Porcupine Peak (Washington)

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Porcupine Peak
Porcupine Peak 7762 North Cascades.jpg
Porcupine Peak from eastbound North Cascades Highway
Highest point
Elevation 7,762 ft (2,366 m) [1]
Prominence 922 ft (281 m) [1]
Parent peak Peak 7865 [2]
Isolation 2.19 mi (3.52 km) [1]
Coordinates 48°33′01″N120°44′12″W / 48.550271°N 120.736653°W / 48.550271; -120.736653 [1]
Geography
USA Washington relief location map.jpg
Red triangle with thick white border.svg
Porcupine Peak
Location in Washington
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Porcupine Peak
Porcupine Peak (the United States)
CountryUnited States
State Washington
County Skagit
Parent range North Cascades
Topo map USGS Washington Pass
Geology
Type of rock Granite
Climbing
Easiest route Scrambling, class 3

Porcupine Peak is a 7,762-foot-elevation (2,366-meter) mountain located in Skagit County of Washington state.

Contents

Description

Porcupine Peak is part of the Okanogan Range which is a sub-range of the North Cascades Range. [1] It is situated north of Rainy Pass and south of Mount Hardy on land administered by the Okanogan–Wenatchee National Forest. The nearest higher peak is Cutthroat Peak, 2.19 miles (3.52 km) to the southeast. [1] Porcupine Peak can be seen from the North Cascades Highway which follows below the southwest slopes of the mountain. Precipitation runoff from the mountain drains into the Porcupine Creek, Swamp Creek, and Granite Creek. These three creeks, which nearly encircle the mountain, ultimately empty to the Skagit River. Topographic relief is significant as the summit rises 3,600 feet (1,100 meters) above Granite Creek in 1.3 mile (2.1 km).

Climate

Porcupine Peak is located in the marine west coast climate zone of western North America. [3] Most 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 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, 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. [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

Related Research Articles

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Tatie Peak is a 7,386-foot (2,251-metre) mountain summit located on the shared border between Okanogan County and Whatcom County in Washington state. It is part of the Okanogan Range, which is a sub-range of the North Cascades. The mountain is situated 2.6 miles (4.2 km) east of Mount Ballard, and 3.3 miles (5.3 km) south of Slate Peak, on land managed by the Okanogan–Wenatchee National Forest. The nearest higher neighbor is Syncline Mountain, 0.8 miles (1.3 km) to the south-southwest. The Pacific Crest Trail traverses the south slope of the peak, with an easy off-trail scramble to reach the summit. Precipitation runoff from Tatie Peak drains south into Trout Creek which is a tributary of the Methow River, or northwest into Slate Creek, which is part of the Skagit River drainage basin.

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

Syncline Mountain is a 7,560-foot (2,300-metre) mountain summit located on the shared border between Okanogan County and Whatcom County in Washington state. It is part of the Okanogan Range, which is a sub-range of the North Cascades, and is situated on land managed by the Okanogan–Wenatchee National Forest. Its nearest neighbor is Tatie Peak, 0.8 miles (1.3 km) to the north, and the nearest higher neighbor is Mount Ballard, 2.1 miles (3.4 km) to the west. The Pacific Crest Trail traverses the east slope of the peak, with an off-trail scramble to reach the summit. Precipitation runoff from Syncline Mountain drains east into Trout Creek which is a tributary of the Methow River, or northwest into Slate Creek, which is part of the Skagit River drainage basin. This unofficially named mountain features a conspicuous syncline, hence its descriptive name.

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

Le Conte Mountain is a 7,762-foot-elevation (2,366-meter) summit located on the shared boundary of Skagit County and Chelan County in Washington state. It is positioned on the crest of the North Cascades Range, and is set within the Glacier Peak Wilderness. Le Conte Mountain is situated on the shared border of Mount Baker-Snoqualmie National Forest and Okanogan-Wenatchee National Forest. Access to the peak is via the Ptarmigan Traverse. The nearest higher neighbor is Sentinel Peak, 1.87 miles (3.01 km) to the south-southeast, and Spider Mountain is 2.4 miles (3.9 km) to the northeast. The Le Conte Glacier and South Cascade Glacier lie to the south of the peak. Precipitation runoff on the east side the mountain drains into Flat Creek which is a tributary of the Stehekin River, while precipitation drains into headwaters of the South Fork Cascade River from the west side. Topographic relief is significant as the southwest aspect rises nearly 2,500 feet above South Cascade Lake in less than one-half mile, and the northeast aspect rises 3,200 feet above Flat Creek in one mile.

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

Majestic Mountain is a 7,530-foot-elevation (2,300-meter) mountain summit located in Whatcom County in Washington state.

References

  1. 1 2 3 4 5 6 "Porcupine Peak, Washington". Peakbagger.com.
  2. "Porcupine Peak - 7,762' WA". listsofjohn.com. Retrieved 2023-08-05.
  3. Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  4. 1 2 Beckey, p. 16
  5. 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.