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About: Chilcotin Group     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatPlateausOfBritishColumbia, within Data Space : dbpedia.org associated with source document(s)

Type: placeyago:GeologicalFormation109287968yago:Highland109302616yago:NaturalElevation109366317yago:Object100002684yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntityyago:Tableland109453008yago:WikicatPlateausOfBritishColumbia New Facet based on Instances of this Class

The Chilcotin Group, also called the Chilcotin Plateau Basalts, is a large area of basaltic lava that forms a volcanic plateau running parallel with the Garibaldi Volcanic Belt in south-central British Columbia, Canada. The Chilcotin Group were thought to potentially be linked to the partly coeval Columbia River Basalt Group. However, its morphology and geochemistry have been proven much similar to other volcanic plateaus such as the Snake River Plain in Idaho and parts of Iceland (Bevier, 1983).