| Stevens Peak | |
| Elevation Ft: | 10051 |
| Elevation Ref: | [1] [2] |
| Prominence Ft: | 499 |
| Prominence Ref: | [3] |
| Isolation Mi: | 1.34 |
| Isolation Ref: | [4] |
| Parent Peak: | Red Lake Peak (10,072 ft) |
| Etymology: | J. M. Stevens |
| Map: | California#USA |
| Map Size: | 240 |
| Label Position: | bottom |
| Location: | Alpine County, California, U.S. |
| Range: | Sierra Nevada |
| Coordinates: | 38.7335°N -119.9826°W |
| Coordinates Ref: | [5] |
| Topo: | USGS Carson Pass |
Stevens Peak is a 10,059-foot-elevation (3,066 meter) mountain summit located in Alpine County, California, United States.
This landmark of Hope Valley is set 13miles south of South Lake Tahoe, on land managed by Humboldt–Toiyabe National Forest. Stevens Peak is situated in the Sierra Nevada mountain range, with precipitation runoff from the peak's east slope draining to the West Fork Carson River, whereas the west slope drains into the Upper Truckee River. The summit is situated 1.5miles north of line parent Red Lake Peak, and 3miles north of Carson Pass. Topographic relief is significant as the east aspect rises 2700abbr=offNaNabbr=off above California State Route 88 in 1.5 mile.
John C. Frémont was the first European-American to see Lake Tahoe, during his second exploratory expedition.[6] He and Charles Preuss saw the lake from the summit of what was likely Stevens Peak (or possibly Red Lake Peak) on February 14, 1844.[7] [8]
This landform's toponym has been officially adopted by the U.S. Board on Geographic Names,[5] and has been in use since at least 1896 when published by the Sierra Club.[9] The name honors Alpine County supervisor J. M. Stevens who operated a stage station in Hope Valley from 1864 through 1866.[10] The USGS surveyed this area in 1889 and labelled the geographic feature on their map.[11]
According to the Köppen climate classification system, Stevens Peak is located in an alpine climate zone.[12] 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.