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Tseax Cone, British Columbia; Volcano Mountain, Yukon; Atlin Volcanic Field, British Columbia; Buck Hill, British Columbia; Cache Hill, British Columbia; Dragon Cone ...
Kana Cone is a red nested cinder cone in northern British Columbia, Canada, located northeast of Eve Cone in Mount Edziza Provincial Park. [1] The name of the cone was adopted 2 January 1980 on National Topographic System map 104G/12 after being submitted to the BC Geographical Names office by the Geological Survey of Canada, although the cone was labelled as Ashwell Cone on a 1988 Geological ...
Cracker Creek Cone is a small cinder cone in northwestern British Columbia.A large lava flow that partly filled Ruby Creek may have originated from this cone. The lower west side of the cone appears to be partly covered by glacial till suggesting that the cone is older than the most recent glacial advances down Ruby Creek.
Mount Edziza, a stratovolcano in northwestern British Columbia A topographic map of Canada, showing elevations shaded from green (lower) to brown (higher). Volcanic activity is a major part of the geology of Canada and is characterized by many types of volcanic landform, including lava flows, volcanic plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, submarine volcanoes ...
Pages in category "Cinder cones of British Columbia" The following 47 pages are in this category, out of 47 total. This list may not reflect recent changes. B.
Volcanic Creek Cone is a small cinder cone 20 kilometres (12 miles) northeast of Atlin in northwestern British Columbia. There are two cinder cones and a lava flow at least 3 kilometres (2 miles) long which is present below parts of the tree covered area. The subdued form of Volcanic Creek cone is visible directly below the largest snow patch.
Gabrielse Cone is a remarkably fresh, clearly postglacial monogenetic cinder cone, located in the Tuya Volcanic Field in British Columbia, Canada. It is about 400 m (1,312 ft) in diameter and has a central crater about 30 m (98 ft) deep. It is Holocene in age and to its northeast appears to be breached with the remnants of a lava flow.
There is no universally accepted hierarchical division of the Canadian Rockies into subranges. [1] [2] For ease of navigation only, this article follows [1] and divides the Canadian Rockies into Far Northern Rockies, Northern Continental Ranges, Central Main Ranges, Central Front Ranges and Southern Continental Ranges, each of these subdivided in distinct areas and ranges.
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