Misplaced Pages

Mount Clark (Washington)

Article snapshot taken from Wikipedia with creative commons attribution-sharealike license. Give it a read and then ask your questions in the chat. We can research this topic together.
Mountain in Washington (state), United States
Mount Clark
Highest point
Elevation7,528 ft (2,295 m)
Prominence608 ft (185 m)
Parent peakMount Johnson
Isolation0.33 mi (0.53 km)
Coordinates47°50′08″N 123°13′54″W / 47.8355277°N 123.2317826°W / 47.8355277; -123.2317826
Geography
Mount Clark is located in Washington (state)Mount ClarkMount ClarkLocation of Mount Clark in WashingtonShow map of Washington (state)Mount Clark is located in the United StatesMount ClarkMount ClarkMount Clark (the United States)Show map of the United States
CountryUnited States
StateWashington
CountyJefferson
Protected areaOlympic National Park
Parent rangeOlympic Mountains
Topo mapUSGS Mount Deception
Geology
Rock ageEocene
Rock typebasalt
Climbing
Easiest routeclass 3 scrambling

Mount Clark is a 7,528-foot (2,295-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Its nearest higher peak is Sweat Spire (7,580 ft) on Mount Johnson, 0.26 mi (0.42 km) to the southwest, and Mount Walkinshaw is set 0.9 mi (1.4 km) to the north. It is the second highest peak in The Needles range, which is a subrange of the Olympic Mountains, and seventh highest in the Olympic Mountains. The climbing routes on Mt. Clark start at Class 3 scrambling and range up to Class 5.5 via the central South Face. Precipitation runoff from the mountain drains into tributaries of the Dungeness River.

History

The first ascent of the mountain was made on August 21, 1940, by George R. Martin and Elvin Johnson who dubbed the peak Mt. Belvedere.

The mountain was officially named in 1965 to honor Irving M. Clark (1882-1960), a Seattle conservationist and leader in the establishment of Olympic National Park.

Climate

Based on the Köppen climate classification, Mount Clark is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snow. As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. 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. The months of July through September offer the most favorable weather for climbing.

Gallery

  • Mount Clark centered, with Sweat Spire and Mt. Johnson (left) Mount Clark centered, with Sweat Spire and Mt. Johnson (left)
  • The Needles and Mount Clark The Needles and Mount Clark

See also

References

  1. ^ "Mount Clark". Peakbagger.com.
  2. ^ "Clark, Mount – 7,528' WA". listsofjohn.com. Retrieved 2024-04-13.
  3. ^ "Mount Clark". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2019-01-21.
  4. ^ Mount Clark at Climbers Guide Olympics
  5. Peakbagger Olympic Mountain 6500-foot Peaks
  6. ^ Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  7. 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.
  8. ^ McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.

External links

Categories: