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Pocket Peak

Pocket Peak is a 7,056-foot (2,151-metre) mountain summit located in the Skagit Range, which is a subset of the North Cascades in Whatcom County of Washington state. It is situated immediately west of Pocket Lake, and 4 mi (6.4 km) east of Mount Larrabee in the Mount Baker Wilderness, which is managed by Mount Baker-Snoqualmie National Forest. Pocket Peak is set on the Slesse Divide, 0.7 mile south of the Canada–United States border. Its nearest higher neighbor is Rapid Peak, 2.24 mi (3.60 km) to the southeast, North Big Bosom Butte is 2.5 miles to the southwest, and Slesse Mountain is set 3.24 mi (5.21 km) to the northwest.[1] Other peaks which can be seen from the summit include Mount Baker, Mount Shuksan, American Border Peak, Mount Chardonnay, Mount Rexford, and many more. This unofficially named peak is named in association with officially named Pocket Lake.[4] Precipitation runoff from this mountain drains into Silesia and Ensawkwatch Creeks, which are both tributaries of the Chilliwack River.

Pocket Peak
Pocket Peak, west aspect
Highest point
Elevation7,056 ft (2,151 m)[1]
Prominence1,136 ft (346 m)[1]
Parent peakRapid Peak (7,259 ft)[2]
Isolation2.25 mi (3.62 km)[3]
Coordinates48°59′22″N 121°33′06″W / 48.989555°N 121.551753°W / 48.989555; -121.551753[1]
Geography
Pocket Peak
Location in Washington
Pocket Peak
Pocket Peak (the United States)
Location
Parent rangeCascade Range
North Cascades
Skagit Range
Topo mapUSGS Mount Sefrit
Climbing
First ascent1967 D. McKeever, R. Tabor[2]
Easiest routeclass 4 scrambling[3]

Climate edit

Pocket Peak is located in the marine west coast climate zone of western North America.[5] This climate supports a pocket glacier on its north slope.[2] 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.[5] 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).[5] 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.[5] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[5] The months July through September offer the most favorable weather for viewing or climbing this peak.

Geology edit

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.

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.[6] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[6] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[6]

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.[6] 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 edit

 
Slesse left, Rexford distant center, Pocket right

References edit

  1. ^ a b c d "Pocket Peak, Washington". Peakbagger.com. Retrieved 2020-07-25.
  2. ^ a b c "Pocket Peak". Bivouac.com. Retrieved 2020-07-25.
  3. ^ a b ""Pocket Peak" - 7,056' WA". listsofjohn.com. Retrieved 2020-07-25.
  4. ^ "Pocket Lake". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2020-07-25.
  5. ^ a b c d e Beckey, Fred W. (2008). Cascade Alpine Guide (3rd ed.). Mountaineers Books.
  6. ^ a b c d Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.

External links edit

  • Pocket Peak: National Weather Service Forecast
  • Mt. Baker Wilderness U.S. Forest Service

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Pocket Peak is a 7 056 foot 2 151 metre mountain summit located in the Skagit Range which is a subset of the North Cascades in Whatcom County of Washington state It is situated immediately west of Pocket Lake and 4 mi 6 4 km east of Mount Larrabee in the Mount Baker Wilderness which is managed by Mount Baker Snoqualmie National Forest Pocket Peak is set on the Slesse Divide 0 7 mile south of the Canada United States border Its nearest higher neighbor is Rapid Peak 2 24 mi 3 60 km to the southeast North Big Bosom Butte is 2 5 miles to the southwest and Slesse Mountain is set 3 24 mi 5 21 km to the northwest 1 Other peaks which can be seen from the summit include Mount Baker Mount Shuksan American Border Peak Mount Chardonnay Mount Rexford and many more This unofficially named peak is named in association with officially named Pocket Lake 4 Precipitation runoff from this mountain drains into Silesia and Ensawkwatch Creeks which are both tributaries of the Chilliwack River Pocket PeakPocket Peak west aspectHighest pointElevation7 056 ft 2 151 m 1 Prominence1 136 ft 346 m 1 Parent peakRapid Peak 7 259 ft 2 Isolation2 25 mi 3 62 km 3 Coordinates48 59 22 N 121 33 06 W 48 989555 N 121 551753 W 48 989555 121 551753 1 GeographyPocket PeakLocation in WashingtonShow map of Washington state Pocket PeakPocket Peak the United States Show map of the United StatesLocationMount Baker WildernessWhatcom County Washington U S Parent rangeCascade RangeNorth CascadesSkagit RangeTopo mapUSGS Mount SefritClimbingFirst ascent1967 D McKeever R Tabor 2 Easiest routeclass 4 scrambling 3 Contents 1 Climate 2 Geology 3 See also 4 References 5 External linksClimate editPocket Peak is located in the marine west coast climate zone of western North America 5 This climate supports a pocket glacier on its north slope 2 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 5 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 5 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 5 Because of maritime influence snow tends to be wet and heavy resulting in high avalanche danger 5 The months July through September offer the most favorable weather for viewing or climbing this peak Geology editThe 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 The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch 6 With the North American Plate overriding the Pacific Plate episodes of volcanic igneous activity persisted 6 In addition small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago 6 During the Pleistocene period dating back over two million years ago glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris 6 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 edit nbsp Mountains portal Geology of the Pacific Northwest Geography of the North Cascades nbsp Slesse left Rexford distant center Pocket rightReferences edit a b c d Pocket Peak Washington Peakbagger com Retrieved 2020 07 25 a b c Pocket Peak Bivouac com Retrieved 2020 07 25 a b Pocket Peak 7 056 WA listsofjohn com Retrieved 2020 07 25 Pocket Lake Geographic Names Information System United States Geological Survey United States Department of the Interior Retrieved 2020 07 25 a b c d e Beckey Fred W 2008 Cascade Alpine Guide 3rd ed Mountaineers Books a b c d Kruckeberg Arthur 1991 The Natural History of Puget Sound Country University of Washington Press External links editPocket Peak National Weather Service Forecast Mt Baker Wilderness U S Forest Service Retrieved from https en wikipedia org w index php title Pocket Peak amp oldid 1194031646, wikipedia, wiki, book, books, library,

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