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.

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