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382:), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the North Cascades experiences 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.
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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.
398:. 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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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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that is 21 mi (34 km) southwest of
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The North
Cascades feature some of the most rugged topography in the
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lies 6.71 mi (10.80 km) to the southwest. Precipitation
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is an 8,347-foot (2,544-metre) mountain summit located in the
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originating in the
Pacific Ocean travel northeast toward the
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16:Mountain in Washington (state), United States
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394:with craggy peaks, spires, ridges, and deep
616:The Natural History of Puget Sound Country
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588:United States Department of the Interior
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660:Mountains of Chelan County, Washington
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579:Geographic Names Information System
323:state. The mountain is situated in
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618:. University of Washington Press.
351:. The mountain's name comes from
331:. The nearest higher neighbor is
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190:Tupshin Peak (the United States)
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655:Mountains of Washington (state)
584:United States Geological Survey
479:Geography of the North Cascades
343:from the peak drains to nearby
160:Show map of Washington (state)
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675:North American 2000 m summits
193:Show map of the United States
33:Tupshin Peak from Lake Chelan
441:about 50 million years ago.
285:1940 by Everett and Ida Darr
49:8,347 ft (2,544 m)
632:Tupshin Peak aerial photo:
614:Kruckeberg, Arthur (1991).
417:persisted. Glacier Peak, a
81:1.56 mi (2.51 km)
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670:Chinook Jargon place names
540:"Tupshin Peak, Washington"
511:"Tupshin Peak - 8,347' WA"
59:1,143 ft (348 m)
415:volcanic igneous activity
374:. As fronts approach the
329:Wenatchee National Forest
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431:continental lithosphere
347:via tributaries of the
313:Glacier Peak Wilderness
236:Glacier Peak Wilderness
109:48.29701°N 120.750681°W
157:Location in Washington
327:, on land managed by
114:48.29701; -120.750681
474:Mountains portal
407:North American Plate
484:White Goat Mountain
232:Protected area
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39:Highest point
372:Cascade Mountains
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439:North Cascades
413:, episodes of
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368:Weather fronts
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353:Chinook jargon
349:Stehekin River
317:North Cascades
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301:class 4-5
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292:Easiest route
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640:Tupshin Peak
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591:. Retrieved
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518:. Retrieved
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437:created the
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337:Bonanza Peak
309:Tupshin Peak
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281:First ascent
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244:Parent range
184:Tupshin Peak
151:Tupshin Peak
22:Tupshin Peak
446:Pleistocene
444:During the
423:Pleistocene
355:and means "
345:Lake Chelan
333:Devore Peak
112: /
100:120°45′02″W
87:Coordinates
70:Devore Peak
65:Parent peak
649:Categories
593:2019-04-26
520:2024-04-08
490:References
321:Washington
216:Washington
97:48°17′49″N
55:Prominence
638:Weather:
125:Geography
77:Isolation
45:Elevation
461:See also
455:faulting
435:terranes
298:Climbing
275:Climbing
269:Stehekin
261:Topo map
433:called
427:oceanic
386:Geology
363:Climate
315:of the
204:Country
451:Uplift
403:Eocene
357:needle
341:runoff
226:Chelan
222:County
634:PBase
212:State
453:and
429:and
266:USGS
359:".
319:in
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602:^
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
