Gray Wolf Ridge
Gray Wolf Mountain, at 7,218 feet (2,200 m) above sea level, is the ridge's highest summit. It was first climbed by Leigh B. Lint in 1928. Other distinct peaks include '7076' (7076), Baldy (6797), Tyler Peak (6364), and Maynard Peak (5065), which forms the northeastern terminus of Gray Wolf Ridge. Gray Wolf River runs through the valley-bottom to the Ridge's north; Royal Creek and the Dungeness River flow through the valley along the Ridge's east and south. Gray Wolf Ridge is the highest point of Clallam County.
Climate
Gray Wolf Ridge is located in the marine west coast climate zone of western North America. 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. 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. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.
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.
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Gray Wolf Ridge from the southeast; Baldy to right
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Baldy from Sequim, Washington
References
- ^ "Gray Wolf Ridge, Washington". Peakbagger.com.
- ^ "Gray Wolf Ridge - 7,218' WA". listsofjohn.com. Retrieved 2021-06-19.
- ^ "Gray Wolf Ridge". Geographic Names Information System. United States Geological Survey, United States Department of the Interior.
- ^ Majors, Harry M. (1975). Exploring Washington. Van Winkle Publishing Co. p. 70. ISBN 978-0-918664-00-6.
- ^ Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN 0-87842-160-2.