Mount Cameron (Washington)

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Mount Cameron
Geology ridge peaks snow BBaccus NPS photo (23109779611).jpg
North aspect of Mt. Cameron
Highest point
Elevation 7,190 ft (2,192 m) [1]
Prominence 990 ft (302 m) [1]
Parent peak Mount Johnson (7,680 ft) [2]
Isolation 4.52 mi (7.27 km) [2]
Coordinates 47°49′31″N123°19′42″W / 47.8253625°N 123.3284517°W / 47.8253625; -123.3284517 [3]
Geography
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Mount Cameron
Location of Mount Cameron in Washington
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Mount Cameron
Mount Cameron (the United States)
CountryUnited States
State Washington
County Jefferson
Protected area Olympic National Park
Parent range Olympic Mountains
Topo map USGS Wellesley Peak
Geology
Rock age Eocene
Climbing
Easiest route class 2 scrambling [1]

Mount Cameron is a 7,190-foot-elevation (2,192-meter) triple-summit mountain located within Olympic National Park in Jefferson County of Washington state. Mount Cameron is situated 21 miles southwest of Sequim, and set within the Daniel J. Evans Wilderness. Topographic relief is significant as the southeast aspect rises over 3,300 feet (1,000 meters) above the Dosewallips River in approximately one mile. Precipitation runoff from the mountain drains south into the Dosewallips River, north to the Gray Wolf River via Cameron Creek, and west into headwaters of Lost River. Neighbors include line parent Mount Deception, 4.5 mi (7.2 km) to the east, and proximate parent Mount Johnson, 4.5 mi (7.2 km) to the east. [2]

Contents

Etymology

This landform's toponym was officially adopted in 1969 by the U.S. Board on Geographic Names. [3] This mountain, Cameron Pass, Cameron Glaciers, Cameron Creek, and Cameron Basin are named after Amos Benson Cameron (1872–1951), an early settler of this area who homesteaded for 41 years in the Deer Park area with his wife and 14 children. [4] He pioneered the first trail into Cameron Basin.

Climate

Based on the Köppen climate classification, Mount Cameron is located in the marine west coast climate zone of western North America. [5] 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. [6] 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. [6] The months June through September offer the most favorable weather for viewing or climbing this mountain. [1]

Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust. [7] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

See also

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Adelaide Peak is a 7,300-foot-elevation mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. It is situated within Olympic National Park and the Daniel J. Evans Wilderness. It is part of The Needles range, which is a subset of the Olympic range. The nearest higher peak is Mount Clark, 0.3 mi (0.48 km) to the south, and Mount Walkinshaw rises 0.66 mi (1.06 km) to the north-northwest. The peak is in the rain shadow of the Olympic Range, resulting in less precipitation than Mount Olympus and the western Olympics receive. Precipitation runoff from the mountain drains east into Royal Creek, and west into Gray Wolf River, which are both within the drainage basin of the Dungeness River. Topographic relief is significant as the east aspect rises 2,600 feet (793 m) above Royal Creek in less than one mile.  

<span class="mw-page-title-main">Mount Elk Lick</span> Mountain in Washington (state), United States

Mount Elk Lick is a 6,517-foot-elevation (1,986 meter) mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. It is situated within Olympic National Park, and is set within the Daniel J. Evans Wilderness at the head of Elk Lick Creek. The nearest neighbor is Mount La Crosse, 2.54 mi (4.09 km) to the west, and the nearest higher neighbor is Diamond Mountain, 3.73 mi (6.00 km) to the north-northwest. Precipitation runoff from the mountain drains south into the Duckabush River, and north into the Dosewallips River. Topographic relief is significant as the south aspect rises over 4,300 feet (1,310 m) above the Duckabush valley in approximately one mile. The mountain is remote and an ascent can take four days and involves 46 miles of hiking.

References

  1. 1 2 3 4 Mount Cameron, climbersguideolympics.com
  2. 1 2 3 "Cameron, Mount - 7,190' WA". listsofjohn.com. Retrieved 2021-12-25.
  3. 1 2 "Mount Cameron". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2021-12-25.
  4. Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  5. 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.
  6. 1 2 McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.
  7. Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN   0-87842-160-2.