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VANCOUVER ISLAND

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Originally appearing in Volume V27, Page 884 of the 1911 Encyclopedia Britannica.
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VANCOUVER See also:ISLAND , the largest of an See also:archipelago of innumerable islands which fringes the Pacific See also:coast of See also:Canada, being at the same See also:time the largest island on the See also:west coast of See also:North See also:America. It forms See also:part of See also:British See also:Columbia. It extends from 48° 20' to 51° N. and from 123° to 128° 30' W., and is thus 285 m. See also:long and from 40 to 8o m. wide, with an See also:area of about 20,000 sq. m., being nearly the See also:size of Nova See also:Scotia, which occupies a corresponding position on the See also:Atlantic coast. It is bounded on the See also:south by the Strait of Juan de Fuca, and is separated from the mainland of the See also:province by the Strait of See also:Georgia and See also:Queen See also:Charlotte See also:Sound. A partially submerged range of mountains, which has been termed the Vancouver Range, runs parallel to the coast of British Columbia; a portion of this range forms Vancouver Island, and it again rises above the level I of the See also:sea farther north, forming the Queen Charlotte Islands. The coast-See also:line is generally precipitous. The west coast is much broken by bays and inlets—the transverse valleys of the-sunken range—which penetrate far inland. Among these may be mentioned the Alberni See also:Canal, which is 20 M. long with a See also:fine See also:harbour at its See also:head, the width of the inlet varying from a See also:half to one mile; See also:Nootka Sound, 6 rn. wide, and sending three arms inland which are from 40 to 16o fathoms deep, as well as See also:Clayoquot, Esperanza, Kyuquot and Quatsino Sounds, which also penetrate deeply into the island. The See also:general height of the See also:mountain-range on Vancouver Island is from 2000 to 3000 ft.; some peaks are 6000 ft.; and See also:Victoria See also:Peak is 7484 ft. high. The island is composed largely of crystalline and metamorphic rocks, but contains some cretaceous areas which hold extensive beds of See also:coal, especially on the See also:east coast. These are See also:mined at See also:Nanaimo, See also:Ladysmith and other points. The island is covered everywhere with an exceedingly dense See also:forest, which makes its interior very difficult to See also:traverse, so that there are still portions of the island which have not been thoroughly explored.

These forests yield immense supplies of magnificent See also:

timber, which together with the coal-See also:field and See also:fisheries constitute the See also:chief resources of the island. There are some level tracts on the south-east coast, as well as in the narrow, well-watered valleys of the interior, which afford excellent agricultural See also:land on which cereals of all kinds, as well as all the fruits of the temperate See also:zone, flourish, and which are also suitable for raising See also:sheep and See also:cattle. The See also:climate of Vancouver Island, especially in the south, is wonder-fully mild for the See also:latitude—as mild as that of See also:Great See also:Britain, with dryer summers. The mean temperature of See also:December at Victoria in the south of the island is about 41° Fahr.; while that of See also:July is about 6o°. In the north and west the rainfall is greater than on the south and east coasts. (F. D.

End of Article: VANCOUVER ISLAND

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