fbpx
Wikipedia

Goat Mountain (Whatcom County)

Goat Mountain is a 6,844-foot (2,086-metre) summit in the Skagit Range which is a subset of the North Cascades of Washington state.[4] It is located south of Mount Larrabee and north of Mount Shuksan in the Mount Baker Wilderness, which is managed by the Mount Baker-Snoqualmie National Forest. Goat Mountain has a subsidiary 6,725 ft summit known as the west peak, and remnants of what was colloquially known as the Swamp Creek Glacier rest on the northern slope between the two summits. The nearest higher neighbor is Mount Chardonnay, 2.75 mi (4.43 km) to the east.[1] The Silver Tip Mine was located on the south slope of the mountain near the 3,000 ft level. The mine produced silver and gold in the 1940s.[5] Precipitation runoff from the mountain drains into tributaries of the Fraser River and the Nooksack River.

Goat Mountain
Goat Mountain from Winchester Mountain Lookout
Highest point
Elevation6,844 ft (2,086 m) NAVD 88[1]
Prominence1,599 ft (487 m)[1]
Parent peakMount Chardonnay (7,020 ft)[2]
Isolation2.75 mi (4.43 km)[2]
Coordinates48°55′43″N 121°37′35″W / 48.928483°N 121.626352°W / 48.928483; -121.626352[1]
Geography
Goat Mountain
Location in Washington
Goat Mountain
Location in the United States
CountryUnited States
StateWashington
CountyWhatcom
Protected areaMount Baker Wilderness
Parent rangeCascade Range
North Cascades
Topo mapUSGS Mount Larrabee/Mount Sefrit
Geology
Type of rockDarrington Phyllite[3]
Climbing
First ascent1904, Frank Calkins and George Otis Smith[3]
Easiest routeScramble

Climate edit

Goat Mountain is 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 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.[3] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[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] 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] 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] The rock of Goat Mountain is Darrington Phyllite of the Easton terrane.

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

Gallery edit

References edit

  1. ^ a b c d "Goat Mountain, Washington". Peakbagger.com. Retrieved 2018-09-02.
  2. ^ a b "Goat Mountain, East - 6,860' WA". listsofjohn.com. Retrieved 2020-06-28.
  3. ^ a b c d e f g Beckey, Fred W. (2008). Cascade Alpine Guide (3rd ed.). Mountaineers Books.
  4. ^ "Goat Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2018-09-02.
  5. ^ Silver Tip Mine westernmininghistory.com
  6. ^ a b c d Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.

External links edit

  • Mt. Baker Wilderness U.S. Forest Service

goat, mountain, whatcom, county, goat, mountain, foot, metre, summit, skagit, range, which, subset, north, cascades, washington, state, located, south, mount, larrabee, north, mount, shuksan, mount, baker, wilderness, which, managed, mount, baker, snoqualmie, . Goat Mountain is a 6 844 foot 2 086 metre summit in the Skagit Range which is a subset of the North Cascades of Washington state 4 It is located south of Mount Larrabee and north of Mount Shuksan in the Mount Baker Wilderness which is managed by the Mount Baker Snoqualmie National Forest Goat Mountain has a subsidiary 6 725 ft summit known as the west peak and remnants of what was colloquially known as the Swamp Creek Glacier rest on the northern slope between the two summits The nearest higher neighbor is Mount Chardonnay 2 75 mi 4 43 km to the east 1 The Silver Tip Mine was located on the south slope of the mountain near the 3 000 ft level The mine produced silver and gold in the 1940s 5 Precipitation runoff from the mountain drains into tributaries of the Fraser River and the Nooksack River Goat MountainGoat Mountain from Winchester Mountain LookoutHighest pointElevation6 844 ft 2 086 m NAVD 88 1 Prominence1 599 ft 487 m 1 Parent peakMount Chardonnay 7 020 ft 2 Isolation2 75 mi 4 43 km 2 Coordinates48 55 43 N 121 37 35 W 48 928483 N 121 626352 W 48 928483 121 626352 1 GeographyGoat MountainLocation in WashingtonShow map of Washington state Goat MountainLocation in the United StatesShow map of the United StatesCountryUnited StatesStateWashingtonCountyWhatcomProtected areaMount Baker WildernessParent rangeCascade RangeNorth CascadesTopo mapUSGS Mount Larrabee Mount SefritGeologyType of rockDarrington Phyllite 3 ClimbingFirst ascent1904 Frank Calkins and George Otis Smith 3 Easiest routeScramble Contents 1 Climate 2 Geology 3 See also 4 Gallery 5 References 6 External linksClimate editGoat Mountain is 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 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 3 Because of maritime influence snow tends to be wet and heavy resulting in high avalanche danger 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 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 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 The rock of Goat Mountain is Darrington Phyllite of the Easton terrane 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 portalGeography of the North CascadesGallery edit nbsp Goat Mountain with Mt Larrabee to left nbsp Twin Lakes bottom Goat Mountain upper right nbsp Goat Mountain to right American Border Peak and Mount Larrabee to left Slesse centered References edit a b c d Goat Mountain Washington Peakbagger com Retrieved 2018 09 02 a b Goat Mountain East 6 860 WA listsofjohn com Retrieved 2020 06 28 a b c d e f g Beckey Fred W 2008 Cascade Alpine Guide 3rd ed Mountaineers Books Goat Mountain Geographic Names Information System United States Geological Survey United States Department of the Interior Retrieved 2018 09 02 Silver Tip Mine westernmininghistory com a b c d Kruckeberg Arthur 1991 The Natural History of Puget Sound Country University of Washington Press External links editMt Baker Wilderness U S Forest Service Retrieved from https en wikipedia org w index php title Goat Mountain Whatcom County amp oldid 1217493886, wikipedia, wiki, book, books, library,

article

, read, download, free, free download, mp3, video, mp4, 3gp, jpg, jpeg, gif, png, picture, music, song, movie, book, game, games.