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 | |
|---|---|
| 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 edit
References edit
- ^ Catalogue of Canadian volcanoes: Seconed Canyon Cone Archived 2010-12-11 at the Wayback Machine
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