Grasshopper Peak

From Wikipedia, the free encyclopedia

Elevation6,850 ft (2,088 m)[1][2]
Prominence430 ft (131 m)[3]
Isolation2.03 mi (3.27 km)[3]
Coordinates47°57′19″N 120°54′20″W / 47.955392°N 120.90544°W / 47.955392; -120.90544[2]
Grasshopper Peak
South aspect
Highest point
Elevation6,850 ft (2,088 m)[1][2]
Prominence430 ft (131 m)[3]
Isolation2.03 mi (3.27 km)[3]
Coordinates47°57′19″N 120°54′20″W / 47.955392°N 120.90544°W / 47.955392; -120.90544[2]
Geography
Grasshopper Peak is located in Washington (state)
Grasshopper Peak
Grasshopper Peak
Location in Washington
Grasshopper Peak is located in the United States
Grasshopper Peak
Grasshopper Peak
Grasshopper Peak (the United States)
Interactive map of Grasshopper Peak
CountryUnited States
StateWashington
CountyChelan
Protected areaGlacier Peak Wilderness
Parent rangeCascade Range
North Cascades
White Mountains[2]
Topo mapUSGS Mount David
Climbing
Easiest routeScrambling[1]

Grasshopper Peak is a 6,850-foot-elevation (2,088-meter) mountain summit in Chelan County of Washington state.

Grasshopper Peak is located near the southern end of the White Mountains which are a small subrange of the North Cascades.[4] It is set along the boundary of Glacier Peak Wilderness on land administered by the Okanogan–Wenatchee National Forest.[2] Precipitation runoff from the mountain's west slope drains into the White River, whereas the east slope drains into the Napeequa River. Topographic relief is significant as the summit rises 4,800 feet (1,500 meters) above the White River in 1.35 mile (2.17 km) and 4,320 feet (1,320 meters) above the Napeequa in 0.9 mile (1.45 km). This mountain's toponym has not been officially adopted by the United States Board on Geographic Names, so it is not labelled on USGS maps, and will remain unofficial as long as the USGS policy of not adopting new toponyms in designated wilderness areas remains in effect.

Climate

Grasshopper Peak is located in the marine west coast climate zone of western North America.[1] Most weather fronts originate in the Pacific Ocean and travel east toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall.[1] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[1] 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.[1] The months July through September offer the most favorable weather for viewing or climbing this peak.

Geology

See also

References

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