Английская Википедия:Coquihalla Mountain

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Шаблон:Short description Шаблон:Infobox mountain

Coquihalla Mountain is an extinct stratovolcano in Similkameen Country, southwestern British Columbia, Canada, located Шаблон:Convert south of Falls Lake and Шаблон:Convert west of Tulameen between the Coquihalla and Tulameen rivers. With a topographic prominence of Шаблон:Convert, it towers above adjacent mountain ridges. It is the highest mountain in the Bedded Range of the northern Canadian Cascades with an elevation of Шаблон:Convert and lies near the physiographic boundaries with the Coast Mountains on the west and the Interior Plateau on the east.

Geology

Coquihalla Mountain is a major preserved feature in the Miocene age Pemberton Volcanic Belt that was erupting about 21 to 22 million years ago.[1][2] Like the Pemberton Volcanic Belt, Coquihalla Mountain formed as result of Cascadia subduction.

See also

References

Шаблон:Reflist

External links


Шаблон:BritishColumbia-geo-stub