| Mount Appleton | |
|---|---|
 Mount Appleton seen from Hurricane Ridge | |
| Highest point | |
| Elevation | 6,000 ft (1,800 m)[1] |
| Prominence | 200 ft (61 m)[1] |
| Coordinates | 47°57′02″N 123°43′59″W / 47.95045°N 123.733194°W[1] |
| Geography | |
  Mount Appleton Location of Mount Appleton in Washington  Mount Appleton Mount Appleton (the United States) | |
| Location | Olympic National Park Clallam County, Washington, US |
| Parent range | Olympic Mountains |
| Topo map | USGS Mount Carrie |
| Geology | |
| Age of rock | Eocene |
| Climbing | |
| Easiest route | class 3 scrambling |
Mount Appleton[2] is a 6,000+ ft (1,830+ m) double summit mountain located in the Olympic Mountains, in Clallam County of Washington state. It is set within Olympic National Park and is situated northwest of Appleton Pass. Its nearest higher peak is South Appleton (6100+ ft), 0.33 mi (0.53 km) to the south.[1] Precipitation runoff from Mount Appleton drains into the Sol Duc River, and Boulder Creek which is a tributary of the Elwha River, thence into the Strait of Juan de Fuca.
History
Mount Appleton was so named to honor Dr. T. J. Appleton, who moved to Port Angeles, Washington, from the state of Michigan, circa 1897.[3] He was a pioneering physician who made house calls in some of the most rural parts of Clallam County and was the first white doctor to treat Native Americans in this area.[3] Appleton was also an eloquent speaker and published author. Later he was a three-term mayor of Port Angeles before he died in 1942.[3]
The first ascent of the mountain is unknown.[4]
Climate
Set in the northwest portion of the Olympic Mountains, Mount Appleton is located in the marine west coast climate zone of western North America.[5] 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.[5] 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 high avalanche danger.[5]
Geology
The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.[6] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.
See also
References
- 1 2 3 4 "Mount Appleton". Peakbagger.com.
- ↑ "Mount Appleton". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2018-08-29.
- 1 2 3 Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
- ↑ Mount Appleton climbersguideolympics.com
- 1 2 3 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.
- Weather: Mount Appleton