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period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The U-shaped cross section of the river valleys is a result of recent glaciation.
257:. It was first climbed in 1926 by Lage Wernstedt, who named it for the destruction caused by a forest fire that swept the slopes bare that same year. At the summit stands a small wooden one-room fire lookout belonging to the
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Desolation Peak Trail, is a steep hike to high meadows, great views and the fire lookout. It is a very popular hike but strenuous along the East Bank Trail. The trail is often hot and dry.
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363:. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences.
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in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North
Cascades area.
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In 2020 Lindsay Hagen published a short film about Jim
Henterley, one of the watchmen remaining in service on the Desolation Peak Lookout.
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spent 63 days during the summer of 1956 as a fire lookout on
Desolation Peak. He wrote about his experiences in
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Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
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The history of the formation of the
Cascade Mountains dates back millions of years ago to the late
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The North
Cascades features some of the most rugged topography in the
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Interior of
Desolation Peak Lookout, with bed and firefinder.
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Desolation Peak
Lookout with Mt. Hozomeen in the background
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Ode to
Desolation by Lindsey Hagen in Vimeo Staff Picks
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405:The view of Hozomeen Mountain from Desolation Peak
382:persisted. In addition, small fragments of the
16:Mountain in Washington (state), United States
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359:with craggy peaks, spires, ridges, and deep
591:The Natural History of Puget Sound Country
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506:. Van Winkle Publishing Co. p. 31.
481:United States Department of the Interior
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641:Mountains of Whatcom County, Washington
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636:North Cascades of Washington (state)
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472:Geographic Names Information System
179:Desolation Peak (the United States)
327:, and travel northeast toward the
311:Desolation Peak is located in the
289:by the name of "Desolation pops".
255:Ross Lake National Recreation Area
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593:. University of Washington Press.
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646:Mountains of Washington (state)
477:United States Geological Survey
149:Show map of Washington (state)
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443:"Desolation Peak, Washington"
398:about 50 million years ago.
182:Show map of the United States
49:6,102 ft (1,860 m)
589:Kruckeberg, Arthur (1991).
251:Canada–United States border
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551:Naum, Chris (2020-07-28),
92:48.9112432°N 121.0162346°W
64:3,249 ft (990 m)
500:Majors, Harry M. (1975).
380:volcanic igneous activity
331:. As fronts approach the
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315:climate zone of western
97:48.9112432; -121.0162346
528:"Desolation Peak Trail"
388:continental lithosphere
285:and in a collection of
243:North Cascade Mountains
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532:National Park Service
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259:National Park Service
503:Exploring Washington
372:North American Plate
343:onto the Cascades (
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52: NGVD 29
39:Highest point
609:"Desolation Peak"
513:978-0-918664-00-6
467:"Desolation Peak"
329:Cascade Mountains
323:originate in the
313:marine west coast
282:Desolation Angels
276:Lonesome Traveler
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378:, episodes of
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321:weather fronts
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227:Easiest route
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616:. Retrieved
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195:Parent range
613:Bivouac.com
411:Pleistocene
409:During the
253:and in the
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83:121°00′58″W
70:Coordinates
630:Categories
618:2010-03-06
560:2020-08-15
537:2010-12-30
486:2010-03-06
452:2010-12-30
426:References
247:Washington
241:is in the
232:Trail hike
80:48°54′40″N
60:Prominence
108:Geography
45:Elevation
420:faulting
392:terranes
341:snowfall
220:Climbing
208:Topo map
390:called
384:oceanic
351:Geology
319:. Most
307:Climate
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416:Uplift
368:Eocene
287:haiku
508:ISBN
418:and
386:and
337:rain
213:USGS
339:or
245:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
