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period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured and shaped the landscape. 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 cross section of the
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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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danger. 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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343:" is the colloquial name for several North American species of birds known for their fearlessness around humans and their proclivity for stealing food from campers.
363:. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snow onto the Cascades (
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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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339:. This peak's name is derived from Camp Robber Creek and Camp Robber Lake, which lie in Camp Robber Valley to the northwest of the peak. "
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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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is a 6,286-foot (1,916-metre) mountain summit located above the western shore of
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The Alpine Lakes
Wilderness features some of the most rugged topography in the
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Alpine Lakes
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originating in the
Pacific Ocean travel northeast toward the
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river valleys is a result of that recent glaciation.
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East aspect of Camp Robber Peak above Big Heart Lake
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from the mountain drains into Camp Robber Creek and
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629:Backpacking Washington's Alpine Lakes Wilderness
416:persisted. In addition, small fragments of the
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16:Mountain in Washington (state), United States
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458:List of peaks of the Alpine Lakes Wilderness
653:The Natural History of Puget Sound Country
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631:. Helena, Montana: The Globe Pequot Press.
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355:climate zone of western North America.
707:Mount Baker-Snoqualmie National Forest
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321:Mount Baker-Snoqualmie National Forest
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697:Mountains of King County, Washington
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191:Camp Robber Peak (the United States)
388:with craggy peaks and ridges, deep
351:Camp Robber Peak is located in the
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33:Camp Robber Peak, southwest aspect
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655:. University of Washington Press.
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323:. The nearest higher neighbor is
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692:Mountains of Washington (state)
604:"Camp Robber Peak Washington"
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567:"Camp Robber Peak - 6,286' WA"
530:"Camp Robber Peak, Washington"
161:Show map of Washington (state)
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712:North American 1000 m summits
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194:Show map of the United States
432:about 50 million years ago.
49:6,286 ft (1,916 m)
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651:Kruckeberg, Arthur (1991).
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82:1.31 mi (2.11 km)
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671:National Weather Service
311:state. It's part of the
110:47.571167°N 121.331948°W
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317:Alpine Lakes Wilderness
237:Alpine Lakes Wilderness
158:Location in Washington
115:47.571167; -121.331948
319:, on land managed by
627:Smoot, Jeff (2004).
591:Washington Scrambles
470:Mountains portal
406:North American Plate
678:U.S. Forest Service
233:Protected area
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669:Weather forecast:
369:maritime influence
39:Highest point
361:Cascade Mountains
353:marine west coast
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245:Parent range
608:Bivouac.com
437:Pleistocene
435:During the
341:Camp robber
305:King County
113: /
101:121°19′55″W
88:Coordinates
65:Parent peak
686:Categories
613:2020-06-22
576:2020-06-22
509:References
333:Foss River
309:Washington
288:scrambling
217:Washington
98:47°34′16″N
72:(6,305 ft)
55:Prominence
373:avalanche
126:Geography
78:Isolation
45:Elevation
452:See also
446:faulting
426:terranes
272:Climbing
258:Topo map
476:Gallery
424:called
418:oceanic
394:granite
380:Geology
347:Climate
205:Country
442:Uplift
402:Eocene
392:, and
329:runoff
223:County
213:State
444:and
420:and
263:USGS
227:King
307:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
