Answer:
Mount Garibaldi
(British Columbia, Canada) is a composite cone and domes built
on a glacier. It is one of the larger volcanoes (6.5 cubic
kilometers) in a chain of small Quaternary volcanic piles
the Garibaldi Belt within the southern Coast Mountains of
British Columbia. Mount Garibaldi is noteworthy both for the
excellent exposures of its internal structure and for its
striking topographic anomalies, which can be attributed to the
growth of the volcano onto a major glacial stream, part of the
Cordilleran Ice Sheet, and the subsequent collapse of the flanks
of the volcano with the melting of the ice.
