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]
57°17′N130°49′W / 57.28°N 130.82°W / 57.28; -130.82
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