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Cinder Mountain facts for kids

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Cinder Mountain
Highest point
Elevation 300 m (980 ft)
Location British Columbia, Canada
Parent range Boundary Ranges
Age of rock Pleistocene
Mountain type Cinder cone
Last eruption Pleistocene

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.

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