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Mount Carillon is a 13,553-foot-elevation (4,131 meter) mountain summit located on the crest of the Sierra Nevada mountain range in California.[2] It is situated on the common border of Tulare County with Inyo County, as well as the shared boundary of Sequoia National Park and John Muir Wilderness. It is set above the south shore of Tulainyo Lake, 12.5 miles (20.1 km) west of the community of Lone Pine, 1.25 mile (2.0 km) northeast of Mount Whitney, and 0.7 mile (1.1 km) east-northeast of Mount Russell, the nearest higher neighbor. Topographic relief is significant as it rises approximately 5,180 feet (1,580 meters) above Whitney Portal in approximately two miles. Carillon has subpeaks, unofficially called "The Cleaver" (13,383 ft/4,079 m), 0.4 mile to the northeast, and "Impala" (12,073+ ft/3,680+ m), on the southeast ridge.[1]

Mount Carillon
Mt. Carillon centered at top, south aspect
(Mt. Russell in upper left corner)
Highest point
Elevation13,553 ft (4,131 m) NAVD 88[1]
Prominence233 ft (71 m)[1]
Parent peakMount Russell (14,088 ft)[1]
Isolation0.41 mi (0.66 km)[1]
ListingSierra Peaks Section
Coordinates36°35′33″N 118°16′40″W[2]
Naming
EtymologyCarillon
Geography
Mount Carillon
Mount Carillon
LocationSequoia National Park
Tulare County/Inyo County
California, U.S.
Parent rangeSierra Nevada
Topo mapUSGS Mount Whitney
Geology
Age of rockCretaceous
Mountain typeFault block
Type of rockgranitic
Climbing
First ascent1925, Norman Clyde
Easiest routeSimple scramble class 2+[3]

History


The first ascent of the summit was made in 1925, by Norman Clyde, who is credited with 130 first ascents, most of which were in the Sierra Nevada.[4][5] The peak's name was submitted by Chester Versteeg of the Sierra Club, and officially adopted by the United States Board on Geographic Names in 1937.[2] It is so named because it is shaped like a bell tower, which often houses a carillon.[6]


Climate


According to the Köppen climate classification system, Mount Carillon has an alpine climate.[7] Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks, causing them to drop their moisture in the form of rain or snowfall onto the range (orographic lift). Precipitation runoff from this mountain drains west to the Kern River via Wallace Creek, and east to Owens Valley via Lone Pine Creek.


Climbing


Established climbing routes:[8]




See also



References


  1. "Mount Carillon, California". Peakbagger.com. Retrieved 2021-05-21.
  2. "Mount Carillon". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2021-05-21.
  3. Roper, Steve (1976). The Climber's Guide to the High Sierra. San Francisco: Sierra Club Books. p. 304. ISBN 978-0871561473.
  4. Mendenhall, John D. and Ruth; Johnson, Arthur B.; Gigas, Braeme; Koster, Howard (1954). "A Climber's Guide to the High Sierra". Yosemite Online. Retrieved 2021-11-05.
  5. "Norman Clyde - Mountaineer". OwensValleyHistory.com. Retrieved 2021-11-05.
  6. Gudde, Erwin G. (1969). California Place Names. University of California Press. p. 66. ISBN 978-0520266193.
  7. Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11 (5): 1633. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606.
  8. Secor, R.J. (2009). The High Sierra Peaks, Passes, and Trails (3rd ed.). Seattle: The Mountaineers. p. 254. ISBN 978-0898869712.
  9. Har-Noy, Shay (2009). "Mt. Carillon, Sweet Carillon and Pipe-Line". American Alpine Journal. Retrieved 2021-11-05.





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