| Highland Peak | |
| Elevation Ft: | 10936 |
| Elevation Ref: | [1] |
| Prominence Ft: | 2456 |
| Isolation Mi: | 10.64 |
| Isolation Ref: | [2] |
| Parent Peak: | Stanislaus Peak (11,233 ft) |
| Map: | California#USA |
| Map Size: | 260 |
| Label Position: | bottom |
| Part Type: | Protected area |
| Part: | Carson–Iceberg Wilderness |
| Country: | United States |
| State: | California |
| Region: | Alpine |
| Region Type: | County |
| Coordinates: | 38.5436°N -119.7555°W |
| Coordinates Ref: | [3] |
| Topo: | USGS Ebbetts Pass |
| Rock: | Rhyolite[4] |
Highland Peak is a prominent 10936feet mountain summit located in the Sierra Nevada mountain range, in Alpine County of northern California, United States.[3] It is situated 3.5 miles east of Ebbetts Pass in the Carson-Iceberg Wilderness, on land managed by Humboldt–Toiyabe National Forest. Although it ranks as the 680th-highest summit in California, it ranks 36th-highest of those with at least 500 meters of topographic prominence.[2] Also, there is no higher peak than Highland Peak to the north within the Sierra Nevada. Highland Peak has a subsidiary South Peak (10824abbr=onNaNabbr=on), with one-half mile separation between summits.[1] The Pacific Crest Trail traverses the western foot of this mountain, providing an approach option. Precipitation runoff from this mountain drains into tributaries of the East Fork Carson River. . Topographic relief is significant as the summit rises over 2900abbr=offNaNabbr=off above Noble Canyon in 1.6 mile (2.6 km).
This mountain's name was applied in 1878 by Lieutenant Montgomery M. Macomb during the Wheeler Survey.[5] The name commemorates the short-lived Highland City, set on the high land between the Carson and Stanislaus watersheds.[6] The mountain's name has been officially adopted by the United States Board on Geographic Names, and a brass USGS benchmark bearing the name was placed at the summit in 1956.[3]
According to the Köppen climate classification system, Highland Peak is located in an alpine climate zone.[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).