Thaw Hill is a cinder cone in northwestern British Columbia, Canada. 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
- ^ Catalogue of Canadian volcanoes: Thaw Hill Archived 2011-07-06 at the Wayback Machine
 | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
Thaw Hill is a cinder cone in northwestern British Columbia, Canada. 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
- ^ Catalogue of Canadian volcanoes: Thaw Hill Archived 2011-07-06 at the Wayback Machine
|
| This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |