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From Wikipedia, the free encyclopedia
(Redirected from Seconed Canyon Cone)
Second Canyon Cone
Highest point
Elevation300 m (980 ft)
Coordinates 56°25′N 130°43′W / 56.41°N 130.72°W / 56.41; -130.72
Geography
Location British Columbia, Canada
Parent range Boundary Ranges
Geology
Age of rock Holocene
Mountain type Volcanic plug
Volcanic arc/ belt Northern Cordilleran Volcanic Province
Last eruption Holocene

Second Canyon Cone, also called Canyon Creek Cone is a cinder cone in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada. It is a volcanic feature of the Iskut-Unuk River Cones which is part of the Northern Cordilleran Volcanic Province and formed in the past 10,000 years of the Holocene epoch. [1]

See also

References


From Wikipedia, the free encyclopedia
(Redirected from Seconed Canyon Cone)
Second Canyon Cone
Highest point
Elevation300 m (980 ft)
Coordinates 56°25′N 130°43′W / 56.41°N 130.72°W / 56.41; -130.72
Geography
Location British Columbia, Canada
Parent range Boundary Ranges
Geology
Age of rock Holocene
Mountain type Volcanic plug
Volcanic arc/ belt Northern Cordilleran Volcanic Province
Last eruption Holocene

Second Canyon Cone, also called Canyon Creek Cone is a cinder cone in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada. It is a volcanic feature of the Iskut-Unuk River Cones which is part of the Northern Cordilleran Volcanic Province and formed in the past 10,000 years of the Holocene epoch. [1]

See also

References



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