Mount Barr
From Infogalactic: the planetary knowledge core
Mount Barr | |
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Highest point | |
Elevation | Lua error in Module:Convert at line 1851: attempt to index local 'en_value' (a nil value). |
Prominence | Lua error in Module:Convert at line 1851: attempt to index local 'en_value' (a nil value). |
Coordinates | Lua error in package.lua at line 80: module 'strict' not found. [1] |
Geography | |
Location | British Columbia, Canada |
Parent range | Skagit Range, Cascade Mountains |
Topo map | NTS 092/H05 |
Geology | |
Mountain type | Intrusive |
Volcanic arc/belt | Canadian Cascade Arc Pemberton Volcanic Belt |
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 1,907 m (6,257 ft).
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.[2][3] 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.[2][4][5]
References
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ 2.0 2.1 Miocene peralkaline volcanism in west-central British Columbia - Its temporal and plate-tectonics setting
- ↑ Chapter 5: The Cascade Episode
- ↑ 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
External links
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