Mount Queets

Last updated
Mount Queets
Mount Queets, Olympic National Park.jpg
Highest point
Elevation 6,476 ft (1,974 m) [1]
Prominence 516 ft (157 m) [1]
Coordinates 47°45′44″N123°35′43″W / 47.762335°N 123.595156°W / 47.762335; -123.595156 [1]
Geography
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Mount Queets
Location of Mount Queets in Washington
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Mount Queets
Mount Queets (the United States)
Location Olympic National Park
Jefferson County, Washington, United States
Parent range Olympic Mountains
Topo map USGS Mount Queets
Geology
Age of rock Eocene
Type of rock basalt
Climbing
First ascent 1890 Harry Fisher (aka James B. Hanmore), Nelson Linsley
Easiest route Scrambling YDS 2 via North Ridge [2]
Summit of Mount Queets with Mt. Meany in background Summit of Mount Queets.jpg
Summit of Mount Queets with Mt. Meany in background

Mount Queets [3] is a 6,476-foot (1,974-metre) mountain summit located deep within Olympic National Park in Jefferson County of Washington state. With a good eye and clear weather, the top of the mountain can be seen from the visitor center at Hurricane Ridge. Its nearest higher peak is Mount Meany (6,695 ft), 0.8 mi (1.3 km) to the south. [1] Due to heavy winter snowfalls, Mount Queets supports the Queets Glacier in a cirque on its north slope, despite its modest elevation. Precipitation runoff from the mountain drains into the headwaters of both the Elwha River and Queets River. There are scrambling routes ranging from class YDS 2 via the North Ridge, class 3 via the ridge from Mt. Meany, and class 4 via the Queets Glacier. [2]

Contents

History

The present day Mt. Meany - Mt. Queets area was referred to as Mt. Mesachie on the 1896 Gilman National Geographic Map. [4] The word mesachie is from Chinook Jargon and means wicked. [5]

The mountain was dubbed "Mt. Hearst" during the 1889-90 Seattle Press Expedition to honor William Randolph Hearst, owner of the San Francisco Examiner, but Mount Queets is the officially accepted name today. [4] The name "Queets" first appeared on the Surveyor General's map of Washington Territory referring to the Queets River, then was later applied to the glacier on the mountain which is the primary source of the river. The word "Queets" is a derivation of the name of the Quai'tso (Queets) tribe.

The first ascent of the mountain was made in 1890 by Harry Fisher (aka James B. Hanmore) and Nelson Linsley during the second O’Neil Expedition. [2] [4]

Climate

Based on the Köppen climate classification, Mount Queets is located in the marine west coast climate zone of western North America. [6] 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 (a process called orographic lift). As a result, the Olympics experience high precipitation and cloudy skies during the winter months. High pressure systems over the Pacific Ocean intensify during the summer months, resulting in low precipitation and clear skies.

See also

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<span class="mw-page-title-main">Mount Steel</span> Mountain in Washington, USA

Mount Steel is a 6,225-foot-elevation (1,897-meter) mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. It is situated in Olympic National Park and the Daniel J. Evans Wilderness. The nearest higher neighbor is Mount Duckabush, 1.36 mi (2.19 km) to the southwest. Precipitation runoff from the mountain drains south into tributaries of the North Fork Skokomish River, and north into headwaters of the Duckabush River. Topographic relief is significant as the summit rises over 3,400 feet (1,036 m) above the Duckabush River in approximately one mile.

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

<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.

References

  1. 1 2 3 4 "Mount Queets". Peakbagger.com.
  2. 1 2 3 climbersguideolympics.com Mount Queets
  3. "Mount Queets". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2019-01-23.
  4. 1 2 3 Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  5. Beckey, Fred (2003). Cascade Alpine Guide: Climbing and High Routes, Stevens Pass to Rainy Pass. The Mountaineers Books. pp. 353–355. ISBN   978-0-89886-838-8.
  6. 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.