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
Features within the Pemberton Belt include:
 * Mount Barr Plutonic Complex
 * Mount Barr
 * Chilliwack batholith
 * Slesse Mountain
 * Chipmunk Mountain 50.58052°N, -122.93235°W
 * Coquihalla Mountain 49.525°N, -121.06°W
 * Crevasse Crag
 * Franklin Glacier Complex
 * Salal Creek Pluton
 * Silverthrone Caldera