Upper Stillwater Reservoir
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Upper Stillwater Reservoir
Upper Stillwater Reservoir is a large high mountain reservoir on the south slope of the High Uintas in Duchesne County, Utah. The reservoir is part of the Central Utah Project. The reservoir was created in 1987 by the construction of a concrete gravity dam (Upper Stillwater Dam). The architecture of the rolled concrete dam is an attraction for engineers. The reservoir elevation is 8,176 ft, and the mean depth is 103.5 ft. Available fish species include rainbow, brown, and brook trout. The watershed is primarily the Uinta Mountains, the watershed high point being Ostler Peak (12,717 ft). It is estimated that twice or more the reservoir capacity is diverted towards the Wasatch Front annually. The primary use of the water is for irrigation. Recreation The area has one main campground, Rock Creek. The reservoir serves as a popular trailhead into the High Uintas Wilderness Area, with the boundary only one mile north of the dam near the high water line for the r ...
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Duchesne County, Utah
Duchesne County ( ) is a county in the northeast part of the U.S. state of Utah. As of the 2010 United States Census, the population was 18,607. Its county seat is Duchesne, and the largest city is Roosevelt. History Much of Duchesne County was part of the Uintah Reservation, created 1861 by US President Abraham Lincoln as a permanent home of the Uintah and White River Utes. Later the Uncompahgre Utes were moved to the Uintah and newly created Uncompahgre Indian reservations from western Colorado. At the turn of the century, under the Dawes Act, both Indian reservations were thrown open to homesteaders. This was done after allotments of land were made to Indians of the three tribes. The homesteading process was opened on the Uintah on August 27, 1905. Unlike much of the rest of Utah Territory, settlement of the future Duchesne County area did not occur due to LDS Church pressures. It was settled by individuals who obtained 160 acres under the federal Homestead Act. Homesteaders ...
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Wasatch Front
The Wasatch Front is a metropolitan region in the north-central part of the U.S. state of Utah. It consists of a chain of contiguous cities and towns stretched along the Wasatch Range from approximately Provo in the south to Logan in the north, and containing the cities of Salt Lake City, Bountiful, Layton, and Ogden. Geography The Wasatch Front is long and narrow. To the east, the Wasatch Mountains rise abruptly several thousand feet above the valley floors, climbing to their highest elevation of at Mount Nebo (bordering southern Utah Valley). The area's western boundary is formed by Utah Lake in Utah County, the Oquirrh Mountains in Salt Lake County, and the Great Salt Lake in northwestern Salt Lake, Davis, Weber, southeastern Box Elder, and Cache counties. Though most residents of the area live between Ogden and Provo (a distance of ), which includes Salt Lake City proper, the fullest built-out extent of the Wasatch Front is long and an average of wide. Along its ...
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Reservoirs In Utah
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley, and rely on the natural topography to provide most of the basin of the ...
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Lakes Of Duchesne County, Utah
A lake is an area filled with water, localized in a Depression (geology), basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the World Ocean, ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glacier, glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic dra ...
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