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| photo_caption = North face of Plinth Peak
| photo_caption = North face of Plinth Peak
| elevation_m = 2677
| elevation_m = 2677
| elevation_ref = <ref name=bivouac>{{cite bivouac|id=952|name=Plinth Peak|accessdate=20 August 2013}}</ref>
| elevation_ref =
| prominence_m = 947
| prominence_m = 947
| prominence_ref =
| prominence_ref = <ref name=bivouac/>
| location = [[British Columbia|British Columbia, Canada]]
| location = [[British Columbia|British Columbia, Canada]]
| range = [[Pacific Ranges]]
| range = [[Pacific Ranges]]
| map =
| coordinates = {{coord|50|38|42.7|N|123|30|38.9|W|type:mountain_region:CA}}
| coordinates = {{coord|50|38|42.7|N|123|30|38.9|W|type:mountain_region:CA}}
| topo = [[National Topographic System|NTS]] 92J/12
| topo = [[National Topographic System|NTS]] 92J/12
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| volcanic_arc/belt = [[Canadian Cascade Arc]]{{clear}}[[Garibaldi Volcanic Belt]]
| volcanic_arc/belt = [[Canadian Cascade Arc]]{{clear}}[[Garibaldi Volcanic Belt]]
| last_eruption = [[Pleistocene]]
| last_eruption = [[Pleistocene]]
| first_ascent = 1931 N. Carter; A. Dalgleish; T. Fyles; M. Winram
| first_ascent = 1931 N. Carter; A. Dalgleish; T. Fyles; M. Winram<ref name=bivouac/>
| easiest_route = rock/ice climb
| easiest_route = rock/ice climb
}}
}}
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'''Plinth Peak''', sometimes called '''Plinth Mountain''', is the highest [[satellite cone]] of [[Mount Meager]], and one of four overlapping volcanic cones which together form a large volcanic complex in the [[Garibaldi Volcanic Belt]] of the [[Canadian Cascade Arc]]. It is one of the most recently formed volcanic formations of the Mount Meager massif.
'''Plinth Peak''', sometimes called '''Plinth Mountain''', is the highest [[satellite cone]] of [[Mount Meager]], and one of four overlapping volcanic cones which together form a large volcanic complex in the [[Garibaldi Volcanic Belt]] of the [[Canadian Cascade Arc]]. It is one of the most recently formed volcanic formations of the Mount Meager massif.


Plinth Peak is the highest volcanic peak of Mount Meager. Located on the steep north flank of Plinth is the remnant of an inner [[Volcanic crater|crater]] wall that was destroyed by a [[lateral eruption|lateral blast]] during a period of volcanic activity about 2,350&nbsp;years ago.
Plinth Peak is the highest volcanic peak of Mount Meager. Located on the steep north flank of Plinth is the remnant of an inner [[Volcanic crater|crater]] wall that was destroyed by a [[lateral eruption|lateral blast]] during a period of volcanic activity about 2,350&nbsp;years ago.{{citation needed|date=August 2013}}


==See also==
==See also==
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==References==
==References==
{{reflist}}

* [http://www.bivouac.com/MtnPg.asp?MtnId=952 Plinth Peak] in the Canadian Mountain Encyclopedia.
* [http://www.bivouac.com/MtnPg.asp?MtnId=952 Plinth Peak] in the Canadian Mountain Encyclopedia.



Revision as of 06:24, 20 August 2013

Plinth Peak
North face of Plinth Peak
Highest point
Elevation2,677 m (8,783 ft)[1]
Prominence947 m (3,107 ft)[1]
Coordinates50°38′42.7″N 123°30′38.9″W / 50.645194°N 123.510806°W / 50.645194; -123.510806
Geography
Map
LocationBritish Columbia, Canada
Parent rangePacific Ranges
Topo mapNTS 92J/12
Geology
Rock agePleistocene
Mountain typeStratovolcano
Volcanic arc/beltCanadian Cascade Arc
Garibaldi Volcanic Belt
Last eruptionPleistocene
Climbing
First ascent1931 N. Carter; A. Dalgleish; T. Fyles; M. Winram[1]
Easiest routerock/ice climb

Plinth Peak, sometimes called Plinth Mountain, is the highest satellite cone of Mount Meager, and one of four overlapping volcanic cones which together form a large volcanic complex in the Garibaldi Volcanic Belt of the Canadian Cascade Arc. It is one of the most recently formed volcanic formations of the Mount Meager massif.

Plinth Peak is the highest volcanic peak of Mount Meager. Located on the steep north flank of Plinth is the remnant of an inner crater wall that was destroyed by a lateral blast during a period of volcanic activity about 2,350 years ago.[citation needed]

See also

References

  1. ^ a b c "Plinth Peak". Bivouac.com. Retrieved 20 August 2013.