“Tom MacKay Creek Cone”的意思、由来-开放百科全书

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Tom MacKay Creek Cone

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Tom MacKay Creek Cone is a basalt subglacial mound in northwestern British Columbia, Canada. It is part of the Iskut-Unuk River Cones group and last erupted during the Pleistocene epoch.^[1] There is a single vent and a single flow, of weathered, fragmented pillow basalt, of maximum 30m thickness.^[2]

References

1. ^Catalogue of Canadian volcanoes: Tom MacKay Creek Cone {{webarchive |url=https://web.archive.org/web/20070320024348/http://cgc.rncan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_tmc_047 |date=March 20, 2007 }}
2. ^Petrography, Geochemistry and Petrogenesis of the Iskut-Unuk Rivers Volcanic Centres, Northwestern British Columbia, by Steinunn Hauksdottir, 1994

4 : Volcanoes of British Columbia|Mountains of British Columbia|Subglacial mounds of Canada|Pleistocene volcanoes

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