Capitol Mountain

From Wikipedia, the free encyclopedia
Capitol Mountain
Capitol Mountain.jpg
Northeast aspect
Highest point
Elevation7,868 ft (2,398 m)[1]
Prominence1,308 ft (399 m)[1]
Parent peakArgosy Mountain (8,155 ft)[2]
Isolation4.52 mi (7.27 km)[2]
Coordinates48°02′46″N 113°18′58″W / 48.04618974°N 113.31620248°W / 48.04618974; -113.31620248Coordinates: 48°02′46″N 113°18′58″W / 48.04618974°N 113.31620248°W / 48.04618974; -113.31620248[3]
Geography
Capitol Mountain is located in Montana
Capitol Mountain
Capitol Mountain
Location in Montana
LocationFlathead County, Montana, U.S.
Parent rangeRocky Mountains
Flathead Range
Topo mapUSGS Capitol Mountain
Geology
Age of rockPrecambrian
Type of rockSedimentary rock

Capitol Mountain is a 7,868-foot (2,398-metre) summit located in Flathead County of the U.S. state of Montana.[3]

Description[]

Capitol Mountain is located in the Flathead Range, a subset of the Rocky Mountains. It is situated in the Great Bear Wilderness, on land managed by Flathead National Forest. Precipitation runoff from the mountain drains north to the Middle Fork Flathead River, and topographic relief is significant as the summit rises over 2,800 feet (853 meters) above Schafer Creek in less than two miles. Union Mountain is set two miles to the east-northeast, and the nearest higher neighbor is Argosy Mountain, 4.6 miles (7.4 km) to the southeast. Access to this remote peak is from the nearby Shafer Ranger Station at the Schafer landing strip which was grandfathered with the wilderness designation.

Climate[]

Based on the Köppen climate classification, Capitol Mountain is located in a subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers.[4] Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geology[]

Capitol Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km) long over younger rock of the cretaceous period.[5]

See also[]

References[]

  1. ^ a b "Capitol Mountain, Montana". Peakbagger.com. Retrieved 2021-11-01.
  2. ^ a b "Capitol Mountain - 7,868' MT". listsofjohn.com. Retrieved 2021-11-01.
  3. ^ a b "Capitol Mountain". Geographic Names Information System. United States Geological Survey. Retrieved 2021-11-01.
  4. ^ 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.
  5. ^ Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias". {{cite journal}}: Cite journal requires |journal= (help)

External links[]

Retrieved from ""