Dugway Range
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Dugway Range
The Dugway Range is a 13-mile (21 km) longUtah DeLorme Atlas & Gazetteer, pp. 23, 31. mountain range located in central-south Tooele County, Utah, on the Juab County north border. The Dugway Range extends northwesterly into the south of the Great Salt Lake Desert, the region at the west and southwest of the Great Salt Lake, about three times its area, a region of a flat white, salt flat, flat alluvial plains, and some alluvial mountain range pediments. It is the location of the Bonneville Salt Flats. The long Granite Mountain lies Utah DeLorme Atlas, p. 23. north of the range; the mountain is a traveler's landmark with landscape sketches made in the 1800s (1859). Description The Dugway Range is about long, with a spur on the south terminus. The spur extends southwest into the Great Salt Lake Desert. The spur, Dugway Ridge, is about long, south-southwest trending mostly, and ends at Pyramid Peak, . The highpoint of the range is Castle Mountain (Utah), ), near the ...
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Thomas Range
The Thomas Range is a mountain range of north central Juab County of western Utah, United States. Topaz Mountain is in the southern part of the range and Spor Mountain lies to the southwest.''Utah Atlas & Gazeteer,'' DeLorme, 9th ed., 2014, pp. 30-1 References External links Spor Mountain beryllium mines article at NASA Earth Observatory, July 16, 2021 Slides of the Fluorspar, Beryllium, and Uranium Deposits at Spor Mountain, Utah by David A. Lindsey USGS The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, a ... Mountain ranges of Utah Mountain ranges of Juab County, Utah {{Utah-geo-stub ...
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Fish Springs Range
The Fish Springs Range is a long narrow, and north-trending mountain range located in center-west Juab County, Utah. The northeast of the range borders the Fish Springs National Wildlife Refuge; the entire east of the range borders the Fish Springs Flat, where the east region of the flat borders the Thomas Range. The Fish Springs Range lies at the south of the Great Salt Lake Desert; southwards, as well as southwest and southeastwards, north-trending valleys and mountain ranges drain northwards to the Great Salt Lake Desert. The sequence of these landforms west-to-east, are Snake Valley (Great Basin), Confusion Range, Tule Valley-(Fish Springs Range-north), House Range, Whirlwind Valley, and Drum Mountains. The south of the range borders the north of Tule Valley. Range description The Fish Springs Range is north-south trending, linear, narrow (mostly 3 to 4-mi wide), the range is veryslightly "arc-shaped", and curved, to the west. A small sub-range, Middle Range, lies 6.5-mi ...
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Mountain Ranges Of Juab County, Utah
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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Mountain Ranges Of Tooele County, Utah
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Utah State Route 196
State Route 196 is a north-south state highway located entirely in Tooele County, Utah that begins at SR-199 and ends at I-80. It passes through Skull Valley, and was added to the state highway system in 1998 to prevent the Skull Valley Band of Goshute Indians from using their reservation to store nuclear waste. Route description SR-196 begins at the junction with SR-199 near the control gate at Dugway Proving Ground. The route travels north through the Skull Valley Indian Reservation and past the ghost town of Iosepa; also, mostly the east side of Skull Valley, at the west foothills of the Stansbury Mountains. The route ends at the junction with I-80 at the Rowley Junction interchange. History Skull Valley Road, then an unimproved dirt trail, was part of the Lincoln Highway from its creation in 1913 until about 1920, when an improved gravel road over Johnson Pass (present SR-199) was built with the help of a donation from Carl G. Fisher. By the 1950s, ...
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Utah State Route 199
State Route 199 (SR-199) is a state highway in the U.S. state of Utah. Spanning , it connects SR-196 and the Dugway Proving Ground with SR-36 between Rush Valley and the Deseret Chemical Depot. Route description State Route 199 begins at the junction with SR-196 near the control gate at Dugway Proving Ground in Skull Valley. The route travels northeast for , passing through the community of Terra before turning east and climbing over Johnson Pass in the Onaqui Mountains. Descending out of the mountains, the route continues to the east through the town of Clover before ending at SR-36, just north of the Deseret Chemical Depot. History In 1920, an improved gravel road over Johnson Pass from St. John to Orr's Ranch (just north of the modern-day terminus of SR-199) was built with the help of a donation from Carl G. Fisher, replacing Skull Valley Road (an unimproved dirt trail) as part of the Lincoln Highway.Kevin J. Patrick and Robert E. Wilson, Indiana University of Penns ...
