Thaw Hill Explained

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

Notes and References

1. http://cgc.rncan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_twh_099 Catalogue of Canadian volcanoes: Thaw Hill