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487:), causing them to drop their moisture in the form of rain or snow onto the Cascades. 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.
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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 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. The U-shaped
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walls spotted with over 700 mountain lakes. 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 Alpine Lakes
Wilderness area.
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Beckey, Fred W. Cascade Alpine Guide Volume 1, Climbing and High Routes. Seattle, WA: Mountaineers Books, 1973, pg 258.
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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 Alpine Lakes
Wilderness features some of the most rugged topography in the
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cross section of the river valleys is a result of that recent glaciation.
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that originate in the north
Pacific Ocean travel east toward the
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is an 8,652-foot (2,637 meter) mountain summit located in
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Alpine Lakes
Wilderness (Okanogan-Wenatchee National Forest)
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618:Backpacking Washington's Alpine Lakes Wilderness
424:persisted. In addition, small fragments of the
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16:Mountain in Washington (state), United States
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513:List of peaks of the Alpine Lakes Wilderness
642:The Natural History of Puget Sound Country
620:. Helena, Montana: The Globe Pequot Press.
468:South aspect of Cannon Mountain seen from
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686:Mountains of Chelan County, Washington
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388:with craggy peaks and ridges, deep
190:Cannon Mountain (the United States)
33:Cannon Mountain seen from northeast
340:state. Cannon Mountain is part of
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644:. University of Washington Press.
348:. Cannon Mountain belongs to the
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681:Mountains of Washington (state)
587:"WA 100 Highest FA Chronology"
372:, which is a tributary of the
160:Show map of Washington (state)
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696:North American 2000 m summits
563:"Cannon Mountain - 8,657' WA"
542:"Cannon Mountain, Washington"
404:Cannon Mountain, north aspect
360:. The nearest higher peak is
193:Show map of the United States
440:about 50 million years ago.
368:from the slopes drains into
49:8,652 ft (2,637 m)
640:Kruckeberg, Arthur (1991).
81:2.15 mi (3.46 km)
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422:volcanic igneous activity
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109:47.502801°N 120.802476°W
59:838 ft (255 m)
430:continental lithosphere
352:which is subset of the
346:Alpine Lakes Wilderness
236:Alpine Lakes Wilderness
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157:Location in Washington
114:47.502801; -120.802476
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616:Smoot, Jeff (2004).
414:North American Plate
667:U.S. Forest Service
591:www.rhinoclimbs.com
254:Wenatchee Mountains
232:Protected area
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658:Weather forecast:
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39:Highest point
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342:The Enchantments
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362:Dragontail Peak
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570:. Retrieved
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436:created the
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370:Icicle Creek
350:Stuart Range
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302:First ascent
285:Type of rock
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258:Stuart Range
244:Parent range
445:Pleistocene
443:During the
112: /
100:120°48′09″W
87:Coordinates
65:Parent peak
675:Categories
572:2024-04-07
519:References
338:Washington
216:Washington
97:47°30′10″N
55:Prominence
125:Geography
77:Isolation
45:Elevation
491:See also
454:faulting
434:terranes
296:Climbing
265:Topo map
460:Climate
432:called
426:oceanic
394:granite
380:Geology
290:Granite
279:Geology
204:Country
450:Uplift
410:Eocene
392:, and
366:runoff
319:Hiking
226:Chelan
222:County
475:Most
322:YDS 2
212:State
452:and
428:and
306:1921
270:USGS
336:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
