Sawmill Point
Northeast aspect, centered
Highest point
Elevation	9,429 ft (2,874 m)[1]
Prominence	591 ft (180 m)[2]
Parent peak	Colosseum Mountain (12,473 ft)[3]
Isolation	2.58 mi (4.15 km)[3]
Coordinates	36°55′01″N 118°19′14″W / 36.9170122°N 118.3205805°W / 36.9170122; -118.3205805[4]
Geography
Sawmill Point Location in California Show map of California Sawmill Point Sawmill Point (the United States) Show map of the United States
Location	John Muir Wilderness
Country	United States of America
State	California
County	Inyo County
Parent range	Sierra Nevada
Topo map	USGS Aberdeen
Geology
Age of rock	Cretaceous
Mountain type	Fault block
Climbing
First ascent	< 1953
Easiest route	class 3 scrambling[5]

Sawmill Point is a 9,429-foot-elevation (2,874 meter) mountain summit located in Inyo County, California. It is situated 2.6 miles east of the crest of the Sierra Nevada mountain range, in the John Muir Wilderness, on land managed by Inyo National Forest. It is also 10.5 miles (16.9 km) northwest of the community of Independence, and 2.6 miles (4.2 km) east of proximate parent Colosseum Mountain. Topographic relief is significant as the summit rises 4,770 feet (1,450 meters) above Owens Valley in two miles. The Sawmill Pass Trail traverses the east and south slopes of the peak, providing an approach option, and access to the John Muir Trail.

History

The landform's toponym has been officially adopted by the United States Board on Geographic Names.^[4] The peak is named in association with Sawmill Creek, which in turn was named for the sawmill that James W. Smith operated along the creek in the 1870s.^[6] The first recorded ascent of the summit was made by Art J. Reyman and Fred L. Jones on January 11, 1953, by ascending the northeast ridge.^[5] The party was not the first on the summit however, because they found cairns, but no record.

Climate

According to the Köppen climate classification system, Sawmill Point 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 (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the range. Precipitation runoff from this mountain drains into Division and Sawmill creeks, thence Owens Valley.