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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.
Lake Bonneville was the largest Late Pleistocene paleolake in the Great Basin of western North America. It was a pluvial lake that formed in response to an increase in precipitation and a decrease in evaporation as a result of cooler temperatures. The lake covered much of what is now western Utah and at its highest level extended into present ...
Comstock Lode geologic map, north. ... (then western Utah Territory), ... This structure was a departure from that of the late 1800s, when upwards of 400 mining ...
The Pogonip Group is an Ordovician period geologic group located in southern Nevada and in Utah. Geology. Its subunits in Nevada, from youngest/later to oldest/earlier, are: Goodwin Limestone — 1,800 metres (5,900 ft) thick; Ninemile Formation — 550 metres (1,800 ft) thick; Antelope Valley Limestone — 1,100 metres (3,600 ft) thick
View from Utah Highway 12 of Grand Staircase–Escalante National Monument The Cockscomb at right runs along Cottonwood Canyon Road. The Grand Staircase is an immense sequence of sedimentary rock layers that stretch south from Bryce Canyon National Park and Grand Staircase–Escalante National Monument, through Zion National Park, and into Grand Canyon National Park.
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 Cedar Mountain Formation is the name given to a distinctive sedimentary geologic formation in eastern Utah, spanning most of the early and mid- Cretaceous. The formation was named for Cedar Mountain in northern Emery County, Utah, where William Lee Stokes first studied the exposures in 1944. [1]
Salt Lake City and Ogden. The Great Salt Lake is the largest saltwater lake in the Western Hemisphere [1] and the eighth-largest terminal lake in the world. [2] It lies in the northern part of the U.S. state of Utah and has a substantial impact upon the local climate, particularly through lake-effect snow. It is a remnant of Lake Bonneville, a ...
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