Lane Peak | |
Elevation Ft: | 6012 |
Prominence Ft: | 332 |
Isolation Mi: | 0.71 |
Isolation Ref: | [1] |
Country: | United States |
State: | Washington |
Region: | Lewis |
Region Type: | County |
Part Type: | Protected area |
Part: | Mount Rainier National Park |
Range: | Cascades |
Etymology: | Franklin Knight Lane |
Map: | Washington#USA |
Label Position: | right |
Coordinates: | 46.758°N -121.753°W |
Topo: | USGS Mount Rainier West |
Lane Peak is a 6012abbr=offNaNabbr=off mountain summit in Lewis County of Washington state. It is situated on the crest of the Tatoosh Range which is a sub-range of the Cascade Range. It is located south of Mount Rainier within Mount Rainier National Park.
Lane Peak's toponym honors United States Secretary of the Interior Franklin Knight Lane,[2] who presided over the establishment of the National Park Service in 1917. Precipitation runoff on the south side of the peak drains into tributaries of the Cowlitz River, whereas the north side drains into tributaries of the Nisqually River.
Lane Peak is located in the marine west coast climate zone of western North America.[3] Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snow onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall.[3] Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger.[3] 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.[3] Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below 0°F or above 80°F.[3]
Climbing Routes on Lane Peak[4]