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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 ...
Nazko Cone / ˈ n æ z k oʊ / is a small potentially active basaltic cinder cone in central British Columbia, Canada, located 75 km west of Quesnel and 150 kilometers southwest of Prince George. It is considered the easternmost volcano in the Anahim Volcanic Belt .
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.
Eve Cone is a well-preserved black cinder cone on the Big Raven Plateau, British Columbia, Canada. [1] It is one of the 30 cinder cones on the flanks of the massive shield volcano of Mount Edziza that formed in the year 700, making it one of the most recent eruptions on the Big Raven Plateau and in Canada.
Sidas Cone is a cinder cone on the Big Raven Plateau at the northern end of Mount Edziza Provincial Park in British Columbia, Canada. Its name, meaning "cut oneself with a knife" in the Tahltan language , is descriptive of the breach that has cut the cone into two symmetrical halves.
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.
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