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Spark Plug Mountain

Spark Plug Mountain is a 6,320-foot (1,926-metre) mountain summit located above the western shore of Glacier Lake, in eastern King County of Washington state.[4] It's part of the Wenatchee Mountains, which are a subset of the Cascade Range, and is situated in the Alpine Lakes Wilderness, on land managed by Mount Baker-Snoqualmie National Forest.[1] The nearest higher neighbor is Surprise Mountain, 1.0 mi (1.6 km) to the southeast, and Thunder Mountain is set above the eastern shore of Glacier Lake.[1] The Pacific Crest Trail skirts this lake as it passes between Spark Plug and Thunder. Spark Plug Lake, elevation 5,587-ft, lies immediately below the north aspect of the mountain, and Little Spark Plug is the 6,016-ft peak on the north side of this lake. Precipitation runoff from the mountain drains into Surprise Creek and Deception Creek, both tributaries of the Skykomish River.

Spark Plug Mountain
East aspect, above Glacier Lake
Highest point
Elevation6,320 ft (1,926 m)[1][2]
Prominence440 ft (134 m)[1]
Parent peakSurprise Mountain (6,330 ft)[3]
Isolation1.0 mi (1.6 km)[3]
Coordinates47°39′34″N 121°09′23″W / 47.659446°N 121.156376°W / 47.659446; -121.156376[1]
Geography
Spark Plug Mountain
Location in Washington
Spark Plug Mountain
Spark Plug Mountain (the United States)
CountryUnited States
StateWashington
CountyKing
Protected areaAlpine Lakes Wilderness
Parent rangeNorth Wenatchee Mountains[1]
Cascade Range
Topo mapUSGS Scenic
Climbing
Easiest routescrambling

Climate edit

Spark Plug Mountain is located in the marine west coast climate zone of western North America.[2] Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snow onto the Cascades (Orographic lift). As a result, the west side of the 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.[2] During the 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.[2] The months of July through September offer the most favorable weather for viewing or climbing this peak.

Geology edit

The Alpine Lakes Wilderness features some of the most rugged topography in the Cascade Range with craggy peaks and ridges, deep glacial valleys, and granite walls spotted with over 700 mountain lakes.[5] 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 and shaped the landscape.[6] The last glacial retreat in the Alpine Lakes area began about 14,000 years ago and was north of the Canada–US border by 10,000 years ago.[6] The U-shaped cross section of the river valleys is a result of that 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 Alpine Lakes Wilderness rea.

See also edit

Gallery edit

References edit

  1. ^ a b c d e f "Spark Plug Mountain, Washington". Peakbagger.com.
  2. ^ a b c d Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  3. ^ a b "Spark Plug Mountain - 6,311' WA". listsofjohn.com. Retrieved 2020-07-19.
  4. ^ "Spark Plug Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2020-07-19.
  5. ^ Smoot, Jeff (2004). Backpacking Washington's Alpine Lakes Wilderness. Helena, Montana: The Globe Pequot Press.
  6. ^ a b c d e Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.

External links edit

  • Weather forecast: Spark Plug Mountain
  • Alpine Lakes Wilderness (Mt. Baker-Snoqualmie National Forest) U.S. Forest Service

spark, plug, mountain, foot, metre, mountain, summit, located, above, western, shore, glacier, lake, eastern, king, county, washington, state, part, wenatchee, mountains, which, subset, cascade, range, situated, alpine, lakes, wilderness, land, managed, mount,. Spark Plug Mountain is a 6 320 foot 1 926 metre mountain summit located above the western shore of Glacier Lake in eastern King County of Washington state 4 It s part of the Wenatchee Mountains which are a subset of the Cascade Range and is situated in the Alpine Lakes Wilderness on land managed by Mount Baker Snoqualmie National Forest 1 The nearest higher neighbor is Surprise Mountain 1 0 mi 1 6 km to the southeast and Thunder Mountain is set above the eastern shore of Glacier Lake 1 The Pacific Crest Trail skirts this lake as it passes between Spark Plug and Thunder Spark Plug Lake elevation 5 587 ft lies immediately below the north aspect of the mountain and Little Spark Plug is the 6 016 ft peak on the north side of this lake Precipitation runoff from the mountain drains into Surprise Creek and Deception Creek both tributaries of the Skykomish River Spark Plug MountainEast aspect above Glacier LakeHighest pointElevation6 320 ft 1 926 m 1 2 Prominence440 ft 134 m 1 Parent peakSurprise Mountain 6 330 ft 3 Isolation1 0 mi 1 6 km 3 Coordinates47 39 34 N 121 09 23 W 47 659446 N 121 156376 W 47 659446 121 156376 1 GeographySpark Plug MountainLocation in WashingtonShow map of Washington state Spark Plug MountainSpark Plug Mountain the United States Show map of the United StatesCountryUnited StatesStateWashingtonCountyKingProtected areaAlpine Lakes WildernessParent rangeNorth Wenatchee Mountains 1 Cascade RangeTopo mapUSGS ScenicClimbingEasiest routescrambling Contents 1 Climate 2 Geology 3 See also 4 Gallery 5 References 6 External linksClimate editSpark Plug Mountain is located in the marine west coast climate zone of western North America 2 Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains As fronts approach they are forced upward by the peaks of the Cascade Range causing them to drop their moisture in the form of rain or snow onto the Cascades Orographic lift As a result the west side of the 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 2 During the 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 2 The months of July through September offer the most favorable weather for viewing or climbing this peak Geology editThe Alpine Lakes Wilderness features some of the most rugged topography in the Cascade Range with craggy peaks and ridges deep glacial valleys and granite walls spotted with over 700 mountain lakes 5 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 and shaped the landscape 6 The last glacial retreat in the Alpine Lakes area began about 14 000 years ago and was north of the Canada US border by 10 000 years ago 6 The U shaped cross section of the river valleys is a result of that 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 Alpine Lakes Wilderness rea See also edit nbsp Mountains portal List of peaks of the Alpine Lakes WildernessGallery edit nbsp Spark Plug Mountain nbsp Surprise Mountain left Spark Plug Mountain right References edit a b c d e f Spark Plug Mountain Washington Peakbagger com a b c d Beckey Fred W Cascade Alpine Guide Climbing and High Routes Seattle WA Mountaineers Books 2008 a b Spark Plug Mountain 6 311 WA listsofjohn com Retrieved 2020 07 19 Spark Plug Mountain Geographic Names Information System United States Geological Survey United States Department of the Interior Retrieved 2020 07 19 Smoot Jeff 2004 Backpacking Washington s Alpine Lakes Wilderness Helena Montana The Globe Pequot Press a b c d e Kruckeberg Arthur 1991 The Natural History of Puget Sound Country University of Washington Press External links editWeather forecast Spark Plug Mountain Alpine Lakes Wilderness Mt Baker Snoqualmie National Forest U S Forest Service Retrieved from https en wikipedia org w index php title Spark Plug Mountain amp oldid 1218178209, wikipedia, wiki, book, books, library,

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