Mount Fairchild
| Mount Fairchild | |
|---|---|
 Mount Fairchild from Hurricane Ridge | |
| Highest point | |
| Elevation | 6,900 ft (2,100 m)[1] |
| Prominence | 450 ft (140 m)[1] |
| Parent peak | Mount Carrie (6,995 ft)[2] |
| Isolation | 0.85 mi (1.37 km)[2] |
| Coordinates | 47°54′01″N 123°38′00″W / 47.900141°N 123.633367°W[1] |
| Geography | |
  Mount Fairchild Location of Mount Fairchild in Washington  Mount Fairchild Mount Fairchild (the United States) | |
| Location | |
Mount Fairchild, also known as Mount William Fairchild, is a 6,900-foot (2,100-metre) glaciated mountain
Washington state.[4] Mt. Fairchild is the second-highest peak in the Bailey Range, which is a subrange of the Olympic Mountains. Its nearest higher neighbor is Mount Carrie, 0.84 mi (1.35 km) to the southwest, and Ruth Peak is set 0.92 mi (1.48 km) to the south.[1] In clear weather, the mountain can be seen from the visitor center at Hurricane Ridge. Precipitation runoff from the mountain drains into tributaries of the Elwha River
.
History
Mount Fairchild is situated at the head of Fairchild Creek, which originates from the
U.S. Board on Geographic Names.[4] 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.[8]
Climate
Based on the
marine west coast climate zone of western North America.[9] 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.[10] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.
See also
Gallery
-
-
Mt. Carrie (center), Mt. Fairchild (right) -
Mt. Fairchild (right) with Fairchild Glacier -
Fairchild (left), Carrie (right) from the west -
-
Bailey Range from Hurricane Ridge, Mt. Fairchild centered, Mount Fitzhenry to its right
References
- ^ a b c d "Mount Fairchild". Peakbagger.com.
- ^ a b c "Fairchild, Mount - 6,925' WA". listsofjohn.com. Retrieved 2020-06-13.
- ^ climbersguideolympics.com Mount Fairchild
- ^ a b c "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.
- ISSN 1027-5606.
- ISBN 0-87842-160-2.
External links
- "Olympic National Park". National Park Service.
- Mount Fairchild: weather forecast