Little Matterhorn (Montana) Explained

Little Matterhorn
Elevation Ft:7886
Elevation Ref:[1]
Prominence Ft:526
Location:Glacier National Park
Flathead County, Montana, U.S.
Map:Montana#USA
Relief:1
Label Position:bottom
Range:Lewis Range
Coordinates:48.6355°N -113.7852°W
Topo:USGS Mount Cannon
Rock:Sedimentary rock
Easiest Route:West face [2]

Little Matterhorn is a 7,886-foot (2,404 meter) elevation mountain summit located in the Lewis Range, of Glacier National Park in the U.S. state of Montana.[3] The nearest higher peak is Edwards Mountain, 0.9miles to the south.[1] Precipitation runoff from the mountain drains into creeks which empty into Lake McDonald. Based on the Köppen climate classification, Little Matterhorn has an alpine climate 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

Like other mountains in Glacier National Park, Little Matterhorn 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 31NaN1 thick, 50miles wide and 160miles long over younger rock of the cretaceous period.[5]

See also

External links

Notes and References

  1. 4797. Little Matterhorn, Montana. 2019-01-27.
  2. https://listsofjohn.com/peak/26731 listsofjohn.com, Little Matterhorn MT
  3. 773462. Little Matterhorn. 2020-01-30.
  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 . 1027-5606.
  5. Geology of the Rocky Mountains and Columbias . Gadd, Ben . 2008.