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Granite Mountain (Tooele County, Utah)
Granite Mountain may refer to: Mountains Canada * Granite Mountain (British Columbia), in the Rossland Range of the Monashee Mountains United States * Granite Mountain (Arizona), in Yavapai County *Granite Mountain (Arkansas), near Little Rock * Granite Mountain (California), in Anza-Borrego Desert State Park *Granite Mountain (Texas), in Burnet County *Granite Mountain (Salt Lake County, Utah), in the Wasatch Range *Granite Mountain (Washington), several peaks, including: **Granite Mountain (King County, Washington) ** Granite Mountain (Wenatchee Mountains) **Granite Mountain (Whatcom County, Washington) Settlements *Granite Mountain, Alaska, a place in Alaska **Granite Mountain Air Station *Granite Mountain, a neighborhood in Little Rock, Arkansas Other uses * Granite Mountain charter school, Lucerne Valley, California, US * ''Only the Brave'' (2017 film) (working title ''Granite Mountain''), an American film See also *Granite Mountains (other) *Granite Peak Mountai ...
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Bonneville Salt Flats
The Bonneville Salt Flats are a densely packed salt pan in Tooele County in northwestern Utah. A remnant of the Pleistocene Lake Bonneville, it is the largest of many salt flats west of the Great Salt Lake. It is public land managed by the Bureau of Land Management and is known for land speed records at the Bonneville Speedway. Access to the Flats is open to the public. The Flats are about 12 miles (19 km) long and 5 miles (8 km) wide, with a crust almost 5 ft (1.5m) thick at the center and less than one inch (2.5 cm) towards the edges. It is estimated to hold 147 million tons of salt, approximately 90% of which is common table salt. History Geologist Grove Karl Gilbert named the area after Benjamin Bonneville, a U.S. Army officer who explored the Intermountain West in the 1830s. In 1907, Bill Rishel and two local businessmen tested the suitability of the salt for driving by taking a Pierce-Arrow onto its surface. A railway line across the Flats was completed in 1910, ma ...
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Salt Pan (geology)
Natural salt pans or salt flats are flat expanses of ground covered with salt and other minerals, usually shining white under the sun. They are found in deserts and are natural formations (unlike salt evaporation ponds, which are artificial). A salt pan forms by evaporation of a water pool, such as a lake or pond. This happens in climates where the rate of water evaporation exceeds the rate of that is, in a desert. If the water cannot drain into the ground, it remains on the surface until it evaporates, leaving behind minerals precipitated from the salt ions dissolved in the water. Over thousands of years, the minerals (usually salts) accumulate on the surface. These minerals reflect the sun's rays (through radiation) and often appear as white areas. Salt pans can be dangerous. The crust of salt can conceal a quagmire of mud that can engulf a truck. The Qattara Depression in the eastern Sahara Desert contains many such traps which served as strategic barriers during World ...
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Great Salt Lake
The Great Salt Lake is the largest saltwater lake in the Western Hemisphere and the eighth-largest terminal lake in the world. 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 prehistoric body of water that covered much of western Utah. The area of the lake can fluctuate substantially due to its low average depth of . In the 1980s, it reached a historic high of , and the West Desert Pumping Project was established to mitigate flooding by pumping water from the lake into the nearby desert. In 2021, after years of sustained drought and increased water diversion upstream of the lake, it fell to its lowest recorded area at 950 square miles (2,460 kmĀ²), falling below the previous low set in 1963. Continued shrinkage could turn the lake into a bowl of toxic dust, poisoning the air around Salt Lake City. The lake's three major tributaries, the ...
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Utah
Utah ( , ) is a state in the Mountain West subregion of the Western United States. Utah is a landlocked U.S. state bordered to its east by Colorado, to its northeast by Wyoming, to its north by Idaho, to its south by Arizona, and to its west by Nevada. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin. Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo and Ute. The Spanish were the first Europe ...
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Fish Springs National Wildlife Refuge
Fish Springs National Wildlife Refuge is at the southern end of the Great Salt Lake Desert, part of the Great Basin in Juab County, Utah, United States. The Refuge is managed by the United States Fish and Wildlife Service. As an oasis in the Great Basin Desert in western Utah, Fish Springs serves a variety of species including fish, migratory birds, deer, coyotes, pronghorn, cougars and other native species. The reserve can be reached by paved road from Lynndyl to Topaz Mountain and then by improved dirt road to the Pony Express Road/Lincoln Highway improved dirt road which runs through the Refuge. The Refuge also is a recreational area for permitted outdoor activities. The Fish Springs Range runs north to south and is immediately west of the Wildlife Refuge. Fish Springs started as a Pony Express and Overland Stage station, and got its name from the fish that populated the springs, which were reported to be over in length. The fish are left over from ancient Lake Bonneville ...
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