Diobsud Buttes

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Diobsud Buttes
Diobsud Buttes seen from North Cascades Highway.jpg
Diobsud Buttes seen from North Cascades Highway
Highest point
Elevation 5,892 ft (1,796 m) [1]
Prominence 852 ft (260 m) [1]
Coordinates 48°37′08″N121°28′37″W / 48.618893°N 121.476845°W / 48.618893; -121.476845 [1]
Geography
USA Washington relief location map.jpg
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Diobsud Buttes
Location in Washington
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Diobsud Buttes
Diobsud Buttes (the United States)
Diobsud Buttes
Interactive map of Diobsud Buttes
CountryUnited States
State Washington
County Skagit
Protected area North Cascades National Park
Noisy-Diobsud Wilderness
Parent range Cascade Range
Topo map USGS Marblemount
Geology
Rock age Early Cretaceous [2]
Rock type Greenschist [2]
Climbing
Easiest route Scrambling

Diobsud Buttes are summits near the western edge of the North Cascades, in Skagit County of Washington state. Diobsud Buttes are located north of Marblemount, Washington, and Helen Buttes, along the shared boundary of North Cascades National Park and the Noisy-Diobsud Wilderness. The nearest higher neighbor is Logger Butte, 0.85 mi (1.37 km) to the north. [1] Precipitation runoff from Diobsud Buttes drains into tributaries of the Skagit River.

Contents

Climate

Diobsud Buttes are located in the marine west coast climate zone of western North America. [3] Weather fronts originating in the Pacific Ocean 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 snow 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. [3] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. [3] 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. [3] Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below 0 °F (−18 °C) or above 80 °F (27 °C). [3]

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. [4] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. [4] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. [4]

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. [4] 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.

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References

  1. 1 2 3 4 "Diobsud Buttes, Washington". Peakbagger.com.
  2. 1 2 Geologic map of the North Cascade Range, Washington, Haugerud, R.A., and Tabor, R.W., US Geological Survey, 2009.
  3. 1 2 3 4 5 Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  4. 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.