Tom MacKay Creek Cone explained

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 that has a maximum thickness of 30m (100feet).^[2]

See also

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

Notes and References

1. http://cgc.rncan.gc.ca/volcanoes/cat/volcano_e.php?id=svb_tmc_047 Catalogue of Canadian volcanoes: Tom MacKay Creek Cone
2. Petrography, Geochemistry and Petrogenesis of the Iskut-Unuk Rivers Volcanic Centres, Northwestern British Columbia, by Steinunn Hauksdottir, 1994