| Fletcher Peak | |
| Elevation Ft: | 11410. |
| Elevation Ref: | [1] |
| Prominence Ft: | 130. |
| Prominence Ref: | [2] |
| Isolation Mi: | 1.28 |
| Isolation Ref: | [3] |
| Parent Peak: | Vogelsang Peak (11,493 ft) |
| Etymology: | Arthur G. Fletcher |
| Map: | California#USA |
| Map Size: | 250 |
| Label Position: | bottom |
| Location: | Yosemite National Park Mariposa County, California, U.S. |
| Range: | Cathedral Range, Sierra Nevada |
| Coordinates: | 37.7918°N -119.3358°W |
| Coordinates Ref: | [4] |
| Topo: | USGS Vogelsang Peak |
| Type: | Fault block |
| Rock: | Granodiorite |
| Age: | Cretaceous |
| First Ascent: | Unknown[5] |
| Easiest Route: | Southwest slope |
Fletcher Peak is an 11,410-foot-elevation (3,478 meter) mountain summit located in Yosemite National Park, in Mariposa County, California, United States. It is situated south of Tuolumne Meadows in the Cathedral Range which is a sub-range of the Sierra Nevada mountain range. The mountain rises 1miles south of Tuolumne Pass, 1.3miles northeast of proximate parent Vogelsang Peak and 1.8miles northwest of line parent Parsons Peak.[3] Topographic relief is significant as the summit rises 1250abbr=offNaNabbr=off above Fletcher Lake in 0.38miles. Precipitation runoff from this landform drains south to the Merced River via Fletcher Creek.
Fletcher Creek and Fletcher Lake were named in 1895 by Lieutenant Nathaniel Fish McClure to honor Arthur G. Fletcher, deputy fish commissioner of California's State Board of Fish Commissioners, who directed the stocking of fish in the streams and lakes of Yosemite National Park.[6] The peak was named in association, and this geographical feature's toponym was officially adopted in 1932 by the U.S. Board on Geographic Names.[4] The landform had been named "Baker Peak" prior to the Fletcher name, for a Mr. Baker who was a cook at nearby Boothe Lake Camp.[4] [7]
According to the Köppen climate classification system, Fletcher Peak is located in an alpine climate zone.[8] 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 (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the range.