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Majestic Mountain

Majestic Mountain is a 7,530-foot-elevation (2,300-meter) mountain summit located in Whatcom County in Washington state.[1]

Majestic Mountain
Majestic's north peak (right)
Camera pointed southwest
Highest point
Elevation7,530 ft (2,295 m)[1]
Prominence720 ft (220 m)[2]
Parent peakMount Ballard (8,340 ft)[2]
Isolation1.75 mi (2.82 km)[3]
Coordinates48°41′09″N 120°48′00″W / 48.6859330°N 120.7999491°W / 48.6859330; -120.7999491[1]
Dimensions
Length5 mi (8.0 km) North-South
Width2 mi (3.2 km) East-West
Geography
Majestic Mountain
Location in Washington
Majestic Mountain
Majestic Mountain (the United States)
LocationWhatcom County, Washington, U.S.
Parent rangeCascade Range
North Cascades
Okanogan Range[2]
Topo mapUSGS Azurite Peak
Climbing
Easiest routeclass 2

Description edit

Majestic Mountain is part of the Okanogan Range which is a sub-range of the North Cascades, and is situated on land administered by the Okanogan–Wenatchee National Forest.[2] The mountain is a long ridge paralleling Mill Creek, and has several subpeaks, the highest of which is the North Peak (7,510 ft).[2] The nearest higher peak is Mount Ballard, 1.9 miles (3.1 km) to the east.[2] Topographic relief is significant as the summit rises 3,300 feet (1,000 meters) above Mill Creek in approximately three-quarters mile. Precipitation runoff from the mountain drains to Ross Lake via Mill Creek and other tributaries of the Skagit River. The Azurite Mine, a gold and silver mine, was located east of the summit along Mill Creek, and over $900,000 in gold was extracted there in the 1930s.[4] The Gold Hill Mine, located on the southwest slope in the East Creek valley, and the North American Mine at the north end of the mountain also produced gold and silver.

Climate edit

Majestic Mountain is located in the marine west coast climate zone of western North America.[5] Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach the North Cascades, 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 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 avalanche danger.[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]

Geology edit

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks and 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.[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

Geography of the North Cascades

References edit

  1. ^ a b c "Majestic Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2012-04-08.
  2. ^ a b c d e f "Majestic Mountain, Washington". Peakbagger.com.
  3. ^ "Majestic Mountain - 7,540' WA". listsofjohn.com. Retrieved 2022-04-08.
  4. ^ Erik Molvar (2009), Hiking the North Cascades: A Guide to More Than 100 Great Hiking Adventures, Falcon Guides, ISBN 9780762757749, p. 271
  5. ^ a b c Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  6. ^ a b c d Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.

External links edit

  • Weather forecast: Majestic Mountain
  • Majestic from McKay Ridge (photo): Flickr

majestic, mountain, this, article, about, mountain, united, states, mountain, jasper, national, park, alberta, foot, elevation, meter, mountain, summit, located, whatcom, county, washington, state, majestic, north, peak, right, camera, pointed, southwesthighes. This article is about a mountain in the United States For the mountain in Jasper National Park see Majestic Mountain Alberta Majestic Mountain is a 7 530 foot elevation 2 300 meter mountain summit located in Whatcom County in Washington state 1 Majestic MountainMajestic s north peak right Camera pointed southwestHighest pointElevation7 530 ft 2 295 m 1 Prominence720 ft 220 m 2 Parent peakMount Ballard 8 340 ft 2 Isolation1 75 mi 2 82 km 3 Coordinates48 41 09 N 120 48 00 W 48 6859330 N 120 7999491 W 48 6859330 120 7999491 1 DimensionsLength5 mi 8 0 km North SouthWidth2 mi 3 2 km East WestGeographyMajestic MountainLocation in WashingtonShow map of Washington state Majestic MountainMajestic Mountain the United States Show map of the United StatesLocationWhatcom County Washington U S Parent rangeCascade RangeNorth CascadesOkanogan Range 2 Topo mapUSGS Azurite PeakClimbingEasiest routeclass 2 Contents 1 Description 2 Climate 3 Geology 4 See also 5 References 6 External linksDescription editMajestic Mountain is part of the Okanogan Range which is a sub range of the North Cascades and is situated on land administered by the Okanogan Wenatchee National Forest 2 The mountain is a long ridge paralleling Mill Creek and has several subpeaks the highest of which is the North Peak 7 510 ft 2 The nearest higher peak is Mount Ballard 1 9 miles 3 1 km to the east 2 Topographic relief is significant as the summit rises 3 300 feet 1 000 meters above Mill Creek in approximately three quarters mile Precipitation runoff from the mountain drains to Ross Lake via Mill Creek and other tributaries of the Skagit River The Azurite Mine a gold and silver mine was located east of the summit along Mill Creek and over 900 000 in gold was extracted there in the 1930s 4 The Gold Hill Mine located on the southwest slope in the East Creek valley and the North American Mine at the north end of the mountain also produced gold and silver Climate editMajestic Mountain is located in the marine west coast climate zone of western North America 5 Most weather fronts originate in the Pacific Ocean and travel east toward the Cascade Mountains As fronts approach the North Cascades 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 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 avalanche danger 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 Geology editThe North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks and 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 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 portalGeography of the North CascadesReferences edit a b c Majestic Mountain Geographic Names Information System United States Geological Survey United States Department of the Interior Retrieved 2012 04 08 a b c d e f Majestic Mountain Washington Peakbagger com Majestic Mountain 7 540 WA listsofjohn com Retrieved 2022 04 08 Erik Molvar 2009 Hiking the North Cascades A Guide to More Than 100 Great Hiking Adventures Falcon Guides ISBN 9780762757749 p 271 a b c Beckey Fred W Cascade Alpine Guide Climbing and High Routes Seattle WA Mountaineers Books 2008 a b c d Kruckeberg Arthur 1991 The Natural History of Puget Sound Country University of Washington Press External links editWeather forecast Majestic Mountain Majestic from McKay Ridge photo Flickr Retrieved from https en wikipedia org w index php title Majestic Mountain amp oldid 1194008675, wikipedia, wiki, book, books, library,

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