Cache Hill Explained

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]

See also

• List of volcanoes in Canada
• List of Northern Cordilleran volcanoes
• Volcanism of Canada
• Volcanism of Western Canada

References

57.5317°N -130.6708°W

Notes and References

1. Web site: Cache Hill . https://web.archive.org/web/20110604164829/http://gsc.nrcan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_cah_036 . 2011-06-04 . Catalogue of Canadian volcanoes.
2. 9345. Cache Hill.