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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.
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.
268,760 (in 2017–2018 FY) [2] Operator. Utah State Parks. Website. Official website. Goblin Valley State Park is a state park of Utah, in the United States. The park features thousands of hoodoos, referred to locally as goblins, [3] which are formations of mushroom-shaped rock pinnacles, some as tall as several yards (meters).
Arches National Park. 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.
Devil's Slide (Utah) Coordinates: 41°03′49″N 111°32′53″W. October 2013. Devil's Slide is a geological formation located near the border of Wyoming in northern Utah 's Weber Canyon, near the community of Croydon in Morgan County, Utah, United States. The Slide consists of two parallel limestone strata that have tilted to lie vertical ...
Kolob Canyons from the end of Kolob Canyons Road. Stream erosion has incised the Kolob Plateau to form canyons that expose the red-orange colored Navajo Sandstone and other formations. The geology of the Zion and Kolob canyons area includes nine known exposed formations, all visible in Zion National Park in the U.S. state of Utah.
75000165. Added to NRHP. November 03, 1975 [1] Hole in the Rock is a narrow and steep crevice in the western rim of Glen Canyon, in southern Utah in the western United States. Together with another canyon on the eastern side of the Colorado River, it provided a route through what would otherwise be a large area of impassable terrain.
Nearly 10,000 feet (3,000 m) of sedimentary strata are found in the Capitol Reef area, representing nearly 200 million years of geologic history of the south-central part of the U.S. state of Utah. These rocks range in age from Permian (as old as 270 million years old) to Cretaceous (as young as 80 million years old.)
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