Mount Fairchild
History
![](http://upload.wikimedia.org/wikipedia/commons/thumb/1/1f/Fairchild_airplane_--_Snow_Dome.png/220px-Fairchild_airplane_--_Snow_Dome.png)
Mount Fairchild is situated at the head of Fairchild Creek, which originates from the Fairchild Glacier, and each are named for pilot William R. Fairchild (1926–1969), who flew hundreds of photographic flights to support scientific studies of glaciers in the Olympic Mountains for the U. S. Geological Survey and U.S. National Park Service, as well as thousands of other glaciers in Western North America. Fairchild's method of taking off from the nearby Blue Glacier became known as the "Fairchild sleigh ride", and was seen in a climactic scene in a two-part show in the Lassie TV series. Fairchild was one of ten who died when the air taxi service he created crashed on February 5, 1969, immediately after take-off from Port Angeles, en route to Seattle. This mountain's toponym was officially adopted in 1975 by the U.S. Board on Geographic Names. The William R. Fairchild International Airport in nearby Port Angeles is also named after him.
The first ascent of this peak was made in 1963 by Denny Pruitt, Dan Baker, Jack Christiansen, and Roy Etten.
Climate
Based on the Köppen climate classification, Mount Fairchild is located in the marine west coast climate zone of western North America. This climate supports the Fairchild and Carrie Glaciers on its slopes. 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. 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. In terms of favorable weather, the best months for viewing and climbing are July through September.
Geology
The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust. The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.
See also
Gallery
References
- ^ "Mount Fairchild". Peakbagger.com.
- ^ "Fairchild, Mount - 6,925' WA". listsofjohn.com. Retrieved 2020-06-13.
- ^ climbersguideolympics.com Mount Fairchild
- ^ "Mount Fairchild". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2020-06-14.
- ^ Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
- ^ Port Angeles Daily News, Sep 5, 1975 - Paxon, Don, "National park sites named for aviator Fairchild"
- ^ "Port Angeles, WA Air Taxi Crashes, Feb 1969 | GenDisasters ... Genealogy in Tragedy, Disasters, Fires, Floods".
- ^ Olympic Mountain Rescue, Olympic Mountains, A climbing Guide, Fourth Edition, The Mountaineers Books, 2006, pg. 190.
- ^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification" (PDF). Hydrol. Earth Syst. Sci. 11 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606.
- ^ Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN 0-87842-160-2.
External links
- "Olympic National Park". National Park Service.
- Mount Fairchild: weather forecast