Age of rock Pleistocene Elevation 300 m Last eruption Pleistocene | Mountain type Cinder cone Province British Columbia Parent range Boundary Ranges | |
Location British Columbia, Canada Mountain range Coast Mountains, Boundary Ranges Similar The Volcano, Nahta Cone, Cocoa Crater, Hoodoo Mountain | ||
Official azop 2016 cinder mountain hare scrambles
Cinder Mountain is a partly eroded cinder cone at the head of Snippaker Creek, British Columbia, Canada. It is one of the Iskut-Unuk River Cones and is the source of a basaltic lava flow that extends 4 km (2 mi) north into Copper King Creek. An isolated pile of subaerial basalt flows and associated pillow lava rest on varved clay and till in King Creek. Cinder Mountain last erupted during the Pleistocene.
Contents
- Official azop 2016 cinder mountain hare scrambles
- Map of Cinder Mountain Kitimat Stikine A BC Canada
- 2016 azop cinder mountain hare scramble
- References
Map of Cinder Mountain, Kitimat-Stikine A, BC, Canada
2016 azop cinder mountain hare scramble
References
Cinder Mountain Wikipedia(Text) CC BY-SA