Mount Frazier (Montana)

Mount Frazier
Mount Frazier
	East aspect
Highest point
Elevation	8,315 ft (2,534 m)
Prominence	1,315 ft (401 m)
Parent peak	Peak 8333
Isolation	3.26 mi (5.25 km)
Coordinates	48°01′04″N112°45′07″W / 48.01774438°N 112.75198195°W
Geography
	Mount Frazier Location in Montana Mount Frazier Location in the United States
Location	Teton County, Montana, U.S.
Parent range	Rocky Mountains ; Rocky Mountain Front
Topo map	USGS Walling Reef
Geology
Type of rock	Limestone
Climbing
Easiest route	West ridge class 2

Last updated June 30, 2023

Mount Frazier is an 8,315-foot (2,534-metre) mountain summit located in Teton County of the U.S. state of Montana.^[3]

Description

Mount Frazier is located along the Rocky Mountain Front, which is a subset of the Rocky Mountains. It is situated seven miles east of the Continental Divide, along the Bob Marshall Wilderness boundary, on land managed by Lewis and Clark National Forest. The nearest town is Choteau, 30 miles to the southeast, and Old Man of the Hills is 2.6 miles to the north-northwest. Precipitation runoff from the mountain drains into Blackleaf Creek and Dupuyer Creek, and eventually makes its way to the Missouri River. Topographic relief is significant as the summit rises 2,700 feet (820 meters) above the South Fork of Dupuyer Creek in one mile (1.6 km).

Geology

Mount Frazier is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.^[4] The Lewis Overthrust extends over 280 miles (450 km) from Mount Kidd in Alberta, south to Steamboat Mountain which is located 53 miles south of Mount Frazier, which places Mount Frazier within the southern part of the Lewis Overthrust.^[5]

Climate

Based on the Köppen climate classification, Mount Frazier has an alpine subarctic climate characterized by long, usually very cold winters, and mild to warm summers.^[6] Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Related Research Articles

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Elk Mountain is a 7,835-foot-elevation (2,388-meter) mountain summit located in Flathead County in the U.S. state of Montana. It is situated in the southern tip of Glacier National Park, in the Lewis Range, about four miles to the west side of the Continental Divide. US Highway 2 and the Hi-Line Subdivision of the BNSF Railway traverse the southern base of this mountain, approximately four miles west of Marias Pass. Topographic relief is significant as the northwest aspect rises 3,400 feet above Ole Creek in one mile. The nearest higher neighbor is Sheep Mountain 2.7 miles to the north-northwest. The mountain's name first appeared on a 1914 USGS map, and was officially adopted in 1929 by the United States Board on Geographic Names. The summit is the site of a former fire lookout that was built in the 1930s, and removed in 1963.

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Pentagon Mountain is an 8,873-foot (2,704-metre) mountain summit located in Flathead County of the U.S. state of Montana.

Argosy Mountain is an 8,155-foot (2,486-metre) summit located in Flathead County of the U.S. state of Montana.

Castle Reef is an 8,330-foot (2,539-metre) mountain summit located in Teton County of the U.S. state of Montana.

Old Baldy is a 9,156-foot (2,791-metre) double summit mountain located in Teton County of the U.S. state of Montana.

Old Man of the Hills is an 8,229-foot (2,508-metre) mountain summit located in Teton County of the U.S. state of Montana.

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References

1 2 "Mount Frazier, Montana". Peakbagger.com. Retrieved 2021-11-09.
1 2 "Frazier, Mount - 8,315' MT". listsofjohn.com. Retrieved 2021-11-09.
1 2 "Mount Frazier". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2021-11-09.
↑ Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".{{cite journal}}: Cite journal requires |journal= (help)
↑ Feinstein, Shimon; Kohn, Barry; Osadetz, Kirk; Price, Raymond A. (2007-01-01). "Thermochronometric reconstruction of the prethrust paleogeothermal gradient and initial thickness of the Lewis thrust sheet, southeastern Canadian Cordillera foreland belt". Geological Society of America Special Papers. 433: 167–182. doi:10.1130/2007.2433(08). ISBN 978-0-8137-2433-1. ISSN 0072-1077.
↑ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.

External links

Weather: Mount Frazier

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[pb-1] 1 2 "Mount Frazier, Montana". Peakbagger.com. Retrieved 2021-11-09.

[listsofjohn-2] 1 2 "Frazier, Mount - 8,315' MT". listsofjohn.com. Retrieved 2021-11-09.

[gnis-3] 1 2 "Mount Frazier". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2021-11-09.

[gadd-4] Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".{{cite journal}}: Cite journal requires |journal= (help)

[Feinstein_2007-5] Feinstein, Shimon; Kohn, Barry; Osadetz, Kirk; Price, Raymond A. (2007-01-01). "Thermochronometric reconstruction of the prethrust paleogeothermal gradient and initial thickness of the Lewis thrust sheet, southeastern Canadian Cordillera foreland belt". Geological Society of America Special Papers. 433: 167–182. doi:10.1130/2007.2433(08). ISBN 978-0-8137-2433-1. ISSN 0072-1077.

[Peel-6] Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.

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