Cache Hill is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period. [1] Once used as an airdrop for food and supplies by the Geological Survey of Canada, hence its name, it is located north of Raspberry Pass in Mount Edziza Provincial Park. [2]
See also
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Volcanism of Canada
- Volcanism of Western Canada
References
- ^ "Cache Hill". Catalogue of Canadian volcanoes. Archived from the original on 2011-06-04.
- ^ "Cache Hill". BC Geographical Names.
57°31′54″N 130°40′15″W / 57.53167°N 130.67083°W
 | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
Cache Hill is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period. [1] Once used as an airdrop for food and supplies by the Geological Survey of Canada, hence its name, it is located north of Raspberry Pass in Mount Edziza Provincial Park. [2]
See also
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Volcanism of Canada
- Volcanism of Western Canada
References
- ^ "Cache Hill". Catalogue of Canadian volcanoes. Archived from the original on 2011-06-04.
- ^ "Cache Hill". BC Geographical Names.
57°31′54″N 130°40′15″W / 57.53167°N 130.67083°W
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| This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |