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Edward Peak

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Mountain in Washington (state), United States
Edward Peak
Edward Peak centered, north aspect  
Highest point
Elevation7,280 ft (2,219 m)
Prominence480 ft (150 m)
Parent peakThree Musketeers Ridge (7,700 ft)
Isolation1.15 mi (1.85 km)
Coordinates47°30′56″N 120°45′27″W / 47.5155979°N 120.7575874°W / 47.5155979; -120.7575874
Geography
Edward Peak is located in Washington (state)Edward PeakEdward PeakLocation in WashingtonShow map of Washington (state)Edward Peak is located in the United StatesEdward PeakEdward PeakEdward Peak (the United States)Show map of the United States
LocationChelan County
Washington state, U.S.
Parent rangeStuart Range
Wenatchee Mountains
Cascade Range
Topo mapUSGS Cashmere Mountain
Geology
Rock ageLate Cretaceous
Rock typeTonalitic pluton
Climbing
First ascent1948 by Fred Beckey
Easiest routeclass 5.7 Climbing

Edward Peak, also known as The Mole, is a 7,280-foot (2,219-metre) granite summit located in Chelan County of Washington state. It is set within the Alpine Lakes Wilderness, on land managed by Okanogan-Wenatchee National Forest. Edward Peak belongs to the Stuart Range which is a subset of the Cascade Range. It is situated 1.9 miles (3.1 km) north of The Temple, and the nearest town is Leavenworth, 7 miles (11 km) to the northeast. Precipitation runoff from the mountain drains north into Icicle Creek via Rat Creek.

Climbing

The first ascent of the summit was made in May 1948 by Fred Beckey, Wesley Grande, and Ralph Widrig via the south face. This party named the peak "The Mole".

Other established climbing routes:

  • West Face – 1957 – class 5.7 – Patrik Callis, James Fraser, Gerry Honey
  • East Corner – 1957 – class 5.8 – Fred Beckey, Bob Lewis
  • North Face – 1962 – class 5.7 – Don Gordon, Patrik Callis, Eric Bjornstad, Dan Davis
  • Southwest Rib – 1980 – class 5.9 – Pete Doorish, Bob Crawford

 

Climate

Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach, 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 Cascades experience high precipitation, especially during the winter months in the form of snowfall. 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.

Geology

The Alpine Lakes Wilderness features some of the most rugged topography in the Cascade Range with craggy peaks and ridges, deep glacial valleys, and granite walls spotted with over 700 mountain lakes.  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. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving  deposits of rock debris. The last glacial retreat in the Alpine Lakes area began about 14,000 years ago and was north of the Canada–US border by 10,000 years ago. The U-shaped cross section of the river valleys is a result of that 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 Alpine Lakes Wilderness area.

See also

Gallery

  • Edward Peak viewed from Prusik Pass Edward Peak viewed from Prusik Pass
  • Southwest aspect, as seen from Little Annapurna Southwest aspect, as seen from Little Annapurna
  • Edward Peak centered, from the north Edward Peak centered, from the north

References

  1. ^ "Edward Peak, Washington". Peakbagger.com.
  2. ^ Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  3. ^ "Edward Peak - 7,300' WA". listsofjohn.com. Retrieved 2021-10-24.
  4. ^ "Edward Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2021-10-22.
  5. ^ Geologic map of the North Cascade Range, Washington, Haugerud, R.A., and Tabor, R.W., US Geological Survey, 2009.
  6. Jim Nelson, Peter Potterfield, Selected Climbs in the Cascades Vol 2, 2nd Ed., The Mountaineers Books, ISBN 9781594853890, page 80.
  7. Fred Beckey, 2012, Challenge of the North Cascades, Mountaineers Books, ISBN 9781594853760, chapter 11.
  8. Smoot, Jeff (2004). Backpacking Washington's Alpine Lakes Wilderness. Helena, Montana: The Globe Pequot Press.
  9. ^ Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.

External links

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