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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.
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.
[2] [6] It was required for geology reporting purposes since Jack Souther, a volcanologist of the Geological Survey of Canada, was studying the area in detail between 1970 and 1992. [ 7 ] [ 8 ] [ 9 ] The escarpment was named for its association with Mess Creek , a tributary of the Stikine River which flows into Sumner Strait of southeast Alaska .
Fiord Ranges - Geophysical Survey of Canada designation for the Kitimat Ranges, plus the lower portion of the Pacific Ranges between the icefield-massifs at the core of the range and the coast. [3] The latter are sometimes labelled the Front Ranges on some topographic maps but are not in evidence on modern versions. Pacific Ranges. Chilcotin Ranges
Topographical map of British Columbia. Geography of British Columbia. British Columbia is: a province of Canada; Location: The regions in which British Columbia is located are: Northern Hemisphere, Western Hemisphere. Americas. North America. Northern America. Canada. Western Canada; Extreme points of British Columbia
This is a list of Boundary Peaks of the Alaska–British Columbia border, including those on the Alaska–Yukon border, being those peaks named as border-points of the Canada–United States border as a result of the Alaska Boundary Settlement of 1903 and associated later surveys.
Mess Creek, formerly known as Mestua, is a tributary of the Stikine River in northwestern British Columbia, Canada. [3] It flows north and northwest for about 110 km (68 mi), through a lake and a gorge to join the Stikine River, which in turn flows southwest across the Canada–United States border into Alaska where it empties into various straits of the Inside Passage.
The Challenger Relief Map of British Columbia is a hand-built topographic map of the province, 80 feet by 76 feet. Built by George Challenger and his family from 1947 to 1954, it features all of B.C.'s mountains, lakes, rivers and valleys in exact-scaled topographical detail.
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related to: bc geological survey maps geography