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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.
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.
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.
Map of Utah showing the location of the Cedar Mountain Formation (red). The San Rafael Swell is the dome-like structure that the formation jogs around. Base map data courtesy of geodata.gov. Besides dinosaurs, the Cedar Mountain Formation has produced a wealth of small fossils (a.k.a. microfossils), mostly teeth from a variety of vertebrates.
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 ...
Billingsley, G.H., Breed, W.J. and Huntoon, P.W.; 1987; Geologic Map of capitol Reef National Park and vicinity, Utah; Utah Geologic Survey Archived 2006-05-24 at the Wayback Machine (viewed March 25, 2006) Halka Chronic, Roadside Geology of Utah (Mountain Press; 1990) ISBN 0-87842-228-5
The Price River Formation is a geologic formation in Utah. It preserves fossils dating back to the Cretaceous period . The Price River Formation is approximately 200 metres (660 ft) thick at its type locality ( Price River Canyon ) and consists of cliff-forming sandstone and siltstone visible in the Book Cliffs .
Location map of the Paradox Basin [1] The Paradox Basin is an asymmetric foreland basin located mostly in southeast Utah and southwest Colorado, but extending into northeast Arizona and northwest New Mexico. The basin is a large elongate northwest to southeast oriented depression formed during the late Paleozoic Era.