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The Utah Geological Survey is based in Salt Lake City, Utah, United States.It also has an office in Cedar City, Utah. [1]It is a division of the Utah Department of Natural Resources [2] and is an applied scientific agency, which creates, interprets, and provides information about Utah's geological environment, resources and hazards, in order to promote safe, beneficial, and wise land usage.
Freedom Bridge over Starvation Reservoir on U.S. Route 40 in Duchesne County, Utah.. Father Escalante's expedition visited the Uinta Basin in September 1776. 1822–1840 French Canadian trappers Étienne Provost, François le Clerc, and Antoine Robidoux entered the Uinta Basin by way of the Old Spanish Trail and made their fortunes by trapping the many beaver and trading with the Uintah tribe.
The geology of Utah, in the western United States, includes rocks formed at the edge of the proto-North American continent during the Precambrian.A shallow marine sedimentary environment covered the region for much of the Paleozoic and Mesozoic, followed by dryland conditions, volcanism, and the formation of the basin and range terrain in the Cenozoic.
The range has peaks ranging from 11,000 to 13,528 feet (3,353 to 4,123 m), 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.
The San Rafael Swell is a large geologic feature located in south-central Utah, United States about 16 miles (26 km) west of Green River. The San Rafael Swell, measuring approximately 75 by 40 miles (121 by 64 km), consists of a giant dome-shaped anticline of sandstone, shale, and limestone that was pushed up during the Paleocene Laramide ...
The landlocked U.S. state of Utah is known for its natural diversity and is home to features ranging from arid deserts with sand dunes to thriving pine forests in mountain valleys. It is a rugged and geographically diverse state at the convergence of three distinct geological regions: the Rocky Mountains, the Great Basin, and the Colorado Plateau.
Location of the Canyons of the Escalante within Utah. The headwaters of the Escalante River are located on the slopes of the Aquarius Plateau, in Utah's Garfield County, just west of the town of Escalante. The Escalante River begins at the confluence of Birch Creek and North Creek, [1] with the flow of Pine Creek added just below the town. [2]
Mudstones of the Uinta Formation (Uinta "C"), Uintah County, Utah. Uinta Formation (Uinta "C"), Uintah County, Utah. The Uinta Formation is a geologic formation in northeastern Utah. The name appears on a geologic map accompanying the Clarence King Fortieth Parallel report for 1876 [1] but not defined until 1878 [2] as the Uinta Group. As ...
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