Lexington Tower
West aspect of Lexington Tower on the right
(Concord Tower to left)
Highest point
Elevation7,560 ft (2,304 m)[1][2]
Prominence80 ft (24 m)[3]
Parent peakEarly Winters Spires (7,807 ft)[3]
Isolation0.17 mi (0.27 km)[3]
Coordinates48°30′51″N 120°39′27″W / 48.514154°N 120.65743°W / 48.514154; -120.65743[4]
Naming
EtymologyLexington
Geography
Lexington Tower is located in Washington (state)
Lexington Tower
Lexington Tower
Location in Washington
Lexington Tower is located in the United States
Lexington Tower
Lexington Tower
Lexington Tower (the United States)
LocationChelan / Okanogan counties
Washington, U.S.
Parent rangeCascade Range
North Cascades
Topo mapUSGS Washington Pass
Geology
Type of rockGranite
Climbing
First ascent1954
Easiest routeclass 5.7

Lexington Tower is a 7,560-foot-elevation (2,300-meter) granite pinnacle located in the North Cascades, approximately one mile south of Washington Pass along the North Cascades Highway. It is set within the Okanogan–Wenatchee National Forest, on the shared border of Okanogan County and Chelan County in the state of Washington. Lexington Tower is part of the iconic Liberty Bell Group, a group of spires which also includes Liberty Bell Mountain, Concord Tower, and the Early Winters Spires. Precipitation runoff from Lexington Tower drains west into State Creek and east into Early Winters Creek. Topographic relief is significant as the summit rises 2,500 feet (760 meters) above Early Winters Creek in approximately one-half mile.

Climbing routes

The first ascent was made July 5, 1954, by Tim Kelley and Dick McGowan via the North Face.[5]

Rock climbing routes on Lexington Tower:[5][6][7]

  • North Face - class 5.7 - Tim Kelley, Dick McGowan (1954)
  • South Face - class 5.7 - Donald Anderson, Larry Scott (1964)
  • East Face - class 5.9+ - Steve Marts, Donald McPherson (1966)
  • East Gully - Sandy Bill, Cindy Wade Burgner, Frank Tarver (1966)
  • Tooth and Claw - class 5.12a - Steven Risse, Dave Tower (1989)

Climate

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. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[1] 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] 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 cover during the summer.[1] The months July through September offer the most favorable weather for viewing or climbing Lexington Tower.

Geology

The North Cascades feature some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.[9] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[9] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[9] Like many of the peaks of the Washington Pass area, Lexington Tower is composed of granite from the Golden Horn batholith.

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.[9] The U-shaped cross section of the river valleys is a result of recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes that have created the tall peaks and deep valleys of the North Cascades area.

See also

References

  1. 1 2 3 Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  2. ↑ Jeff Smoot (2019), Rock Climbing Washington, Falcon Guides, ISBN 9781493039425, p. 433.
  3. 1 2 3 "Lexington Tower - 7,580' WA". listsofjohn.com. Retrieved 2022-03-13.
  4. ↑ "Lexington Tower, Washington". Peakbagger.com.
  5. 1 2 Beckey, Fred W. (2009). Cascade Alpine Guide: climbing and high routes, Vol. 3, Rainy Pass to Fraser River (3rd ed.). Mountaineers Books. p. 345. ISBN 978-1-59485-136-0.
  6. ↑ Lexington Tower Rock Climbing Mountain Project
  7. ↑ Jeff Smoot (2019), Rock Climbing Washington, Falcon Guides, ISBN 9781493039425, p. 447.
  8. ↑ Avalanche Control.wsdot.wa.gov
  9. 1 2 3 4 Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.