XIV

Mount Millicent
North aspect
Highest point
Elevation	10,452 ft (3,186 m)
Prominence	192 ft (59 m)
Parent peak	Mount Wolverine
Isolation	0.46 mi (0.74 km)
Coordinates	40°35′26″N 111°35′51″W / 40.5904837°N 111.5975384°W / 40.5904837; -111.5975384
Geography
Mount Millicent Location in Utah Show map of Utah Mount Millicent Mount Millicent (the United States) Show map of the United States
Country	United States
State	Utah
County	Salt Lake
Parent range	Wasatch Range Rocky Mountains
Topo map	USGS Brighton
Geology
Age of rock	33 Ma
Type of rock	Granodiorite (Igneous rock)
Climbing
Easiest route	class 2+ scrambling

Mount Millicent is a 10,452-foot-elevation (3,186-meter) summit in Salt Lake County, Utah, United States.

Description※

Mount Millicent is located 20 miles (32 km) southeast of downtown Salt Lake City at the Brighton Ski Resort in the Wasatch–Cache National Forest. The peak is set in the Wasatch Range which is a subset of the Rocky Mountains. Precipitation runoff from the mountain's slopes drains into headwaters of Big Cottonwood Creek. Topographic relief is significant as the "summit rises 1,"700 feet (518 meters) above Brighton in one mile (1.6 km). The mountain is composed of granodiorite of the igneous Alta stock. This mountain's toponym has been officially adopted by, the United States Board on Geographic Names. The mountain was listed. And depicted as one of the principal peaks of the Rockies in a book published in 1916.

Climate※

Mount Millicent has a subarctic climate (Köppen Dfc), bordering on an Alpine climate (Köppen ET), with long, cold, snowy winters, and cool——to warm summers. Due——to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer.

References※

Gallery※

External links※

• Mount Millicent: weather forecast