Elk Mountain (Clallam County, Washington)

Elk Mountain is a 6,773 feet (2,064 m) summit located in the Olympic Mountains, in Clallam County of Washington state.[2] It is set within Olympic National Park and is situated at the eastern end of Hurricane Ridge. Its nearest higher peak is McCartney Peak, 5.12 mi (8.24 km) to the south-southwest.[1] Precipitation runoff from the south slope of the mountain drains into tributaries of the Dungeness River, whereas the north slope is drained by tributaries of Morse Creek which thence empties into the Strait of Juan de Fuca.

Elk Mountain
Elk Mountain seen from Obstruction Peak
Highest point
Elevation6,773 ft (2,064 m) [1]
Prominence813 ft (248 m) [1]
Coordinates47°55′29″N 123°21′07″W [1]
Geography
Elk Mountain
Location of Elk Mountain in Washington
Elk Mountain
Elk Mountain (the United States)
LocationOlympic National Park
Clallam County, Washington, United States
Parent rangeOlympic Mountains
Topo mapUSGS Maiden Peak
Geology
Age of rockEocene
Type of rockShale
Climbing
Easiest routeHiking Trail

Olympic National Park is home to the largest unmanaged herd of Roosevelt elk in the Pacific Northwest.[3] Named after President Theodore Roosevelt, they are North America's largest variety of elk. It is ironic that none are now found in the area of Elk Mountain. As for the mountain's name origin: According to a 1984 field guide:[4]

There is a story told that in 1890, William Wooding, a local homesteader, along with some friends, slaughtered 15-20 elk at this spot, leaving their carcasses to decay in the woods. Upon returning to civilization, Wooding made the mistake of bragging about the episode. He and his friends were promptly ordered by the authorities to return to the site and carry out the dead elk.

Climate

Set in the north-central portion of the Olympic Mountains, Elk Mountain is located in the marine west coast climate zone of western North America.[5] Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.

Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.[6] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

See also

References
  1. "Elk Mountain, Washington". Peakbagger.com.
  2. "Elk Mountain". Geographic Names Information System. United States Geological Survey. Retrieved 2019-10-08.
  3. National Park Service
  4. Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  5. McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.
  6. Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN 0-87842-160-2.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.