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
Features within the Pemberton Belt include: Mount Barr Plutonic Complex Mount Barr Chilliwack batholith Slesse Mountain Chipmunk Mountain Coquihalla Mountain Crevasse Crag Franklin Glacier Complex Salal Creek Pluton Silverthrone Caldera