Glee Peak

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Glee Peak
Pickets range.jpg
East aspect
Highest point
Elevation 7,180 ft (2,188 m) [1]
Prominence 920 ft (280 m) [2]
Parent peak McMillan Spire (8,004 ft) [1]
Isolation 1.66 mi (2.67 km) [1]
Coordinates 48°45′15″N121°15′22″W / 48.754289°N 121.256146°W / 48.754289; -121.256146 [2]
Naming
Etymology Glee Glenmore Davis
Geography
USA Washington relief location map.jpg
Red triangle with thick white border.svg
Glee Peak
Location in Washington
Usa edcp relief location map.png
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Glee Peak
Glee Peak (the United States)
Location North Cascades National Park
Whatcom County, Washington, U.S.
Parent range Cascade Range
North Cascades
Picket Range
Topo map USGS Mount Challenger
Geology
Type of rock Granodiorite
Climbing
Easiest route scrambling

Glee Peak is a 7,180-foot-elevation (2,190-meter) mountain summit located in Whatcom County of Washington state, United States. [2] It is set within North Cascades National Park and Stephen Mather Wilderness, where it is situated 1.7 mile north of The Roost and one mile south of Azure Lake. The nearest higher neighbor is McMillan Spire, 1.7 miles (2.7 km) to the north-northwest. [2] Glee Peak is part of the Picket Range which is a sub-range of the North Cascades, and like many North Cascades peaks, it is more notable for its large, steep rise above local terrain than for its absolute elevation. Topographic relief is significant as the northeast aspect rises 4,000 feet (1,200 meters) above Stetattle Creek in approximately one mile, and the southwest aspect rises 6,000 feet (1,800 meters) above Goodell Creek in three miles. Precipitation runoff from the mountain drains into these two creeks which are both tributaries of the Skagit River. Who made the first ascent of the summit is unknown, but Glee Davis and Burton Babcock were climbing in the immediate area as early as 1905. [3]

Contents

Etymology

Glee Davis, wife Hazel, and baby in 1918 Glee and Hazel Davis.jpg
Glee Davis, wife Hazel, and baby in 1918

Davis Peak, located three miles southeast of Glee Peak, is officially named for the pioneering Davis family, who settled in the Skagit Valley near the base of the mountain. [4] The family was led by Lucinda Davis, the mother of three children, who named her youngest son, Glee Davis (1885–1982). In his later years, Glee would have a homestead here and construct an electric generator on Stetattle Creek. [5] The homestead was lost when Seattle City Light had the land condemned for the purpose of building hydroelectric dams on the Skagit. He also worked for the Forest Service, and in 1917 he built one of the country's first fire lookout towers on nearby Sourdough Mountain after he built the Sourdough Mountain trail in 1916. [6] [7] Glee Peak is the unofficial name of this landform, and will remain unofficial as long as the USGS policy of not adopting new toponyms in designated wilderness areas stays in effect.

Geology

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. These climate differences lead to vegetation variety defining the ecoregions in this area.

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. [8] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. [8] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. [8]

During the Pleistocene period, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. [8] The U-shaped cross section of the river valleys is a result of recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.

Climate

Glee Peak is located in the marine west coast climate zone of western North America. [7] Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. [7] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. [7] 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. [7]

See also

Related Research Articles

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Mount Crowder is a remote 7,082-foot (2,159-metre) mountain summit in the Picket Range of the North Cascades, in Whatcom County of Washington state. Mount Crowder is situated in North Cascades National Park and Stephen Mather Wilderness. Neighbors include Mount Fury, 1.64 mi (2.64 km) to the northeast, and Twin Needles is set 2.3 mi (3.7 km) to the southeast. Precipitation runoff from this peak drains south into headwaters of Goodell Creek, and northwest into Picket Creek which is a tributary of the Baker River. Topographic relief is significant as the summit rises 4,300 feet above Goodell Creek in approximately one mile.

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

Mount Buckindy is a remote 7,320-foot-elevation (2,230-meter) mountain summit located in the North Cascades, in Skagit County of Washington state. It is the second-highest point of the Buckindy Range, or Buckindy Ridge. It is set in the Glacier Peak Wilderness on land managed by the Mount Baker-Snoqualmie National Forest. It is situated 20 miles east-northeast of Darrington, Washington, and 17 miles north-northwest of Glacier Peak which is one of the Cascade stratovolcanoes. Precipitation runoff from Mount Buckindy drains south to the Suiattle River via Buck Creek and Downey Creek, and north to the Cascade River via Kindy Creek. Topographic relief is significant as the summit rises 4,700 feet above Kindy Creek in less than two miles. The mountain's toponym is a portmanteau of Buck and Kindy Creeks, and has been officially adopted by the United States Board on Geographic Names.

<span class="mw-page-title-main">Little Devil Peak</span>

Little Devil Peak is a 6,985-foot-elevation (2,129 m) mountain summit located in Skagit County of Washington state. It is set within North Cascades National Park and Stephen Mather Wilderness, where it is situated 3.1 miles northeast of Lookout Mountain. Little Devil is the second-highest peak of Teebone Ridge, and other peaks on this ridge include line parent Big Devil Peak, Fallen Angel, and The Trapezoid. Precipitation runoff from the mountain drains into tributaries of the Skagit River. Like many North Cascades peaks, it is more notable for its large, steep rise above local terrain than for its absolute elevation. Topographic relief is significant as the south aspect rises 5,400 feet above Marble Creek in three miles, and the east aspect rises 4,200 feet above Newhalem Creek in approximately 1.5 mile.

References

  1. 1 2 3 "Glee Peak - 7,180' WA". listsofjohn.com. Retrieved 2022-04-02.
  2. 1 2 3 4 "Glee Peak, Washington". Peakbagger.com.
  3. Fred Beckey (1987), Cascade Alpine Guide: Columbia River to Stevens Pass, Mountaineers Books, p. 97
  4. Lucinda J. Davis - National Park Service
  5. Glee Davis, Pioneering in upper Skagit recalled by early settler Glee Davis, Bellingham Herald, June 26, 1953
  6. Erik Molvar (2019), Hiking the North Cascades: A Guide to More Than 100 Great Hiking Adventures, Falcon Guides, ISBN   9781493037087, p. 70
  7. 1 2 3 4 5 Beckey, Fred W. (1996). Cascade Alpine Guide, Volume 2: Stevens Pass to Rainy Pass (2nd ed.). ISBN   978-0-89886-838-8.
  8. 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.