| Mount Steel | |
|---|---|
 North aspect of Mt. Steel | |
| Highest point | |
| Elevation | 6,225 ft (1,897 m)[1] |
| Prominence | 825 ft (251 m)[1] |
| Parent peak | Mount Duckabush (6,254 ft)[2] |
| Isolation | 1.13 mi (1.82 km)[2] |
| Coordinates | 47°38′23″N123°20′10″W / 47.6396268°N 123.3359891°W /47.6396268; -123.3359891[3] |
| Geography | |
  Mount Steel Location of Mount Steel in Washington Show map of Washington (state) Mount Steel Mount Steel (the United States) Show map of the United States | |
| Country | United States |
| State | Washington |
| County | Jefferson |
| Protected area | Olympic National Park |
| Parent range | Olympic Mountains |
| Topo map | USGSMount Steel |
| Geology | |
| Rock age | Eocene |
| Climbing | |
| First ascent | July 19, 1897[4] |
| Easiest route | class 1[1] |
Mount Steel is a 6,225-foot-elevation (1,897-meter) mountainsummit located in theOlympic Mountains, inJefferson County ofWashington state.[3] It is situated inOlympic National Park and theDaniel J. Evans Wilderness. The nearest higher neighbor isMount Duckabush, 1.36 mi (2.19 km) to the southwest.[5] Precipitationrunoff from the mountain drains south into tributaries of the North ForkSkokomish River, and north into headwaters of theDuckabush River.Topographic relief is significant as the summit rises over 3,400 feet (1,000 m) above the Duckabush River in approximately one mile.
Mount Steel is located in themarine west coast climate zone of western North America.[6]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.[7] Because ofmaritime influence, snow tends to be wet and heavy, resulting inavalanche 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.[7] The months May through October offer the most favorable weather for climbing or viewing.[1]
The mountain's name was officially adopted in 1902 by theU.S. Board on Geographic Names.[3] It honorsWilliam 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 the1885 and 1890 O'Neil Expeditions.[4][8] Steel was also founder of theOregon Alpine Club, the first mountaineering organization in the Pacific Northwest. Steel recruited three of the club's members to join LieutenantJoseph 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]
Established ascent routes on Mt. Steel:[1]
The Olympic Mountains are composed ofobductedclastic wedge material and oceanic crust, primarilyEocenesandstone,turbidite, andbasaltic oceanic crust.[9] The mountains were sculpted during thePleistocene era by erosion and glaciers advancing and retreating multiple times.
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