Pillow Ridge
| 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°WCoordinates: 57°45′34″N 130°39′6″W / 57.75944°N 130.65167°W |
| Geography | |
| Location | British Columbia, Canada |
| District | Cassiar Land District |
| Parent range | Tahltan Highland |
| Topo map | NTS 104G15 |
| 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[]
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[]
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[]
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Volcanism of Canada
- Volcanism of Western Canada
References[]
- ^ a b "Pillow Ridge". BC Geographical Names.
- ^ "Catalogue of Canadian volcanoes: Pillow Ridge". Archived from the original on 2007-11-10. Retrieved 2008-05-02.
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- Subglacial mounds of Canada
- Mount Edziza volcanic complex
- Ridges of British Columbia
- Ridges of Canada
- Pleistocene volcanoes
- Monogenetic volcanoes
- Two-thousanders of British Columbia
- British Columbia geography stubs