Mount Scott (Washington)

Last updated
Mount Scott
Mount Scott, west aspect.jpg
West aspect
Highest point
Elevation 5,913 ft (1,802 m) [1]
Prominence 1,173 ft (358 m) [2]
Parent peak Mount Ferry (6,195 ft) [2]
Isolation 1.79 mi (2.88 km) [2]
Coordinates 47°50′28″N123°31′47″W / 47.8409886°N 123.5298473°W / 47.8409886; -123.5298473 [3]
Naming
Etymology James Wilmot Scott
Geography
USA Washington relief location map.jpg
Red triangle with thick white border.svg
Mount Scott
Location of Mount Scott in Washington
Usa edcp relief location map.png
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Mount Scott
Mount Scott (the United States)
CountryUnited States
State Washington
County Jefferson
Protected area Olympic National Park
Parent range Olympic Mountains
Topo map USGS Mount Queets
Geology
Rock age Eocene
Climbing
Easiest route class 2 scrambling [2]

Mount Scott is a 5,913-foot (1,802-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. [3]

Contents

Description

Mount Scott is part of the Bailey Range, which is a subrange of the Olympic Mountains, and is set within the Daniel J. Evans Wilderness. [4] The nearest higher neighbor is line parent Mount Ferry, 1.8 mi (2.9 km) to the west, Ludden Peak is set one mile to the north, and Mount Pulitzer rises two miles to the west-southwest. [4] Precipitation runoff from the mountain drains into tributaries of the Goldie River, which in turn is a tributary of the Elwha River. Topographic relief is significant as the summit rises 4,300 feet (1,310 m) above the Elwha Valley in approximately two miles.

Climate

Northwest aspect seen from the side of Ludden Peak Hiker mountain backpacker slope flowers scenic BBaccus NPS photo (22938921381).jpg
Northwest aspect seen from the side of Ludden Peak

Based on the Köppen climate classification, Mount Scott 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]

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.

Etymology

James Scott Review of reviews and world's work (1890) (14740995476).jpg
James Scott

This peak was named by the 1889–90 Seattle Press Expedition for James Wilmot Scott (1849–1895), editor and publisher of the Chicago Herald, a newspaper he started in 1881. [8]

This geographical feature's name has been officially adopted by the U.S. Board on Geographic Names. [3]

See also

Related Research Articles

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

Mount Barnes is a 5,987-foot (1,825-metre) mountain summit in Olympic National Park in Jefferson County of Washington state. Mount Barnes is part of the Bailey Range, which is a subrange of the Olympic Mountains, and is set within the Daniel J. Evans Wilderness. Neighbors include Mount Queets, 1.7 mi (2.7 km) to the southwest, and Mount Olympus is set 6.2 mi (10.0 km) to the west. Precipitation runoff from the mountain drains west into the Queets River, south into headwaters of the Elwha River, and northeast into Goldie River which is a tributary of the Elwha. Topographic relief is significant as the summit rises 3,200 feet (975 m) above Elwha Basin in approximately two miles.

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

Mount Childs is a 6,193-foot (1,888-metre) mountain summit in Olympic National Park in Jefferson County of Washington state. Mount Childs is part of the Bailey Range, which is a subrange of the Olympic Mountains, and is set within the Daniel J. Evans Wilderness. Neighbors include line parent Mount Pulitzer, 1.7 mi (2.7 km) to the north, Mount Barnes, 2 mi (3.2 km) to the south, and Mount Olympus is situated 5.6 mi (9.0 km) to the west. Precipitation runoff from the mountain drains west into headwaters of the Hoh River, and east into Goldie River, which is a tributary of the Elwha River. The first ascent of the summit was made August 6, 1961, by Doug Waali, Bob Wood, and Kent Heathershaw via the east slope.

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

Dodger Point is a 5,760-foot (1,756-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state.

References

  1. Olympic Mountain Rescue, Olympic Mountains: A Climbing Guide, 4th Edition, 2006, Mountaineers Books, ISBN   9780898862065, page 193.
  2. 1 2 3 4 "Scott, Mount – 5,913' WA". listsofjohn.com. Retrieved 2022-01-22.
  3. 1 2 3 "Mount Scott". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2022-01-22.
  4. 1 2 "Mount Scott". Peakbagger.com.
  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.
  8. Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).