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Blue Mountain (Washington)

Blue Mountain is a 6,004-foot-elevation (1,830-meter) mountain summit located within Olympic National Park in Clallam County of Washington state. Blue Mountain is situated in the Daniel J. Evans Wilderness, 13 miles southeast of Port Angeles and 11 miles southwest of Sequim. Topographic relief is significant as the south aspect rises 4,000 feet (1,200 meters) above Gray Wolf River in approximately 2.5 miles. The mountain's name is due to a soft, blue haze that forms around the mountain in the summer.[3] New settlers to the Olympic Peninsula near the end of the 19th century brought devastating fires started by land clearing and logging activities.[4] The Dungeness Fire of 1891 burned about 30,000 acres, destroying much of the forest around Blue Mountain.[3]

Blue Mountain
West aspect, viewed from Hurricane Ridge Road
Highest point
Elevation6,004 ft (1,830 m)[1]
Prominence1,107 ft (337 m)[2]
Parent peakMaiden Peak (6,434 ft)[2]
Isolation3.14 mi (5.05 km)[2]
Coordinates47°57′16″N 123°15′34″W / 47.9545206°N 123.2594388°W / 47.9545206; -123.2594388[1]
Geography
Blue Mountain
Location of Blue Mountain in Washington
Blue Mountain
Blue Mountain (the United States)
CountryUnited States
StateWashington
CountyClallam
Protected areaOlympic National Park
Parent rangeOlympic Mountains
Topo mapUSGS Maiden Peak
Geology
Age of rockEocene
Climbing
Easiest routeclass 1 walking

Access is via the 19-mile Deer Park Road, and the summit can be reached by walking the half-mile Rain Shadow Loop Trail which gains 170 feet of elevation from road's end.[5] The trail is so named because Blue Mountain lies within the rain shadow of the Olympic Mountains, receiving 50 inches of precipitation annually compared to more than 200 inches on Mount Olympus, 23 miles distant.[6] Precipitation runoff from the mountain drains north to the Strait of Juan de Fuca via Maiden Creek, Siebert Creek, McDonald Creek, Canyon Creek, and Gray Wolf River. The summit offers a view of the San Juan Islands, Victoria across the strait on Vancouver Island, Canada, and on a clear day the eye can see as far as Mount Baker, 87 miles away. The endemic Olympic bellflower can be found near the summit.[5]

Climate edit

Based on the Köppen climate classification, Blue Mountain is located in the marine west coast climate zone of western North America.[7] Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks (orographic lift), 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.[8] Because of maritime influence, snow tends to be wet and heavy, resulting in high 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.[8]

Geology edit

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.[9] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

See also edit

Gallery edit

References edit

  1. ^ a b "Blue Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2021-12-29.
  2. ^ a b c "Blue Mountain - 6,007' WA". listsofjohn.com. Retrieved 2021-12-29.
  3. ^ a b Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  4. ^ "Fire History - Olympic National Park (U.S. National Park Service)". nps.gov. Retrieved 2021-12-30.
  5. ^ a b "Deer Park Area Brochure - Olympic National Park (U.S. National Park Service)". nps.gov. Retrieved 2021-12-30.
  6. ^ Alan Leftridge, 2017, The Best of Olympic National Park, Farcountry Press, ISBN 9781560376620
  7. ^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.
  8. ^ a b McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.
  9. ^ Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN 0-87842-160-2.

External links edit

  • "Olympic National Park". National Park Service.
  • Deer Park Area Brochure: National Park Service
  • Blue Mountain: Mountain-forecast.com

