| Mount Carillon | |
| Elevation Ft: | 13,559 |
| Elevation Ref: | [1] |
| Prominence Ft: | 233 |
| Isolation Mi: | 0.41 |
| Parent Peak: | Mount Russell (14,088 ft) |
| Etymology: | Carillon |
| Listing: | Sierra Peaks Section |
| Map: | California#USA |
| Map Size: | 210 |
| Label Position: | left |
| Location: | Sequoia National Park California, U.S. |
| Range: | Sierra Nevada |
| Coordinates: | 36.5924°N -118.2779°W |
| Coordinates Ref: | [2] |
| Topo: | USGS Mount Whitney |
| Rock: | granitic |
| Type: | Fault block |
| Age: | Cretaceous |
| First Ascent: | 1925, Norman Clyde |
| Easiest Route: | Simple scramble [3] |
Mount Carillon is a 13559feet 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, west of the community of Lone Pine, 1.25miles northeast of Mount Whitney, and 0.7miles east-northeast of Mount Russell, the nearest higher neighbor. Topographic relief is significant as it rises approximately 5180abbr=offNaNabbr=off above Whitney Portal in approximately two miles. Carillon has subpeaks, unofficially called "The Cleaver" (13383feet, 0.4 mile to the northeast, and "Impala" (12,073+ ft/3,680+ m), on the southeast ridge.[1]
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]
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.
Established climbing routes:[8]