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The Triad (mountain)

Coordinates:48°31′11″N121°09′47″W / 48.519665°N 121.163°W /48.519665; -121.163
From Wikipedia, the free encyclopedia
Mountain in Washington (state), United States
The Triad
The Triad seen from Eldorado Peak
Highest point
Elevation7,520+ ft (2,290+ m)[1]
Prominence760 ft (230 m)[1]
Parent peakEldorado Peak (8,868 ft)[1]
Isolation1.84 mi (2.96 km)[2]
Coordinates48°31′11″N121°09′47″W / 48.519665°N 121.163°W /48.519665; -121.163[1]
Geography
The Triad is located in Washington (state)
The Triad
The Triad
Location in Washington
Show map of Washington (state)
The Triad is located in the United States
The Triad
The Triad
The Triad (the United States)
Show map of the United States
Map
Interactive map of The Triad
CountryUnited States
StateWashington
CountySkagit
Protected areaNorth Cascades National Park
Parent rangeNorth Cascades
Topo mapUSGSEldorado Peak
Geology
Rock ageEocene toLate Cretaceous[4]
Rock typeGranodioriticOrthogneiss[4]
Climbing
First ascent1949 Dick Eilertsen, Dick Lowery, Dick Scales, Don Wilde[3]
Easiest routeScramblingclass 4

The Triad is a mountain with three peaks located in theNorth Cascades, inSkagit County ofWashington state.[5] Situated inNorth Cascades National Park, The Triad is positioned west of the crest of theCascade Range, approximately 12 miles east of the town ofMarblemount. The middle peak (highest) has an elevation of 7,520+ ft (2,290+ m), the west peak 7,440+ ft (2,270+ m), and the east peak 7,520+ ft (2,290+ m).[1] The popular hiking objective,Hidden Lake Peak Lookout, lies three miles to the southwest, and the nearest higher peak,Eldorado Peak, two miles to the northeast, is a popular mountaineering objective.[1] Precipitationrunoff from The Triad drains into tributaries of theCascade River which in turn is a tributary of theSkagit River. Thefirst ascent of the mountain was made in 1949 by Dick Eilertsen, Dick Lowery, Dick Scales, and Don Wilde. This climbing party which had three identical first names, named it theThree Dicks. However, in the interest of good taste, the more suitable and similar name was adopted since "triad" means a group or set of three connected people or things.[3]

Climate

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The Triad is located in themarine west coast climate zone of western North America.[3]

The Triad,Dorado Needle, andEldorado Peak (right) seen in winter from theSnowking Mountain area

Mostweather fronts coming off the Pacific Ocean travel northeast toward theCascade 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.Because ofmaritime influence, snow tends to be wet and heavy, resulting in highavalanche 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] This climate supports a small unnamed glacier on the north slope below the steep walls of the north face.

Geology

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The North Cascades features some of the most rugged topography in theCascade Range with craggy peaks and ridges, deepglacial valleys, andgranite spires. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to various climate differences.

The history of the formation of the Cascade Mountains dates back millions of years ago to the lateEocene Epoch.[6] With theNorth American Plate overriding thePacific Plate, episodes ofvolcanic igneous activity persisted.[6] In addition, small fragments of theoceanic andcontinental lithosphere calledterranes created theNorth Cascades about 50 million years ago.[6]

During thePleistocene 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 andfaulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.

Access

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The trailhead for Hidden Lake Trail #745 to access The Triad is located at the end of five mile long Forest Service Road #1540, which junctions 9.5 miles up the Cascade River Road from Marblemount. The steep trail starts in forest then transitions to wonderfulwildflower filled meadows before climbing high into heather and rock gardens.[7] From this transition zone the route leaves the trail to bear east and up to the top of the ridge where a boot path reappears.

Gallery

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  • The Triad from Sahale Mountain
    The Triad fromSahale Mountain
  • The Triad from Sahale Mountain
    The Triad from Sahale Mountain
  • West aspect
    West aspect
  • The Triad from WSW
    The Triad from WSW

See also

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References

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  1. ^abcdef"The Triad, Washington".Peakbagger.com.
  2. ^"Triad, The - 7,540' WA".listsofjohn.com. Retrieved2021-06-23.
  3. ^abcdeBeckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  4. ^abGeologic map of the North Cascade Range, Washington, Haugerud, R.A., and Tabor, R.W., US Geological Survey, 2009.
  5. ^"The Triad".Geographic Names Information System.United States Geological Survey,United States Department of the Interior. Retrieved2019-05-11.
  6. ^abcdKruckeberg, Arthur (1991).The Natural History of Puget Sound Country. University of Washington Press.
  7. ^"Hidden Lake Lookout Trail #745 Mt. Baker-Snoqualmie National Forest".U.S. Forest Service. Retrieved2019-05-11.

External links

[edit]
Places adjacent to The Triad (mountain)
Retrieved from "https://en.wikipedia.org/w/index.php?title=The_Triad_(mountain)&oldid=1297747385"
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