Mount Barnes (Washington)

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Mount Barnes
Bailey traverse mtn.jpg
North aspect, centered
Highest point
Elevation 5,987 ft (1,825 m) [1]
Prominence 387 ft (118 m) [2]
Isolation 0.79 mi (1.27 km) [3]
Coordinates 47°47′02″N123°34′34″W / 47.7839245°N 123.5760872°W / 47.7839245; -123.5760872 Coordinates: 47°47′02″N123°34′34″W / 47.7839245°N 123.5760872°W / 47.7839245; -123.5760872 [4]
Naming
Etymology Charles A. Barnes
Geography
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Mount Barnes
Location of Mt. Barnes in Washington
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Mount Barnes
Mount Barnes (the United States)
Location Olympic National Park
Jefferson County, Washington, US
Parent range Olympic Mountains
Bailey Range
Topo map USGS Mount Queets
Geology
Age of rock Eocene
Climbing
First ascent Unknown [2]
Easiest route class 2 scrambling [3]

Mount Barnes is a 5,987-foot (1,825-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. [4] 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. [5] 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.

Contents

Etymology

Seattle Press Expedition, C.A. Barnes tallest in center Seattle Press Exploring Expedition, Seattle, Washington, December 6, 1889 (LAROCHE 20).jpeg
Seattle Press Expedition, C.A. Barnes tallest in center

A peak was named by the Seattle Press Expedition to honor Captain Charles Adams Barnes (1859–1900), the expedition's topographer and historian. [6] In December 1889, he and James Halbold Christie, the leader of the expedition, climbed through deep snow to the ridge just north of the peak, and finally laid eyes on the interior of the range which had been a mystery. Barnes wrote of the spectacle: "Range after range of peaks, snow-clad from base to summit, extended as far as the eye could reach, in splendid confusion." [7] That peak is today known instead as Mount Wilder, and the Mount Barnes of today was originally christened "Mt. Childs" by that same expedition. [6] Mount Childs now rises two miles north of Mount Barnes.

Climate

Based on the Köppen climate classification, Mount Barnes is located in the marine west coast climate zone of western North America. [8] Most weather fronts originate in the Pacific Ocean, and travel east 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. 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 June through August offer the most favorable weather for viewing and climbing. [2]

Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust. [9] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

See also

Related Research Articles

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

Mount Wilder is a 5,939-foot (1,810-metre) mountain summit located near the head of the Elwha Valley, deep within Olympic National Park in Jefferson County of Washington state. Part of the Olympic Mountains, Wilder represents the southernmost peak of the Bailey Range. It is situated 8.7 miles east-southeast of Mount Olympus, and is set within the Daniel J. Evans Wilderness. Neighbors include line parent Mount Dana, 2.3 miles (3.7 km) to the northeast, and Mount Seattle rises 3.7 miles to the southwest. The headwaters of the Goldie River form on the south slope of the mountain, and precipitation runoff from the mountain drains into Goldie River and other tributaries of the Elwha River. Topographic relief is significant as the south aspect of the peak rises nearly 3,800 feet (1,160 m) in less than two miles.

The Bailey Range is a mountain range located within Olympic National Park in Washington state.

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

Ludden Peak is a 5,854-foot (1,784-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Ludden Peak is part of the Bailey Range, which is a subrange of the Olympic Mountains, and is set within the Daniel J. Evans Wilderness. In clear weather, the mountain can be seen from the park's visitor center on Hurricane Ridge. The nearest higher neighbor is Mount Scott, one mile to the south-southeast, line parent Mount Ferry rises 1.6 mi (2.6 km) to the southwest, Dodger Point is 1.9 mi (3.1 km) to the northeast, and Stephen Peak is set 2.7 mi (4.3 km) to the northwest. Precipitation runoff from the mountain drains into tributaries of the Elwha River.

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

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

<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 located within 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.

References

  1. Olympic Mountain Rescue, Olympic Mountains: A Climbing Guide, 4th Edition, 2006, Mountaineers Books, ISBN   9780898862065, page 208.
  2. 1 2 3 Mount Barnes, climbersguideolympics.com
  3. 1 2 "Barnes, Mount - 5,987' WA". listsofjohn.com. Retrieved 2022-01-25.
  4. 1 2 "Mount Barnes". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2022-01-25.
  5. "Mount Barnes". Peakbagger.com.
  6. 1 2 Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  7. Tim McNulty, 2018, Olympic National Park: A Natural History, University of Washington Press, ISBN   9780295743271, page 14.
  8. 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.
  9. Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN   0-87842-160-2.