Reids Peak | |
---|---|
Highest point | |
Elevation | 11,724 ft (3,573 m) [1] |
Prominence | 670 ft (204 m) [1] |
Parent peak | Bald Mountain (11,948 ft) [1] |
Isolation | 0.59 mi (0.95 km) [2] |
Coordinates | 40°42′23″N110°54′45″W / 40.7063807°N 110.9124702°W [3] |
Geography | |
Country | United States of America |
State | Utah |
County | Summit |
Parent range | Uinta Mountains Rocky Mountains |
Topo map | USGS Mirror Lake |
Geology | |
Rock age | Late Precambrian |
Rock type | Quartz arenite |
Climbing | |
Easiest route | class 2+ scrambling [1] |
Reids Peak is an 11,724-foot-elevation (3,573-meter) mountain summit in Summit County, Utah, United States.
Reids Peak is located 50 miles (80 km) east of Salt Lake City in the Uinta-Wasatch-Cache National Forest. [2] It is situated in the western Uinta Mountains which are a subrange of the Rocky Mountains. Precipitation runoff from this mountain drains north into headwaters of the Weber River. [2] Topographic relief is significant as the summit rises 2,300 feet (701 meters) above the Weber River in one mile (1.6 km). Access to the mountain is via the Mirror Lake Highway. The mountain was first named "Reeds Peak" in 1875, and the present spelling of the toponym was officially adopted in 1932 by the U.S. Board on Geographic Names. [3] The peak is named after an early explorer of this region. [4] William "Toopeechee" Reed was an early pioneer of this region who founded Reed Trading Post in 1828, making this the first permanent non-Indian residence and business in what would become the State of Utah.
Reids Peak is composed of metasedimentary rock of the Mount Watson Formation. [5] Fluvial sediment processes deposited a sequence of nearly white quartz arenite and subarkose interbedded with minor amounts of pale-red arkosic arenite and grayish-green shale during the Late Precambrian. [6] The Uintas were uplifted during the Laramide orogeny about 70 to 50 million years ago. The area around Reids Peak and Bald Mountain became an ice cap during glaciation of the Ice age, transforming these peaks into nunataks. [7] Numerous glacial cycles during the Quaternary Period sculpted the peak and scoured the surrounding land forming many depressions that are now lakes. Viewed from the summit, as many as 70 lakes can be counted. [8]
Based on the Köppen climate classification, Reids Peak is located in a subarctic climate zone with cold snowy winters and mild summers. [9] Tundra climate characterizes the summit and highest slopes.
The Uinta Mountains are an east-west trending mountain range in northeastern Utah extending a short distance into northwest Colorado and slightly into southwestern Wyoming in the United States. As a subrange of the Rocky Mountains, they are unusual for being the highest range in the contiguous United States running east to west, and lie approximately 100 miles (160 km) east of Salt Lake City. The range has peaks ranging from 11,000 to 13,528 feet, with the highest point being Kings Peak, also the highest point in Utah. The Mirror Lake Highway crosses the western half of the Uintas on its way to Wyoming. Utah State Route 44 crosses the east end of the Uintas between Vernal and Manila.
Bald Mountain is a 11,949-foot (3,642 m) peak in the western Uinta Mountain Range in the Uinta-Wasatch-Cache National Forest on the border between Summit and Wasatch counties in northeastern Utah, United States.
The High Uintas Wilderness is a wilderness area located in northeastern Utah, United States. The wilderness covers the Uinta Mountains, encompassing parts of Duchesne and Summit counties. Designated as a wilderness in 1984, the area is located within parts of Ashley National Forest and Uinta-Wasatch-Cache National Forest, managed by the U.S. Forest Service. The highest peak in Utah, Kings Peak, lies within the wilderness area along with some of Utah's highest peaks, particularly those over 13,000 feet.
Ostler Peak is a 12,718-foot elevation (3,876 m) mountain summit located in Summit County, Utah, United States.
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