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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.
404:), causing them to drop their moisture in the form of rain or snow. As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. Because of
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originating in the
Pacific Ocean travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks (
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Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification".
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364:. Mt. Skokomish has three summits, the south peak being the highest. Precipitation
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Gods and
Goblins: A Field Guide to Place Names of Olympic National Park
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Mt. Skokomish (left) and Mt. Stone (upper right) seen from Mt. Ellinor
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era by erosion and glaciers advancing and retreating multiple times.
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Mount
Skokomish (left) and Mount Stone (right) seen from Seattle
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state, United States. It is situated on the shared boundary of
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704:. Seattle, Washington: University of Washington Press.
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oceanic crust. The mountains were sculpted during the
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408:, snow tends to be wet and heavy, resulting in
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16:Mountain in Washington (state), United States
428:wedge material and oceanic crust, primarily
332:is a 6,434-foot (1,961 meter) mountain
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583:climbersguideolympics.com Mount Skokomish
469:(left), Skokomish (right) from Mt. Gladys
158:Location of Mount Skokomish in Washington
702:Olympic National Park: A Natural History
636:United States Department of the Interior
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505:Mount Skokomish seen from Gladys Divide
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421:The Olympic Mountains are composed of
779:Mountains of Mason County, Washington
481:Mount Skokomish seen from Mount Stone
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627:Geographic Names Information System
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191:Mount Skokomish (the United States)
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388:Mount Skokomish is located in the
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715:Alt, D.D.; Hyndman, D.W. (1984).
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534:Geology of the Pacific Northwest
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784:Mountains of Washington (state)
632:United States Geological Survey
717:Roadside Geology of Washington
598:"Skokomish, Mount - 6,154' WA"
161:Show map of Washington (state)
1:
789:North American 1000 m summits
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194:Show map of the United States
49:6,434 ft (1,961 m)
7:
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82:1.67 mi (2.69 km)
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744:Mount Skokomish Wilderness
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354:Mount Skokomish Wilderness
237:Mount Skokomish Wilderness
59:1,154 ft (352 m)
757:Mount Skokomish weather:
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753:. National Park Service.
655:Parratt, Smitty (1984).
392:climate zone of western
110:47.591087°N 123.294132°W
751:"Olympic National Park"
672:Hydrol. Earth Syst. Sci
115:47.591087; -123.294132
794:Olympic National Park
700:McNulty, Tim (2009).
350:Olympic National Park
241:Olympic National Park
719:. pp. 249–259.
746:U.S. Forest Service
233:Protected area
106: /
406:maritime influence
39:Highest point
774:Olympic Mountains
759:Mountain Forecast
622:"Mount Skokomish"
563:"Mount Skokomish"
390:marine west coast
370:Hamma Hamma River
338:Olympic Mountains
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639:. Retrieved
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342:Mason County
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319:class 2
294:Type of rock
269:
249:Parent range
445:Pleistocene
358:Mount Stone
282:Age of rock
113: /
101:123°17′39″W
88:Coordinates
70:Mount Stone
65:Parent peak
768:Categories
641:2019-01-17
607:2024-04-14
540:References
346:Washington
322:scrambling
217:Washington
98:47°35′28″N
72:(6,612 ft)
55:Prominence
684:1027-5606
467:Henderson
437:turbidite
433:sandstone
410:avalanche
126:Geography
78:Isolation
45:Elevation
512:See also
441:basaltic
423:obducted
306:Climbing
262:Topo map
451:Gallery
426:clastic
417:Geology
384:Climate
362:Seattle
298:pillow
276:Geology
205:Country
723:
682:
439:, and
430:Eocene
366:runoff
334:summit
300:basalt
287:Eocene
223:County
465:Mts.
352:with
340:, in
227:Mason
213:State
721:ISBN
680:ISSN
372:and
267:USGS
396:.
344:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
