| Volcanic Creek Cone | |
|---|---|
![]() | |
| Interactive map of Volcanic Creek Cone | |
| Highest point | |
| Elevation | 1,520 m (4,990 ft) |
| Coordinates | 59°46′N133°23′W / 59.76°N 133.38°W /59.76; -133.38 |
| Geography | |
| Location | British Columbia, Canada |
| District | Cassiar Land District |
| Parent range | Tagish Highland |
| Geology | |
| Rock age | Pleistocene |
| Mountain type | Cinder cone |
| Last eruption | Holocene |
Volcanic Creek Cone is a smallcinder cone 20 kilometres (12 miles) northeast ofAtlin in northwesternBritish Columbia. There are twocinder cones and alava 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. The cone has probably suffered through at least oneglacial episode. Volcanic Creek cone is part of theNorthern Cordilleran Volcanic Province.
This article about a mountain in theInterior of British Columbia,Canada is astub. You can help Wikipedia byexpanding it. |