Mount Meany
History
![](http://upload.wikimedia.org/wikipedia/commons/thumb/8/8f/8178_Mt_Meany%2C_Olympic_NP%2C_WA_1909_-_Asahel_Curtis_%2822730444136%29.jpg/180px-8178_Mt_Meany%2C_Olympic_NP%2C_WA_1909_-_Asahel_Curtis_%2822730444136%29.jpg)
The present day Mt. Meany - Mt. Queets area was referred to as Mt. Mesachie on the 1896 Gilman National Geographic Map. The word mesachie is from the Chinook Jargon and means wicked.
The mountain was named during the 1889-90 Seattle Press Expedition to honor Edmond S. Meany (1862–1935), at that time an employee of the Seattle Press who arranged the meeting between the expedition's newspaper sponsor, with Canadian James Halbold Christie, the leader of group of five which ascended the Elwha River and descended the North Fork Quinault River. Meany later became a renowned scholar and professor at the University of Washington, a Washington state legislator, and also a mountain climber who served as president of The Mountaineers.
The first ascent of the mountain was made August 8, 1907, by Asahel Curtis, Lorenz Nelson, and Peter McGregor.
Climate
Based on the Köppen climate classification, Mount Meany is located in the marine west coast climate zone of western North America. 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. 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. The months of July through September offer the most favorable weather for climbing.
Geology
![](http://upload.wikimedia.org/wikipedia/commons/thumb/6/6b/Olympic_Mountains_seen_from_Mount_Seattle%2C_Olympic_National_Park%2C_date_unknown.jpg/220px-Olympic_Mountains_seen_from_Mount_Seattle%2C_Olympic_National_Park%2C_date_unknown.jpg)
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
References
- ^ "Mount Meany". Peakbagger.com.
- ^ climbersguideolympics.com Mount Meany
- ^ "Mount Meany". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2019-01-21.
- ^ Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
- ^ Beckey, Fred (2003). Cascade Alpine Guide: Climbing and High Routes, Stevens Pass to Rainy Pass. The Mountaineers Books. pp. 353–355. ISBN 978-0-89886-838-8.
- ^ 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.
- ^ 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
- "Olympic National Park". National Park Service.
- Mount Meany: weather forecast