigable by rafts and See also:

light boats for 5o m., flows north and north-east with numerous rapids and shallows, and enters the Sea of See also:Okhotsk. The Poronai flows south-south-east to the Gulf of See also:Patience or Shichiro See also:Bay, on the south-east coast. Three other small streams enter the wide semicircular Gulf of Aniva or Higashifushimi Bay at the See also:southern extremity of the island. Owing to the See also:influence of the raw, foggy Sea of Okhotsk, the climate is very See also:cold. At Dui the See also:average yearly temperature is only 33.0° Fahr. (See also:January 3.4°; See also:July 61 .o°), 35.0° at Kusunai and 37.6° at Aniva (January, 9-50; July, 60.2°). At See also:Alexandrovsk near Dui the See also:annual range is from 81 in July to -38° in January, while at Rykovsk in the interior the minimum is -49° Fahr. The rainfall averages 223 in. Thick clouds for the most part shut out the See also:sun; while the cold current from the Sea of Okhotsk, aided by north-east winds, brings immense See also:ice-floes to the east coast in summer. The whole of the island is covered with dense forests, mostly coniferous. The Ayan spruce (Abies ayanensis), the Sakhalin See also:fir (Abies sachalensis) and the Daurian See also:larch are the See also:chief trees; on the upper parts of the mountains are the Siberian rampant See also:cedar (Cembra pumila) and the Kurilian See also:bamboo (Arundinaria kurilense). See also:Birch, both See also:European and Kamchatkan (Betula See also:elba and B.

Ermani), See also:

elder, See also:poplar, See also:elm, See also:wild See also:cherry (Prunus padus), Taxus baccata and several willows are mixed with the conifers; while farther south the See also:maple, See also:mountain ash and See also:oak, as also the Japanese Panax ricinifolium, the See also:Amur See also:cork (Philodendron amurense), the spindle See also:tree (See also:Euonymus macropterus) and the See also:vine (Vitis thunbergii) make their See also:appearance. The under-See also:woods abound in See also:berry-bearing See also:plants (e.g. See also:cloudberry, See also:cranberry, See also:crowberry, red whortleberry), berried elder (Sambucus racemosa), wild See also:raspberry and Spiraea. Bears, foxes, otters and sables are numerous, as also the See also:reindeer in the north, and the See also:musk See also:deer, See also:hares, squirrels, rats and mice everywhere. The avi-fauna is the See also:common Siberian, and the rivers swarm with See also:fish, especially See also:species pf See also:salmon (Oncorhynchus). Numerous whales visit the sea-coast. Sea-lions, See also:seals and dolphins are a source of profit. Sakhalin was inhabited in the See also:Neolithic See also:Stone See also:Age. See also:Flint implements, exactly like those of Siberia and See also:Russia, have been found at Dui and Kusunai in See also:great See also:numbers, as well as polished stone hatchets, like the European ones, See also:primitive pottery with decorations like those of See also:Olonets and stone weights for nets. Afterwards a See also:population to whom See also:bronze was known See also:left traces in earthen walls and See also:kitchen-middens on the Bay of Aniva. The native inhabitants consist of some 2000 Gilyaks, 1300 Ainus, with 750 Orochons, 200 See also:Tunguses and Some Yakuts. The Gilyaks in the north support themselves by fishing and See also:hunting. The Ainus inhabit the south part of the island.

There are also 32,000 Russians, of whom over 22,150 are convicts. A little coal is See also:

mined and some See also:rye, See also:wheat, oats, See also:barley and vegetables are grown, although the period during which vegetation can grow averages less than roo days. Fishing is actively prosecuted, especially by the Japanese in the south. See also:History.—Sakhalin, which was under See also:Chinese dominion until the 19th See also:century, became known to Europeans from the travels of See also:Martin Gerritz de Vries in the 17th century, and still better from those of La Perouse (1787) and See also:Krusenstern (1805). Both, however, regarded it as a See also:peninsula, and were unaware of the existence of the Strait of Tartary, which was discovered in 1809 by a Japanese, Mamiya Rinzo. The Russian navigator Nevelskoi in 1849 definitively established the existence and navigability of this strait. The Russians made their first permanent See also:settlement on Sakhalin in 1857; but the southern part of the island was held by the Japanese until 1875, when they ceded it to Russia. By the treaty of See also:Portsmouth (U.S.A.) of 1905 the southern part of the island below 5o° N. was re-ceded to Japan, the Russians retaining the other three-fifths of the area. See C. H. See also:Hawes, In the Uttermost East (See also:London, 1903). (P.

A. K. ; J. T.

End of Article: SAKHALIN, or SAGHALIEN

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