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is significant as the southeast aspect rises 2,800 feet (850 meters) above the Big
Quilcene River in less than one mile, and the north aspect rises 1,700 feet (520 meters) above Buckhorn Lake in one-half mile. Old-growth forests of Douglas fir, western hemlock, and western redcedar grow in the
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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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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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Iron
Mountain (left) and Buckhorn Mountain (center and right) seen from the north along Tubal Cain Trail.
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647:, Olympic Mountain Rescue, Third Edition, 1988, The Mountaineers Books, page 25.
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View from Mount
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era by erosion and glaciers advancing and retreating multiple times.
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Places adjacent to Iron
Mountain (Jefferson County, Washington)
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valleys surrounding the peak. The nearest community is
691:. Seattle, Washington: University of Washington Press.
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oceanic crust. The mountains were sculpted during the
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418:wedge material and oceanic crust, primarily
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887:Mountains of Jefferson County, Washington
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689:Olympic National Park: A Natural History
645:Climber's Guide to the Olympic Mountains
626:United States Department of the Interior
325:is a 6,826-foot (2,081-metre) elevation
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386:climate zone of western North America.
158:Location of Iron Mountain in Washington
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411:The Olympic Mountains are composed of
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617:Geographic Names Information System
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702:Alt, D.D.; Hyndman, D.W. (1984).
191:Iron Mountain (the United States)
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524:Geology of the Pacific Northwest
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382:Iron Mountain is located in the
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877:Mountains of Washington (state)
622:United States Geological Survey
704:Roadside Geology of Washington
161:Show map of Washington (state)
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892:North American 2000 m summits
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194:Show map of the United States
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49:6,826 ft (2,081 m)
585:"Iron Mountain - 6,826' WA"
549:"Iron Mountain, Washington"
82:0.30 mi (0.48 km)
16:Mountain in Washington, USA
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110:47.8284289°N 123.1101090°W
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349:. It is situated between
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341:state. It is set within
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659:Hydrol. Earth Syst. Sci
347:Olympic National Forest
329:located in the eastern
59:266 ft (81 m)
565:USGS topographic map,
374:11 miles to the east.
687:McNulty, Tim (2009).
345:, on land managed by
706:. pp. 249–259.
343:Buckhorn Wilderness
237:Buckhorn Wilderness
233:Protected area
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855:Big Quilcene River
826:Big Quilcene River
396:maritime influence
367:Topographic relief
359:Big Quilcene River
39:Highest point
882:Olympic Mountains
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846:Buckhorn Mountain
784:Mount Worthington
384:marine west coast
355:Mount Worthington
351:Buckhorn Mountain
331:Olympic Mountains
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251:Olympic Mountains
70:Buckhorn Mountain
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731:Weather forecast
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335:Jefferson County
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306:Easiest route
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22:Iron Mountain
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804:Petunia Peak
777:Copper Creek
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629:. Retrieved
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592:. Retrieved
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312:class 3
295:First ascent
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245:Parent range
435:Pleistocene
278:Age of rock
113: /
101:123°06′36″W
88:Coordinates
65:Parent peak
871:Categories
631:2022-02-18
594:2022-02-18
569:Quadrangle
530:References
339:Washington
315:scrambling
217:Washington
98:47°49′42″N
72:(6,988 ft)
55:Prominence
671:1027-5606
427:turbidite
423:sandstone
400:avalanche
227:Jefferson
126:Geography
78:Isolation
45:Elevation
498:See also
431:basaltic
413:obducted
372:Quilcene
289:Climbing
258:Topo map
441:Gallery
416:clastic
407:Geology
378:Climate
299:Unknown
272:Geology
205:Country
710:
669:
429:, and
420:Eocene
327:summit
283:Eocene
223:County
213:State
708:ISBN
667:ISSN
263:USGS
337:of
333:in
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
