Cinder Mountain

This article needs additional citations for verification. Please help by adding citations to reliable sources. Unsourced material may be challenged and removed. Find sources:  –  ·  ·  · scholar · JSTOR (February 2021) (Learn how and when to remove this template message)

Cinder Mountain
Highest point
Elevation	300 m (980 ft)
Coordinates	56°34′N 130°37′W / 56.57°N 130.61°W / 56.57; -130.61
Geography
Location	British Columbia, Canada
Parent range	Boundary Ranges
Geology
Age of rock	Pleistocene
Mountain type	Cinder cone
Last eruption	Pleistocene

Cinder Mountain is a partly eroded cinder cone at the head of , 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 . 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.^[1]

See also[]

• List of volcanoes in Canada
• List of Northern Cordilleran volcanoes
• Northern Cordilleran Volcanic Province
• The Volcano
• Volcanism of Canada
• Volcanism of Western Canada

References[]

This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by .

• v
• t