Mount Steel
North aspect of Mt. Steel
Highest point
Elevation6,225 ft (1,897 m)[1]
Prominence825 ft (251 m)[1]
Parent peakMount Duckabush (6,254 ft)[2]
Isolation1.13 mi (1.82 km)[2]
Coordinates47°38′23″N 123°20′10″W / 47.6396268°N 123.3359891°W / 47.6396268; -123.3359891[3]
Geography
Mount Steel is located in Washington (state)
Mount Steel
Mount Steel
Location of Mount Steel in Washington
Mount Steel is located in the United States
Mount Steel
Mount Steel
Mount Steel (the United States)
LocationOlympic National Park
Jefferson County, Washington, US
Parent rangeOlympic Mountains
Topo mapUSGS Mount Steel
Geology
Age of rockEocene
Climbing
First ascentJuly 19, 1897[4]
Easiest routeclass 1[1]

Mount Steel is a 6,225-foot-elevation (1,897-meter) mountain summit located in the Olympic Mountains, in Jefferson County of Washington state.[3] It is situated in Olympic National Park and the Daniel J. Evans Wilderness. The nearest higher neighbor is Mount Duckabush, 1.36 mi (2.19 km) to the southwest.[5] Precipitation runoff from the mountain drains south into tributaries of the North Fork Skokomish River, and north into headwaters of the Duckabush River. Topographic relief is significant as the summit rises over 3,400 feet (1,036 m) above the Duckabush River in approximately one mile.

Climate

Mount Steel is located in the marine west coast climate zone of western North America.[6] Most weather fronts originate in the Pacific Ocean, and travel east 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. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. The months May through October offer the most favorable weather for climbing or viewing.[1]

History

The mountain's name was officially adopted in 1902 by the U.S. Board on Geographic Names.[3] It honors William Gladstone Steel (1854–1934), American journalist and mountaineer who encouraged the US Army to permit one of theirs to explore the Olympic Mountains, which resulted in the 1885 and 1890 O'Neil Expeditions.[4][7] Steel was also founder of the Oregon Alpine Club, the first mountaineering organization in the Pacific Northwest. Steel recruited three of the club's members to join Lieutenant Joseph P. O'Neil's second expedition, and sometime during or immediately after the expedition, the mountain was christened after him. It was during the second expedition that the north slope of Mt. Steel was burned when a small fire that the group set to eradicate wasps got out of control.[4] William G. Steel led an ascent of Mount Steel on August 24, 1906.[4]

Climbing routes

Established ascent routes on Mt. Steel:[1]

  • via First Divide – class 1
  • via Marmot Lake Trail – class 1

Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.[8] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

See also

References

  1. 1 2 3 4 5 Mount Steel, climbersguideolympics.com
  2. 1 2 "Steel, Mount – 6,225' WA". listsofjohn.com. Retrieved January 13, 2022.
  3. 1 2 3 "Mount Steel". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved January 13, 2022.
  4. 1 2 3 4 Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  5. ↑ "Mount Steel, Washington". Peakbagger.com.
  6. ↑ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN 1027-5606.
  7. ↑ Gail E. H. Evans, T. Allan Comp, 1983, Olympic Historic Resource Study, nps.gov
  8. ↑ Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN 0-87842-160-2.
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