{{Short description|Cinder cone in British Columbia, Canada}} '''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.<ref name="SI">[http://cgc.rncan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_shl_100 Catalogue of Canadian volcanoes: Source Hill] {{webarchive|url=https://web.archive.org/web/20110706184018/http://cgc.rncan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_shl_100 |date=2011-07-06 }}</ref> It is one of the volcanoes in the central portion of the [[Mount Edziza volcanic complex]] and last erupted during the [[Pleistocene]] period.<ref name="SI"/>

==See also== *[[List of volcanoes in Canada]] *[[List of Northern Cordilleran volcanoes]] *[[Volcanology of Canada]] *[[Volcanology of Western Canada]]

==References== {{reflist}}

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{{Mount Edziza volcanic complex}} {{Northern Cordilleran volcanoes}} {{Interior Mountains}}

[[Category:Cinder cones of British Columbia]] [[Category:Volcanoes of the Mount Edziza volcanic complex]] [[Category:Polygenetic cinder cones]] [[Category:One-thousanders of British Columbia]] [[Category:Pleistocene British Columbia]]

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