Second Canyon Cone, also called Canyon Creek Cone is a cinder cone in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada. It is a volcanic feature of the Iskut-Unuk River Cones which is part of the Northern Cordilleran Volcanic Province and formed in the past 10,000 years of the Holocene epoch.[1]
Second Canyon Cone | |
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Highest point | |
Elevation | 300 m (980 ft) |
Coordinates | 56°25′N 130°43′W / 56.41°N 130.72°W |
Geography | |
Location | British Columbia, Canada |
Parent range | Boundary Ranges |
Geology | |
Age of rock | Holocene |
Mountain type | Volcanic plug |
Volcanic arc/belt | Northern Cordilleran Volcanic Province |
Last eruption | Holocene |
See also
editReferences
edit- ^ Catalogue of Canadian volcanoes: Seconed Canyon Cone Archived 2010-12-11 at the Wayback Machine