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. (en)
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. (en)