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・ Mount Bishop
・ Mount Bishop (British Columbia)
・ Mount Bishop (Camelsfoot Range)
・ Mount Bishop (Elk Range)
・ Mount Bishop (Fannin Range)
・ Mount Bisoke
・ Mount Bistra
・ Mount Bistre
・ Mount Bitgood
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・ Mount Barnard (Canada)
・ Mount Barnett Station
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・ Mount Barney National Park
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Mount Barr
・ Mount Barr Smith
・ Mount Barre
・ Mount Barren
・ Mount Barrington
・ Mount Barrow
・ Mount Barsa
・ Mount Barsoum
・ Mount Bartle Frere
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Mount Barr : ウィキペディア英語版
Mount Barr

Mount Barr is a mountain in the Skagit Range of the Cascade Mountains of southern British Columbia, Canada, located on the northeast side of Wahleach Lake and just southwest of Hope. It is a ridge highpoint with an elevation of .
Mount Barr is one of the numerous magmatic features just north of the Chilliwack batholith. It is part of a large circular igneous intrusion that was placed along the Fraser Fault 16 to 21 million years ago.〔〔(Chapter 5: The Cascade Episode )〕 The intrusion is part of the Pemberton Volcanic Belt, an eroded volcanic belt that formed as a result of subduction of the Farallon Plate starting 29 million years ago.〔(Miocene peralkaline volcanism in west-central British Columbia - Its temporal and plate-tectonics setting )〕〔(Cenozoic to Recent plate configurations in the Pacific Basin: Ridge subduction and slab window magmatism in western North America )〕〔(Catalogue of Canadian volcanoes: Franklin Glacier )〕
==References==


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「Mount Barr」の詳細全文を読む



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