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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.
Biek, Robert F.; Grant C. Willis; Micheal D. Hylland; Hellmut H. Doelling (August 2003). "Geology of Zion National Park, Utah". In Paul B. Anderson (ed.). Geology of Utah's Parks and Monuments. Bryce Canyon Natural History Association and Utah Geological Association. ISBN 1-882054-10-5. GORP. "Zion National Park Geology". GORP / Orbitz Away LLC.
Arches National Park is a national park of the United States in eastern Utah.The park is adjacent to the Colorado River, 4 mi (6 km) north of Moab, Utah.The park contains more than 2,000 natural sandstone arches, including the well-known Delicate Arch, which constitute the highest density of natural arches in the world.
Thomas H. Morris, Vicky Wood Manning, and Scott M. Ritter, "Geology of Capitol Reef National Park, Utah" in Geology of Utah's Parks and Monuments, Douglas A. Sprinkel, Thomas C. Chindsey, Jr., and Paul B. Anderson, Editors (Salt Lake City; Utah Geological Association; 2003) ISBN 1-882054-10-5
The park is located in southwestern Utah about 50 miles (80 km) northeast of and 1,000 feet (300 m) higher than Zion National Park. [6] [7]Bryce Canyon National Park lies within the Colorado Plateau geographic province of North America and straddles the southeastern edge of the Paunsaugunt Plateau west of Paunsaugunt Faults (Paunsaugunt is Paiute for "home of the beaver"). [8]
The eight National Monuments in the state of Utah are: Bears Ears National Monument near San Juan County [2] Cedar Breaks National Monument near Cedar City [1] Dinosaur National Monument near Vernal [1] Grand Staircase–Escalante National Monument near Kanab [3] Hovenweep National Monument near Bluff [1] Natural Bridges National Monument near ...
Goblin Valley State Park and Bryce Canyon National Park, also in Utah about 190 miles (310 km) to the southwest, contain some of the largest occurrences of hoodoos in the world. The park lies within the San Rafael Desert on the southeastern edge of the San Rafael Swell, north of the Henry Mountains.
The SITLa plots within the monument were exchanged for federal lands elsewhere in Utah, plus equivalent mineral rights and $50 million cash by an act of Congress, the Utah Schools and Lands Exchange Act of 1998, supported by Democrats and Republicans, and signed into law as Public Law 105–335 on October 31, 1998. [20]
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