geo.wikisort.org - MountainsGabrielse 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. The cone is near the headwaters of Iverson Creek.
Postglacial monogenetic cinder cone
Gabrielse Cone |
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Elevation | 1,600 m (5,200 ft) |
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Coordinates | 59°25′07″N 130°23′50″W |
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Location | British Columbia, Canada |
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District | Cassiar Land District |
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Parent range | Stikine Ranges |
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Topo map | NTS 104O8 Maria Lake |
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Age of rock | Holocene |
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Mountain type | Cinder cone |
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Volcanic arc/belt | Northern Cordilleran Volcanic Province |
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Last eruption | Holocene |
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Gabrielse Cone is named after Hu Gabrielse, a Canadian geologist who first identified the cone.[1]
See also
References
- Simpson, K.; Edwards, B.; Wetherell, K. (2006). Documentation of a Holocene volcanic cone in the Tuya-Teslin volcanic field, northern British Columbia. Geological Survey of Canada. p. 2. ISBN 0-662-42326-7.
Volcanoes of the Northern Cordilleran Volcanic Province |
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Cinder cones | |
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Subglacial volcanoes | |
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Lava domes | |
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Shield volcanoes | |
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Volcanic fields | |
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Stratovolcanoes | |
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Volcanic plugs | |
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Mountain ranges | |
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Mountains | |
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