Source Hill is a cinder cone in northwestern British Columbia, Canada. It is polygenetic in nature, having erupted more than once throughout its eruptive history. [1] It is one of the volcanoes in the central portion of the Mount Edziza volcanic complex and last erupted during the Pleistocene period. [1]
See also
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Volcanology of Canada
- Volcanology of Western Canada
References
- ^ a b Catalogue of Canadian volcanoes: Source Hill Archived 2011-07-06 at the Wayback Machine
57°17′N 130°49′W / 57.28°N 130.82°W
 | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
Source Hill is a cinder cone in northwestern British Columbia, Canada. It is polygenetic in nature, having erupted more than once throughout its eruptive history. [1] It is one of the volcanoes in the central portion of the Mount Edziza volcanic complex and last erupted during the Pleistocene period. [1]
See also
- List of volcanoes in Canada
- List of Northern Cordilleran volcanoes
- Volcanology of Canada
- Volcanology of Western Canada
References
- ^ a b Catalogue of Canadian volcanoes: Source Hill Archived 2011-07-06 at the Wayback Machine
57°17′N 130°49′W / 57.28°N 130.82°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. |