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From Wikipedia, the free encyclopedia

Cache Hill is a cinder cone in northern British Columbia, Canada. It is thought to have last erupted in the Holocene period.[1] Once used as an airdrop for food and supplies by the Geological Survey of Canada, hence its name, it is located north of Raspberry Pass in Mount Edziza Provincial Park.[2]

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Transcription

See also

References

  1. ^ "Cache Hill". Catalogue of Canadian volcanoes. Archived from the original on 2011-06-04.
  2. ^ "Cache Hill". BC Geographical Names.

57°31′54″N 130°40′15″W / 57.53167°N 130.67083°W / 57.53167; -130.67083


This page was last edited on 9 January 2024, at 03:32
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