Big Devil Peak

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Big Devil Peak
Big Devil Peak from Snowfield.jpg
Big Devil Peak from the northeast
Highest point
Elevation 7,055 ft (2,150 m) [1]
Prominence 1,655 ft (504 m) [1]
Isolation 5.32 mi (8.56 km) [2]
Coordinates 48°36′16″N121°17′37″W / 48.60444°N 121.29361°W / 48.60444; -121.29361 [1]
Geography
USA Washington relief location map.jpg
Red triangle with thick white border.svg
Big Devil Peak
Location in Washington
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Big Devil Peak
Big Devil Peak (the United States)
Big Devil Peak
Interactive map of Big Devil Peak
CountryUnited States
State Washington
County Skagit
Protected area North Cascades National Park
Parent range North Cascades
Cascade Range
Topo map USGS Big Devil Peak
Geology
Rock type Gneiss, Schist
Climbing
First ascent 1963 J. Haggerty, J. Roper [3]
Easiest route Climbing YDS 3

Big Devil Peak is a 7,055-foot-elevation (2,150 meter) mountain summit located in North Cascades National Park in Skagit County of Washington state. The peak lies midway between Marblemount and Newhalem and can be seen from the North Cascades Highway at the road pullout for Big Devil Falls. The peak rises 6,600+ feet above the valley floor at this viewing location in the valley. Big Devil is the highest peak of Teebone Ridge, and other peaks on this ridge include Little Devil Peak, Fallen Angel, and The Trapezoid. Precipitation runoff from the mountain drains into tributaries of the Skagit River.

Contents

Climate

Big Devil Peak is located in the marine west coast climate zone of western North America. [4] Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. [4] 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. [4]

Geology

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, spires, 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.

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. [5] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. [5] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. [5]

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. [5] 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.

See also

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<span class="mw-page-title-main">Little Devil Peak</span> Mountain in Skagit County, Washington, United States

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 "Big Devil Peak, Washington". Peakbagger.com.
  2. "Big Devil Peak - 7,055' WA". Lists of John. Retrieved 2021-01-30.
  3. Kenn Carpenter (1966) American Alpine Journal
  4. 1 2 3 Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  5. 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.