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Pemberton Volcanic Belt : ウィキペディア英語版 | Pemberton Volcanic Belt
The Pemberton Volcanic Belt is an eroded Oligocene-Miocene volcanic belt at a low angle near Mount Meager, 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 *Salal Creek Pluton
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Pemberton Volcanic Belt」の詳細全文を読む
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