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Colchuck Balanced Rock

Colchuck Balanced Rock is an 8,200+ ft (2,500+ m) granite mountain summit located in Chelan County of Washington state. Colchuck Balanced Rock is part of The Enchantments within the Alpine Lakes Wilderness. It belongs to the Stuart Range which is subset of the Cascade Range. Colchuck Balanced Rock is situated west of Enchantment Peak, and east of Jabberwocky Tower and Colchuck Lake. Precipitation runoff from the peak drains into the lake and Mountaineer Creek, a tributary of Icicle Creek. The climbing approach is via the Colchuck Lake Trail, then traversing away from Aasgard Pass approximately 400 feet above the lake. The mountain is named for its pyramidal summit which has a top-block that nests, rather than balances, on the summit.[3] The mountain and glacier take their name from the lake, which in Chinook jargon means "cold water".[4]

Colchuck Balanced Rock
Colchuck Balanced Rock from Colchuck Lake Trail
Highest point
Elevation8,200 ft (2,500 m)[1]
Prominence160 ft (49 m)[1]
Parent peakEnchantment Peak 8520+ ft[1]
Coordinates47°29′29″N 120°49′08″W / 47.491451°N 120.818789°W / 47.491451; -120.818789Coordinates: 47°29′29″N 120°49′08″W / 47.491451°N 120.818789°W / 47.491451; -120.818789[1]
Geography
Colchuck Balanced Rock
Location in Washington
Colchuck Balanced Rock
Colchuck Balanced Rock (the United States)
LocationChelan County
Washington state, U.S.
Parent rangeStuart Range
Cascade Range
Topo mapUSGS Enchantment Lakes
Geology
Type of rockGranite
Climbing
First ascent1958 by Gene Prater,Thomas Quin[2]
Easiest routeClimbing

Climate

Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains.[3] 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 snowfall onto the Cascades (Orographic lift). As a result, the Cascades experience high precipitation, especially during the winter months in the form of snowfall. 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.

Geology

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 spires 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 various climate differences.

 
Colchuck Balanced Rock

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 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 are 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 area.

Climbing Routes

 
Colchuck Balanced Rock above Colchuck Lake

Climbing Routes on Colchuck Balanced Rock[7]

References

  1. ^ a b c d "Colchuck Balanced Rock, Washington". Peakbagger.com.
  2. ^ Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  3. ^ a b Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  4. ^ Birght, William (2004). Native American Placenames of the United States. University of Oklahoma Press. p. 115. ISBN 0806135980.
  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.
  7. ^ Colchuck Balanced Rock Climbing Mountain Project
 
Colchuck Balanced Rock (left) at sunset

External links

  • Alpine Lakes Wilderness (Mt. Baker-Snoqualmie National Forest) U.S. Forest Service

colchuck, balanced, rock, granite, mountain, summit, located, chelan, county, washington, state, part, enchantments, within, alpine, lakes, wilderness, belongs, stuart, range, which, subset, cascade, range, situated, west, enchantment, peak, east, jabberwocky,. Colchuck Balanced Rock is an 8 200 ft 2 500 m granite mountain summit located in Chelan County of Washington state Colchuck Balanced Rock is part of The Enchantments within the Alpine Lakes Wilderness It belongs to the Stuart Range which is subset of the Cascade Range Colchuck Balanced Rock is situated west of Enchantment Peak and east of Jabberwocky Tower and Colchuck Lake Precipitation runoff from the peak drains into the lake and Mountaineer Creek a tributary of Icicle Creek The climbing approach is via the Colchuck Lake Trail then traversing away from Aasgard Pass approximately 400 feet above the lake The mountain is named for its pyramidal summit which has a top block that nests rather than balances on the summit 3 The mountain and glacier take their name from the lake which in Chinook jargon means cold water 4 Colchuck Balanced RockColchuck Balanced Rock from Colchuck Lake TrailHighest pointElevation8 200 ft 2 500 m 1 Prominence160 ft 49 m 1 Parent peakEnchantment Peak 8520 ft 1 Coordinates47 29 29 N 120 49 08 W 47 491451 N 120 818789 W 47 491451 120 818789 Coordinates 47 29 29 N 120 49 08 W 47 491451 N 120 818789 W 47 491451 120 818789 1 GeographyColchuck Balanced RockLocation in WashingtonShow map of Washington state Colchuck Balanced RockColchuck Balanced Rock the United States Show map of the United StatesLocationChelan CountyWashington state U S Parent rangeStuart RangeCascade RangeTopo mapUSGS Enchantment LakesGeologyType of rockGraniteClimbingFirst ascent1958 by Gene Prater Thomas Quin 2 Easiest routeClimbing Contents 1 Climate 2 Geology 3 Climbing Routes 4 References 5 External linksClimate EditMost weather fronts originate in the Pacific Ocean and travel east toward the Cascade Mountains 3 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 snowfall onto the Cascades Orographic lift As a result the Cascades experience high precipitation especially during the winter months in the form of snowfall 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 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 spires 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 various climate differences Colchuck Balanced Rock 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 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 are 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 area Climbing Routes Edit Colchuck Balanced Rock above Colchuck Lake Climbing Routes on Colchuck Balanced Rock 7 Colchuck Balanced Rock Col class 3 The Tipping Point class 5 12 8 pitches Let it Burn class 5 12 8 pitches West Face class 5 11 9 pitches The Tempest class 5 12 6 pitches Full Tilt Tempest Wall Free Version class 5 12 5 pitches The Scoop class 5 11c 10 pitches Rikki Tikki Tavi class 5 11 5 pitches Leche La Vaca class 5 10 4 pitchesReferences Edit a b c d Colchuck Balanced Rock Washington Peakbagger com Beckey Fred W Cascade Alpine Guide Climbing and High Routes Seattle WA Mountaineers Books 2008 a b Beckey Fred W Cascade Alpine Guide Climbing and High Routes Seattle WA Mountaineers Books 2008 Birght William 2004 Native American Placenames of the United States University of Oklahoma Press p 115 ISBN 0806135980 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 Colchuck Balanced Rock Climbing Mountain Project Colchuck Balanced Rock left at sunsetExternal links EditAlpine Lakes Wilderness Mt Baker Snoqualmie National Forest U S Forest Service Retrieved from https en wikipedia org w index php title Colchuck Balanced Rock amp oldid 1074225335, wikipedia, wiki, book, books, library,

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