Mount Johnson is a summit in the Olympic Mountains and is located in Jefferson County of Washington state. It is situated within Olympic National Park and the Daniel J. Evans Wilderness. At 7,680 feet (2,341 m) high, Mount Johnson is the fourth-highest peak of the Olympic Mountains, after Mount Olympus, Mount Deception, and Mount Constance.[1] It is the highest peak in The Needles range which is a subset of the Olympic range. The nearest higher neighbor is Mount Deception, 1.34 mi (2.16 km) to the south.[1] Mount Johnson is set in the eastern portion of the Olympic Mountains within the drainage basin of the Dungeness River. This location puts it in the rain shadow of the Olympic Range, resulting in less precipitation than Mount Olympus and the western Olympics receive.
| Mount Johnson | |
|---|---|
 Mount Johnson (highest point) from northwest | |
| Highest point | |
| Elevation | 7,680 ft (2,341 m)[1] |
| Prominence | 480 ft (146 m)[1] |
| Parent peak | Mount Deception |
| Isolation | 1.34 mi (2.16 km)[2] |
| Coordinates | 47°49′58″N 123°14′14″W / 47.832665°N 123.237308°W[1] |
| Geography | |
  Mount Johnson Location of Mount Johnson in Washington  Mount Johnson Mount Johnson (the United States) | |
| Country | United States |
| State | Washington |
| County | Jefferson |
| Protected area | Olympic National Park |
| Parent range | Olympic Mountains |
| Topo map | USGS Mount Deception |
| Geology | |
| Rock age | Eocene |
| Climbing | |
| First ascent | 1935 or 1940 |
| Easiest route | class 4 Scramble[2] |
History
editMount Johnson was given its name based on what was believed to be the first ascent by Elvin Johnson and George Martin in 1940. However, new evidence has become available establishing that it was climbed by Scott Osborn, Joe Halwax, and John King circa 1935.[3]
Climate
editMount Johnson is located in the marine west coast climate zone of western North America.[4] 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.[5] 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.[5] The months July through September offer the most favorable weather for viewing or climbing this peak.[6]
Recreation
editWhile not a particularly technical climb, Mount Johnson is a steep and exposed class 4 scramble.[2] It's one of several mountaineering objectives in the Royal Basin area.
Gallery
edit-
Mt. Johnson summit (upper left), Sweat Spire and Gasp Pinnacle are centered. -
Mount Johnson (center) seen from Mount Deception -
The Needles from Mount Deception. Johnson in upper left behind Martin Peak -
Mount Johnson and The Needles seen from Elk Mountain -
Mount Johnson centered in the distance, as seen from Marmot Pass.
References
edit- ^ a b c d e "Mount Johnson". Peakbagger.com. Retrieved 2019-10-10.
- ^ a b c ""Mount Johnson" - 7,700' WA". listsofjohn.com. Retrieved 2020-06-17.
- ^ Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
- ^ 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.
- ^ a b McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.
- ^ Mount Johnson, climbersguideolympics.com
External links
edit
- "Olympic National Park". National Park Service.
- Mount Johnson photo: Flickr