  Media related to Blue Mountain (Washington) at Wikimedia Commons

blue, mountain, washington, blue, mountain, foot, elevation, meter, mountain, summit, located, within, olympic, national, park, clallam, county, washington, state, blue, mountain, situated, daniel, evans, wilderness, miles, southeast, port, angeles, miles, sou. Blue Mountain is a 6 004 foot elevation 1 830 meter mountain summit located within Olympic National Park in Clallam County of Washington state Blue Mountain is situated in the Daniel J Evans Wilderness 13 miles southeast of Port Angeles and 11 miles southwest of Sequim Topographic relief is significant as the south aspect rises 4 000 feet 1 200 meters above Gray Wolf River in approximately 2 5 miles The mountain s name is due to a soft blue haze that forms around the mountain in the summer 3 New settlers to the Olympic Peninsula near the end of the 19th century brought devastating fires started by land clearing and logging activities 4 The Dungeness Fire of 1891 burned about 30 000 acres destroying much of the forest around Blue Mountain 3 Blue MountainWest aspect viewed from Hurricane Ridge RoadHighest pointElevation6 004 ft 1 830 m 1 Prominence1 107 ft 337 m 2 Parent peakMaiden Peak 6 434 ft 2 Isolation3 14 mi 5 05 km 2 Coordinates47 57 16 N 123 15 34 W 47 9545206 N 123 2594388 W 47 9545206 123 2594388 1 GeographyBlue MountainLocation of Blue Mountain in WashingtonShow map of Washington state Blue MountainBlue Mountain the United States Show map of the United StatesCountryUnited StatesStateWashingtonCountyClallamProtected areaOlympic National ParkParent rangeOlympic MountainsTopo mapUSGS Maiden PeakGeologyAge of rockEoceneClimbingEasiest routeclass 1 walking Access is via the 19 mile Deer Park Road and the summit can be reached by walking the half mile Rain Shadow Loop Trail which gains 170 feet of elevation from road s end 5 The trail is so named because Blue Mountain lies within the rain shadow of the Olympic Mountains receiving 50 inches of precipitation annually compared to more than 200 inches on Mount Olympus 23 miles distant 6 Precipitation runoff from the mountain drains north to the Strait of Juan de Fuca via Maiden Creek Siebert Creek McDonald Creek Canyon Creek and Gray Wolf River The summit offers a view of the San Juan Islands Victoria across the strait on Vancouver Island Canada and on a clear day the eye can see as far as Mount Baker 87 miles away The endemic Olympic bellflower can be found near the summit 5 Contents 1 Climate 2 Geology 3 See also 4 Gallery 5 References 6 External linksClimate editBased on the Koppen climate classification Blue Mountain is located in the marine west coast climate zone of western North America 7 Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains As fronts approach they are forced upward by the peaks orographic lift 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 8 Because of maritime influence snow tends to be wet and heavy resulting in high 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 8 Geology editThe Olympic Mountains are composed of obducted clastic wedge material and oceanic crust primarily Eocene sandstone turbidite and basaltic oceanic crust 9 The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times See also edit nbsp Mountains portal Olympic Mountains Geology of the Pacific NorthwestGallery edit nbsp Summit vista looking south nbsp View of summit from Deer Park nbsp West aspect near sunsetReferences edit a b Blue Mountain Geographic Names Information System United States Geological Survey United States Department of the Interior Retrieved 2021 12 29 a b c Blue Mountain 6 007 WA listsofjohn com Retrieved 2021 12 29 a b Parratt Smitty 1984 Gods and Goblins A Field Guide to Place Names of Olympic National Park 1st ed Fire History Olympic National Park U S National Park Service nps gov Retrieved 2021 12 30 a b Deer Park Area Brochure Olympic National Park U S National Park Service nps gov Retrieved 2021 12 30 Alan Leftridge 2017 The Best of Olympic National Park Farcountry Press ISBN 9781560376620 Peel M C Finlayson B L McMahon T A 2007 Updated world map of the Koppen Geiger climate classification Hydrol Earth Syst Sci 11 1633 1644 ISSN 1027 5606 a b McNulty Tim 2009 Olympic National Park A Natural History Seattle Washington University of Washington Press Alt D D Hyndman D W 1984 Roadside Geology of Washington pp 249 259 ISBN 0 87842 160 2 External links edit Olympic National Park National Park Service Deer Park Area Brochure National Park Service Blue Mountain Mountain forecast com nbsp Media related to Blue Mountain Washington at Wikimedia Commons Retrieved from https en wikipedia org w index php title Blue Mountain Washington amp oldid 1218700172, wikipedia, wiki, book, books, library,

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