fbpx
Wikipedia

Sitting Bull Mountain

Sitting Bull Mountain is a 7,759-foot (2,365-metre) double summit mountain in the North Cascades of Washington state. The north summit is higher than the south peak (7680+ ft), and easier to climb (class 3 vs. class 4), however neither peak sees much climbing activity.[3] Sitting Bull Mountain is located 2.1 mi (3.4 km) northwest of Suiattle Pass in the heart of the Glacier Peak Wilderness. Its nearest higher peak is Plummer Mountain, 1.51 mi (2.43 km) to the south-southwest.[1] The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County. Precipitation runoff from Sitting Bull Mountain drains east into Agnes Creek which is a tributary of the Stehekin River, or west into Canyon Creek which is a tributary of the Suiattle River.

Sitting Bull Mountain
Sitting Bull Mountain seen from Cloudy Pass
Highest point
Elevation7,759 ft (2,365 m)[1]
Prominence599 ft (183 m)[1]
Parent peakPlummer Mountain 7870 ft[1]
Isolation1.53 mi (2.46 km)[2]
Coordinates48°13′39″N 120°57′34″W / 48.227595°N 120.959499°W / 48.227595; -120.959499[1]
Geography
Sitting Bull Mountain
Location in Washington state
Sitting Bull Mountain
Sitting Bull Mountain (the United States)
CountryUnited States
StateWashington
CountySnohomish / Chelan
Protected areaGlacier Peak Wilderness
Parent rangeCascade Range
Topo mapUSGS Suiattle Pass
Geology
Age of rockCretaceous
Mountain typeMetamorphic brown Gneiss
Climbing
First ascent1921 party of The Mountaineers[3]
Easiest routeScrambling[3]
Sitting Bull Mountain and Dome Peak seen from Spider Gap

Geology edit

Subduction and tectonic activity in the area began during the late cretaceous period, about 90 million years ago. The area was previously an oceanic environment, consisting mainly of sedimentary and volcanic rocks.[3] Extensive volcanic activity began to take place in the oligocene, about 35 million years ago.[4] However, mountain building in the area did not begin until the miocene, approximately 10 million years ago.[3] Sitting Bull Mountain is located in the Cloudy Pass batholith, an intrusive formation that was formed approximately 20 million years ago, during the early miocene.[3]Glacier Peak, a stratovolcano that is south of Sitting Bull Mountain, began forming in the mid-Pleistocene.[3] Due to Glacier Peak's proximity to Sitting Bull Mountain, volcanic ash is quite common in the area.

Throughout the ice age, the North Cascades were mostly covered in thick glaciers, extending to near Puget Sound. Glaciation was most prevalent approximately 18,000 years ago, and most valleys were ice-free by 12,000 years ago.[3] As a result, valleys in the area are deep and u-shaped, and mountains tend to be rocky, with steep slopes and narrow summits.

Climate edit

Sitting Bull Mountain 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.[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] The months of July through September offer the most favorable weather for viewing or climbing this peak.

See also edit

References edit

  1. ^ a b c d e "Sitting Bull Mountain, Washington". Peakbagger.com.
  2. ^ "Sitting Bull Mountain - 7,759' WA". Lists of John. Retrieved 2021-03-01.
  3. ^ a b c d e f g h i j k l m Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  4. ^ "North Cascades Geology". United States Geological Survey. Retrieved July 29, 2013.

External links edit

  • Sitting Bull Mountain: weather forecast

sitting, bull, mountain, foot, metre, double, summit, mountain, north, cascades, washington, state, north, summit, higher, than, south, peak, 7680, easier, climb, class, class, however, neither, peak, sees, much, climbing, activity, located, northwest, suiattl. Sitting Bull Mountain is a 7 759 foot 2 365 metre double summit mountain in the North Cascades of Washington state The north summit is higher than the south peak 7680 ft and easier to climb class 3 vs class 4 however neither peak sees much climbing activity 3 Sitting Bull Mountain is located 2 1 mi 3 4 km northwest of Suiattle Pass in the heart of the Glacier Peak Wilderness Its nearest higher peak is Plummer Mountain 1 51 mi 2 43 km to the south southwest 1 The mountain is situated on the crest of the Cascade Range on the shared border of Snohomish County and Chelan County Precipitation runoff from Sitting Bull Mountain drains east into Agnes Creek which is a tributary of the Stehekin River or west into Canyon Creek which is a tributary of the Suiattle River Sitting Bull MountainSitting Bull Mountain seen from Cloudy PassHighest pointElevation7 759 ft 2 365 m 1 Prominence599 ft 183 m 1 Parent peakPlummer Mountain 7870 ft 1 Isolation1 53 mi 2 46 km 2 Coordinates48 13 39 N 120 57 34 W 48 227595 N 120 959499 W 48 227595 120 959499 1 GeographySitting Bull MountainLocation in Washington stateShow map of Washington state Sitting Bull MountainSitting Bull Mountain the United States Show map of the United StatesCountryUnited StatesStateWashingtonCountySnohomish ChelanProtected areaGlacier Peak WildernessParent rangeCascade RangeTopo mapUSGS Suiattle PassGeologyAge of rockCretaceousMountain typeMetamorphic brown GneissClimbingFirst ascent1921 party of The Mountaineers 3 Easiest routeScrambling 3 Sitting Bull Mountain and Dome Peak seen from Spider Gap Contents 1 Geology 2 Climate 3 See also 4 References 5 External linksGeology editSubduction and tectonic activity in the area began during the late cretaceous period about 90 million years ago The area was previously an oceanic environment consisting mainly of sedimentary and volcanic rocks 3 Extensive volcanic activity began to take place in the oligocene about 35 million years ago 4 However mountain building in the area did not begin until the miocene approximately 10 million years ago 3 Sitting Bull Mountain is located in the Cloudy Pass batholith an intrusive formation that was formed approximately 20 million years ago during the early miocene 3 Glacier Peak a stratovolcano that is south of Sitting Bull Mountain began forming in the mid Pleistocene 3 Due to Glacier Peak s proximity to Sitting Bull Mountain volcanic ash is quite common in the area Throughout the ice age the North Cascades were mostly covered in thick glaciers extending to near Puget Sound Glaciation was most prevalent approximately 18 000 years ago and most valleys were ice free by 12 000 years ago 3 As a result valleys in the area are deep and u shaped and mountains tend to be rocky with steep slopes and narrow summits Climate editSitting Bull Mountain 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 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 The months of July through September offer the most favorable weather for viewing or climbing this peak See also edit nbsp Mountains portalGeography of the North Cascades Geology of the Pacific Northwest Glacier Peak WildernessReferences edit a b c d e Sitting Bull Mountain Washington Peakbagger com Sitting Bull Mountain 7 759 WA Lists of John Retrieved 2021 03 01 a b c d e f g h i j k l m Beckey Fred W Cascade Alpine Guide Climbing and High Routes Seattle WA Mountaineers Books 2008 North Cascades Geology United States Geological Survey Retrieved July 29 2013 External links editSitting Bull Mountain weather forecast Retrieved from https en wikipedia org w index php title Sitting Bull Mountain amp oldid 1217791189, 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.