Liberty Bell Mountain

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Elevation7,720+ ft (2,350+ m) NGVD 29[1]
Prominence200 ft (60 m)[1]
Coordinates48°30′55″N 120°39′28″W / 48.5154151°N 120.6578808°W / 48.5154151; -120.6578808[2]
Liberty Bell Mountain
Liberty Bell Mountain (right) viewed from the east
Highest point
Elevation7,720+ ft (2,350+ m) NGVD 29[1]
Prominence200 ft (60 m)[1]
Coordinates48°30′55″N 120°39′28″W / 48.5154151°N 120.6578808°W / 48.5154151; -120.6578808[2]
Geography
Locationnear Washington Pass,
Chelan / Okanogan counties, Washington, U.S.
Parent rangeNorth Cascades
Topo mapUSGS Washington Pass
Geology
Rock typeGranite
Climbing
First ascent1946, Fred Beckey, Jerry O'Neil, and Charles Welsh
Easiest routeclass 5.6 The Beckey Route

Liberty Bell Mountain is located in the North Cascades, State of Washington, United States, approximately one mile south of Washington Pass on the North Cascades Highway. Liberty Bell is the most northern spire of the Liberty Bell Group, a group of spires that also includes Concord Tower, Lexington Tower, North Early Winters Spire, and South Early Winters Spire.

It is a well-known peak in Washington, although it lacks high prominence and elevation. It is well known for having high-quality alpine climbing, with a short approach since the completion of The Washington Pass Highway. A mixture of high-quality granite and difficult rock has made it a very popular weekend climbing area. Routes range from 5.6 class and grade II to 5.12a class, and grade IV to V.[3]

Liberty Bell Mountain has 18 named traditional climbing routes.[4] Liberty Crack is featured in Fifty Classic Climbs of North America.[5] The first ascent was on September 27, 1946, by Fred Beckey, Jerry O’Neil, and Charles Welsh by way of what is now known as the Beckey route.[4]

Climbing Routes on Liberty Bell Mountain[6]

Liberty Bell Mountain, NW Face

Climate

Liberty Bell Group avalanche chute

Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, 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 snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During the winter months, weather is usually cloudy, but, due to high-pressure systems over the Pacific Ocean that intensify during the summer months, there is often little or no cloud covering the summer.[7] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[7] The North Cascades Highway east of Washington Pass has the distinction of being among the top areas in the United States for most avalanche paths per mile of highway.[8] The months of July through September offer the most favorable weather for viewing or climbing Liberty Bell Mountain.

Geology

References

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