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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. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below
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0 °F (−18 °C) or above 80 °F (27 °C). 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. Because of
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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.
344:. 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 background left to right, Mouth Terror, Mount
Degenhardt, The Pyramid, Inspiration Peak and the McMillan Spires
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Mount
Degenhardt seen from north side and centered between Inspiration Peak on left and Mount Terror on right
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259:. Located in the northern section of the park, Mount Degenhardt is .30 mi (0.48 km) southeast of
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The history of the formation of the
Cascade Mountains dates back millions of years ago to the late
271:. Mount Degenhardt is named after William Degenhardt, an early 20th century mountain climber. The
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The North
Cascades features some of the most rugged topography in the
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Cascade alpine guide, Volume 3: Rainy Pass to Fraser River
522:(Map). TopoQwest (United States Geological Survey Maps)
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16:Mountain in Washington (state), United States
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550:The Natural History of Puget Sound Country
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267:. and .75 mi (1.21 km) west of
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471:United States Department of the Interior
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580:Mountains of Whatcom County, Washington
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263:, .28 mi (0.45 km) west of
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415:Degenhardt is highest point centered
340:with craggy peaks, ridges, and deep
462:Geographic Names Information System
283:Mount Degenhardt is located in the
299:, and travel northeast toward the
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552:. University of Washington Press.
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570:Mountains of Washington (state)
467:United States Geological Survey
432:"Mount Degenhardt, Washington"
138:Show map of Washington (state)
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171:Show map of the United States
168:Location in the United States
575:North Cascades National Park
405:North Cascades National Park
379:about 50 million years ago.
257:North Cascades National Park
548:Kruckeberg, Arthur (1991).
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186:Whatcom County, Washington
361:volcanic igneous activity
303:. As fronts approach the
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502:Beckey, Fred W. (1996).
287:climate zone of western
369:continental lithosphere
59:280 ft (90 m)
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135:Location in Washington
87:48.77139°N 121.29306°W
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407:National Park Service
251:in the U.S. state of
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519:Mount Challenger, WA
353:North American Plate
92:48.77139; -121.29306
49:8,000+ ft (2,440+ m)
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457:"Mount Degenhardt"
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322:maritime influence
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39:Highest point
301:Cascade Mountains
295:originate in the
285:marine west coast
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399:External links
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377:North Cascades
359:, episodes of
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305:North Cascades
293:weather fronts
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273:Terror Glacier
269:McMillan Spire
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261:Mount Terror
249:Picket Range
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226:First ascent
195:Parent range
384:Pleistocene
382:During the
255:and within
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78:121°17′35″W
65:Coordinates
564:Categories
253:Washington
75:48°46′17″N
55:Prominence
326:avalanche
103:Geography
45:Elevation
526:July 20,
476:July 20,
441:July 20,
393:faulting
373:terranes
328:danger.
317:snowfall
220:Climbing
208:Topo map
182:Location
371:called
365:oceanic
332:Geology
291:. Most
279:Climate
389:Uplift
349:Eocene
188:, U.S.
528:2013
478:2013
443:2013
391:and
367:and
313:rain
213:USGS
315:or
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
