Pillow Ridge

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Pillow Ridge
Highest point
Elevation 2,400 m (7,900 ft)
Coordinates 57°45′34″N 130°39′6″W / 57.75944°N 130.65167°W / 57.75944; -130.65167Coordinates: 57°45′34″N 130°39′6″W / 57.75944°N 130.65167°W / 57.75944; -130.65167
Geography
Location British Columbia, Canada
Parent range Tahltan Highland
Geology
Age of rock Pleistocene
Mountain type Subglacial mound
Volcanic arc/belt Northern Cordilleran Volcanic Province
Last eruption Pleistocene

Pillow Ridge is a ridge of the Tahltan Highland in northern British Columbia, Canada, located southeast of Telegraph Creek. It extends northwest from Mount Edziza in Mount Edziza Provincial Park.[1]

History[edit]

As its name suggests, Pillow Ridge was named on January 2, 1980 by the Geological Survey of Canada for the classic exposures of subaqueous pillow lava that form the ridge.[1]

Geology[edit]

Pillow Ridge is a volcanic feature associated with the Mount Edziza volcanic complex which in turn form part of the Northern Cordilleran Volcanic Province. It is a subglacial mound that formed in the Pleistocene period when this area was buried beneath glacial ice during the last ice age.[2]

See also[edit]

References[edit]