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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 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
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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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in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the
Cascade Range.
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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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from this mountain drains into tributaries of the North and Middle Forks of the
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of the river valleys is a result of that recent glaciation.
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South aspect of
Moolock Mountain (centered), seen from
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586:Native American Placenames of the United States
367:, snow tends to be wet and heavy, resulting in
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319:is 2.5 miles to the southwest. Precipitation
16:Mountain in Washington (state), United States
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627:The Natural History of Puget Sound Country
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546:United States Department of the Interior
288:is a 4,965-foot-elevation (1,513-meter)
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657:Mount Baker-Snoqualmie National Forest
306:Mount Baker-Snoqualmie National Forest
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647:Mountains of King County, Washington
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194:Moolock Mountain (the United States)
537:Geographic Names Information System
339:Moolock Mountain is located in the
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629:. University of Washington Press.
588:, University of Oklahoma Press,
566:Dictionary of the Chinook Jargon
460:Geology of the Pacific Northwest
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662:Mountains of Washington (state)
542:United States Geological Survey
508:"Moolock Mountain - 4,965' WA"
487:"Moolock Mountain, Washington"
164:Show map of Washington (state)
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667:North American 1000 m summits
355:, and travel east toward the
197:Show map of the United States
52:4,965 ft (1,513 m)
33:Southeast aspect, seen from
625:Kruckeberg, Arthur (1991).
85:1.81 mi (2.91 km)
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672:Chinook Jargon place names
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343:climate zone of western
113:47.547367°N 121.641897°W
62:925 ft (282 m)
584:William Bright (2004),
161:Location in Washington
118:47.547367; -121.641897
564:George Gibbs (2021),
304:, on land managed by
331:word meaning "elk."
109: /
384:Epoch. During the
365:maritime influence
42:Highest point
357:Cascade Mountains
351:originate in the
341:marine west coast
313:Bessemer Mountain
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73:Bessemer Mountain
35:Preacher Mountain
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549:. Retrieved
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429:Mailbox Peak
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238:Parent range
386:Pleistocene
310:line parent
294:King County
292:located in
116: /
104:121°38′31″W
91:Coordinates
68:Parent peak
641:Categories
551:2022-03-25
517:2022-03-25
466:References
298:Washington
220:Washington
101:47°32′51″N
75:(5,166 ft)
58:Prominence
369:avalanche
129:Geography
81:Isolation
48:Elevation
438:See also
395:faulting
265:Climbing
259:Mount Si
251:Topo map
596:, p.297
401:Gallery
376:Geology
347:. Most
335:Climate
208:Country
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391:Uplift
382:Eocene
321:runoff
290:summit
278:hiking
226:County
216:State
590:ISBN
570:ISBN
393:and
256:USGS
230:King
296:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
