Styloid Peak

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Elevation6,972 ft (2,125 m)[1]
Prominence412 ft (126 m)[1]
Parent peakDistal Phalanx 7620 ft [2]
Coordinates48°38′13″N 121°06′06″W / 48.63694°N 121.10167°W / 48.63694; -121.10167[1]
Styloid Peak
Styloid Peak seen from Ruby Mountain
Highest point
Elevation6,972 ft (2,125 m)[1]
Prominence412 ft (126 m)[1]
Parent peakDistal Phalanx 7620 ft [2]
Coordinates48°38′13″N 121°06′06″W / 48.63694°N 121.10167°W / 48.63694; -121.10167[1]
Geography
Styloid Peak is located in Washington (state)
Styloid Peak
Styloid Peak
Location in Washington
Styloid Peak is located in the United States
Styloid Peak
Styloid Peak
Location in the United States
LocationNorth Cascades National Park, Washington, U.S.
Parent rangeNorth Cascades
Cascade Range
Topo mapUSGS Ross Dam
Climbing
First ascent1981 John Roper and party[3]

Styloid Peak is the unofficial name of a 6,972-foot (2,125-metre) mountain summit located in North Cascades National Park in Skagit County of Washington state. Its nearest higher peak is Mantis Peak, 0.33 mi (0.53 km) to the west, and Snowfield Peak rises 1.7 mi (2.7 km) to the west.[1] Precipitation runoff from Styloid Peak drains into Neve Creek and McAllister Creek, both tributaries of Thunder Creek. The first ascent of Styloid Peak was made on May 31, 1981, by John Roper and party, on the same day that they climbed Distal Phalanx.[3] Roper, being a doctor, named some of his many first ascents for anatomical parts of the body.

Styloid Peak is located in the marine west coast climate zone of western North America.[3] Most weather fronts originate in the Pacific Ocean, and travel northeast 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. 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.[4] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[4]

Geology

References

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