Chilcotin Group
Chilcotin Plateau basalts cover a large area in British Columbia. Basaltic lava formed a volcanic plateau running parallel with the Garibaldi Volcanic Belt, about 150 km from the ocean.
During the Miocene and Pliocene, a volcanic field occurred in British Columbia's Interior Plateau. The basalt is assumed to cover up to 50,000 km2 of the Pacific Northwest. It forms a medium-sized large igneous province, of volume 3300 km3.[1]
Volcanism still continues from time to time. Eruptions were most vigorous 6–10 million years ago (mya) and 2–3 mya, when most of the basalt was released. Smaller eruptions continued from 1.6 mya to 0.01 mya.[2]
Chilcotin Group Media
Cliffs made of low viscosity lava flows in Chasm Provincial Park suggest extensive volcanic activity in the Chilcotin Plateau Basalts
Chilko River and cliffs made of lava flows and ash beds
References
- ↑ Regional stratigraphy and age of Chilcotin Group basalts, south-central British Columbia Retrieved on 20012-09-22
- ↑ National Resources Canada - Catalogue of Canadian volcanoes: Chilcotin Plateau basalts Archived 2008-03-15 at the Wayback Machine Retrieved on 2008-03-15
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