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The Triplex Cones are a group of three cinder cones in northern British Columbia, Canada. [1] They are thought to have last erupted during the Holocene epoch. [ 2 ]
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.
Cinder cones of British Columbia (47 P) Pages in category "Cinder cones of Canada" The following 6 pages are in this category, out of 6 total.
Nahta Cone is located in Cassiar Land District of northwestern British Columbia, Canada, near the northern edge of the Arctic Lake Plateau. [2] [6] [7] It has an elevation of 1,670 metres (5,480 feet) and rises about 60 metres (200 feet) above the glacially scored surface of the plateau to a circular crater breached on the east.
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.
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. Eve Cone stands by itself in the ...
Williams Cone is a satellite cone of Mount Edziza, located 36 km (22 mi) east of Telegraph Creek. It lies just off the northern edge of the Tencho Icefield and is one of the many postglacial cinder cones that lie on the Mount Edziza volcanic complex .
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.