Online Encyclopedia

VANCOUVER ISLAND

Online Encyclopedia
Originally appearing in Volume V27, Page 884 of the 1911 Encyclopedia Britannica.
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VANCOUVER ISLAND  , the largest of an
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archipelago of innumerable islands which fringes the Pacific coast of
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Canada, being at the same time the largest island on the west coast of North
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America . It forms
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part of
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British
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Columbia . It extends from 48° 20' to 51° N. and from 123° to 128° 30' W., and is thus 285 m. long and from 40 to 8o m. wide, with an
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area of about 20,000 sq. m., being nearly the
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size of Nova Scotia, which occupies a corresponding position on the
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Atlantic coast . It is bounded on the south by the Strait of Juan de Fuca, and is separated from the mainland of the province by the Strait of
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Georgia and Queen
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Charlotte 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 sea farther north, forming the Queen Charlotte Islands . The coast-
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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 Canal, which is 20 M. long with a
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fine harbour at its head, the width of the inlet varying from a
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half to one mile;
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Nootka Sound, 6 rn. wide, and sending three arms inland which are from 40 to 16o fathoms deep, as well as
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Clayoquot, Esperanza, Kyuquot and Quatsino Sounds, which also penetrate deeply into the island . The general height of the mountain-range on Vancouver Island is from 2000 to 3000 ft.; some peaks are 6000 ft.; and Victoria
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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
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coal, especially on the east coast . These are
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mined at
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Nanaimo,
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Ladysmith and other points . The island is covered everywhere with an exceedingly dense
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forest, which makes its interior very difficult to
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traverse, so that there are still portions of the island which have not been thoroughly explored .

These forests yield immense supplies of magnificent

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timber, which together with the coal-field and
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fisheries constitute the 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
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land on which cereals of all kinds, as well as all the fruits of the temperate zone, flourish, and which are also suitable for raising sheep and cattle . The
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climate of Vancouver Island, especially in the south, is wonder-fully mild for the latitude—as mild as that of
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Great Britain, with dryer summers . The mean temperature of December at Victoria in the south of the island is about 41° Fahr.; while that of
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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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GEORGE VANCOUVER (c. 1758-1798)

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