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The landforms of British Columbia include two major continental landforms, the Interior Plains in the province's northeast, the British Columbia portion of which is part of the Alberta Plateau. The rest of the province is part of the Western Cordillera of North America , often referred to in Canada as the Pacific Cordillera or Canadian Cordillera.
The geology of British Columbia is a function of its location on the leading edge of the North American continent. The mountainous physiography and the diversity of the different types and ages of rock hint at the complex geology , which is still undergoing revision despite a century of exploration and mapping.
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The following outline is provided as an overview of and topical guide to British Columbia: British Columbia is the westernmost of Canada's provinces. It lies between the Pacific Ocean to the west and the province of Alberta to the east. British Columbia was the sixth province to join the Canadian Confederation.
As of January 2020, there were 100 National Historic Sites designated in British Columbia, 13 of which are administered by Parks Canada (identified below by the beaver icon ). [1] [2] The first National Historic Sites to be designated in British Columbia were Fort Langley and Yuquot in 1923.
The province's name was chosen by Queen Victoria, when the Colony of British Columbia (1858–1866), i.e., "the Mainland", became a British colony in 1858. [24] It refers to the Columbia District, the British name for the territory drained by the Columbia River, in southeastern British Columbia, which was the namesake of the pre-Oregon Treaty Columbia Department of the Hudson's Bay Company.
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The Chilcotin (/ tʃ ɪ l ˈ k oʊ t ɪ n /) [2] region of British Columbia is usually known simply as "the Chilcotin", and also in speech commonly as "the Chilcotin Country" or simply Chilcotin. It is a plateau and mountain region in British Columbia on the inland lee of the Coast Mountains on the west side of the Fraser River. Chilcotin is ...