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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 ...
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 ...
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.
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.
Coffee Crater is located in Cassiar Land District of northwestern British Columbia, Canada, just south of Mount Edziza at the southern end of the Big Raven Plateau. [2] [3] [10] It has an elevation of 2,000 metres (6,600 feet) and is one of several volcanic cones in the Snowshoe Lava Field, which is one of the largest areas of Holocene lava flows in the Mount Edziza volcanic complex.
Eve Cone, sometimes referred to as Eve's Cone, is a cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of 1,740 metres (5,710 feet) and is one of several volcanic cones in the Desolation Lava Field at the northern end of the Big Raven Plateau .
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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.