Pemberton Volcanic Belt
The Pemberton Volcanic Belt is an eroded Oligocene-Miocene volcanic belt at a low angle near the Mount Meager massif, British Columbia, Canada. The Garibaldi and Pemberton volcanic belts appear to merge into a single belt, although the Pemberton is older than the Garibaldi Volcanic Belt. The Pemberton Volcanic Belt is one of the geological formations comprising the Canadian Cascade Arc. It formed as a result of subduction of the former Farallon Plate.
Features[edit]
Features within the Pemberton Belt include:
- Mount Barr Plutonic Complex
- Chilliwack batholith
- Chipmunk Mountain 50°34′49.87″N 122°55′56.47″W / 50.5805194°N 122.9323528°W
- Coquihalla Mountain 49°31′30.0″N 121°03′36.0″W / 49.525000°N 121.060000°W
- Crevasse Crag
- Franklin Glacier Complex
- Salal Creek Pluton
- Silverthrone Caldera
See also[edit]
- Garibaldi Volcanic Belt
- Geology of the Pacific Northwest
- Cascade Volcanoes
- Volcanism of Canada
- Volcanism of Western Canada
References[edit]
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