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Iron Mountain (Jefferson County, Washington)

Iron Mountain is a 6,826-foot (2,081-metre) elevation summit located in the eastern Olympic Mountains in Jefferson County of Washington state.[4] It is set within Buckhorn Wilderness, on land managed by Olympic National Forest. It is situated between Buckhorn Mountain, 0.58 mi (0.93 km) to the southwest, and Mount Worthington, 0.76 mi (1.22 km) to the northeast.[1] Precipitation runoff from Iron Mountain drains south into the Big Quilcene River, and north into Copper Creek which is a tributary of the Dungeness River. Topographic relief 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 valleys surrounding the peak. The nearest community is Quilcene 11 miles to the east.

Iron Mountain
Northwest aspect
Highest point
Elevation6,826 ft (2,081 m)[1][2]
Prominence266 ft (81 m)[1]
Parent peakBuckhorn Mountain (6,988 ft)[3]
Isolation0.30 mi (0.48 km)[3]
Coordinates47°49′42″N 123°06′36″W / 47.8284289°N 123.1101090°W / 47.8284289; -123.1101090[4]
Geography
Iron Mountain
Location of Iron Mountain in Washington
Iron Mountain
Iron Mountain (the United States)
LocationBuckhorn Wilderness
Jefferson County, Washington, US
Parent rangeOlympic Mountains
Topo mapUSGS Mount Townsend
Geology
Age of rockEocene
Climbing
First ascentUnknown[5]
Easiest routeclass 3 scrambling[3]

Climate edit

Iron Mountain is located in the marine west coast climate zone of western North America.[6] Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche 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.

Geology edit

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.[7] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

Gallery edit

See also edit

References edit

  1. ^ a b c "Iron Mountain, Washington". Peakbagger.com.
  2. ^ USGS topographic map, Mount Townsend Quadrangle
  3. ^ a b c "Iron Mountain - 6,826' WA". listsofjohn.com. Retrieved 2022-02-18.
  4. ^ a b "Iron Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2022-02-18.
  5. ^ Climber's Guide to the Olympic Mountains, Olympic Mountain Rescue, Third Edition, 1988, The Mountaineers Books, page 25.
  6. ^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN 1027-5606.
  7. ^ Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN 0-87842-160-2.

External links edit

  • Weather forecast

iron, mountain, jefferson, county, washington, iron, mountain, foot, metre, elevation, summit, located, eastern, olympic, mountains, jefferson, county, washington, state, within, buckhorn, wilderness, land, managed, olympic, national, forest, situated, between. Iron Mountain is a 6 826 foot 2 081 metre elevation summit located in the eastern Olympic Mountains in Jefferson County of Washington state 4 It is set within Buckhorn Wilderness on land managed by Olympic National Forest It is situated between Buckhorn Mountain 0 58 mi 0 93 km to the southwest and Mount Worthington 0 76 mi 1 22 km to the northeast 1 Precipitation runoff from Iron Mountain drains south into the Big Quilcene River and north into Copper Creek which is a tributary of the Dungeness River Topographic relief 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 valleys surrounding the peak The nearest community is Quilcene 11 miles to the east Iron MountainNorthwest aspectHighest pointElevation6 826 ft 2 081 m 1 2 Prominence266 ft 81 m 1 Parent peakBuckhorn Mountain 6 988 ft 3 Isolation0 30 mi 0 48 km 3 Coordinates47 49 42 N 123 06 36 W 47 8284289 N 123 1101090 W 47 8284289 123 1101090 4 GeographyIron MountainLocation of Iron Mountain in WashingtonShow map of Washington state Iron MountainIron Mountain the United States Show map of the United StatesLocationBuckhorn WildernessJefferson County Washington USParent rangeOlympic MountainsTopo mapUSGS Mount TownsendGeologyAge of rockEoceneClimbingFirst ascentUnknown 5 Easiest routeclass 3 scrambling 3 Contents 1 Climate 2 Geology 3 Gallery 4 See also 5 References 6 External linksClimate editIron Mountain is located in the marine west coast climate zone of western North America 6 Most weather fronts originate in the Pacific Ocean and travel northeast toward the Olympic Mountains As fronts approach they are forced upward by the peaks of the Olympic Range causing them to drop their moisture in the form of rain or snowfall Orographic lift As a result the Olympics experience high precipitation especially during the winter months in the form of snowfall Because of maritime influence snow tends to be wet and heavy resulting in avalanche 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 Geology editThe Olympic Mountains are composed of obducted clastic wedge material and oceanic crust primarily Eocene sandstone turbidite and basaltic oceanic crust 7 The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times Gallery edit nbsp Iron Mountain left and Buckhorn Mountain center and right seen from the north along Tubal Cain Trail nbsp Northwest aspect nbsp Northwest aspect nbsp View from Mount Constance with Buckhorn Iron and Worthington at topSee also edit nbsp Mountains portal Geology of the Pacific NorthwestReferences edit a b c Iron Mountain Washington Peakbagger com USGS topographic map Mount Townsend Quadrangle a b c Iron Mountain 6 826 WA listsofjohn com Retrieved 2022 02 18 a b Iron Mountain Geographic Names Information System United States Geological Survey United States Department of the Interior Retrieved 2022 02 18 Climber s Guide to the Olympic Mountains Olympic Mountain Rescue Third Edition 1988 The Mountaineers Books page 25 Peel M C Finlayson B L McMahon T A 2007 Updated world map of the Koppen Geiger climate classification Hydrol Earth Syst Sci 11 ISSN 1027 5606 Alt D D Hyndman D W 1984 Roadside Geology of Washington pp 249 259 ISBN 0 87842 160 2 External links editWeather forecast Retrieved from https en wikipedia org w index php title Iron Mountain Jefferson County Washington amp oldid 1133727916, wikipedia, wiki, book, books, library,

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