Thaw Hill
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.
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.