Geography Of Utah
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Geography Of Utah
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 tree, 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. Overview Utah covers an area of . It is one of the Four Corners states and is bordered by Idaho in the north, Wyoming in the north and east, by Colorado in the east, at a single point by New Mexico to the southeast, by Arizona in the south, and by Nevada in the west. Only three U.S. states (Utah, Colorado, and Wyoming) have exclusively latitude and longitude lines as boundaries. One of Utah's defining characteristics is the variety of its terrain. Running down the middle of the state's northern third is the Wasatch Range, which rises to heights of almost above sea level. Utah is home to world-renowned ski resorts made popula ...
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Utah Counties
There are 29 County (United States), counties in the U.S. state of Utah. There were originally seven counties established under the provisional State of Deseret in 1849: Davis County, Utah, Davis, Iron County, Utah, Iron, Sanpete County, Utah, Sanpete, Salt Lake County, Utah, Salt Lake, Tooele County, Utah, Tooele, Utah County, Utah, Utah, and Weber County, Utah, Weber. The Utah Territory, Territory of Utah was created in 1851 with the first territorial legislature meeting from 1851–1852. The first legislature re-created the original counties from the State of Deseret under territorial law as well as establishing three additional counties: Juab County, Utah, Juab, Millard County, Utah, Millard, and Washington County, Utah, Washington. All other counties were established between 1854 and 1894 by the Utah Territorial Legislature under territorial law except for the last two counties formed, Daggett County, Utah, Daggett and Duchesne County, Utah, Duchesne. They were cr ...
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Basin And Range Province
The Basin and Range Province is a vast physiographic region covering much of the inland Western United States and northwestern Mexico. It is defined by unique basin and range topography, characterized by abrupt changes in elevation, alternating between narrow faulted mountain chains and flat arid valleys or basins. The physiography of the province is the result of tectonic extension that began around 17 million years ago in the early Miocene epoch. The numerous ranges within the province in the United States are collectively referred to as the "Great Basin Ranges", although many are not actually in the Great Basin. Major ranges include the Snake Range, the Panamint Range, the White Mountains, and the Sandia Mountains. The highest point fully within the province is White Mountain Peak in California, while the lowest point is the Badwater Basin in Death Valley at . The province's climate is arid, with numerous ecoregions. Most North American deserts are located within it. The ...
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Great Basin National Park
Great Basin National Park is an American national park located in White Pine County in east-central Nevada, near the Utah border, established in 1986. The park is most commonly entered by way of Nevada State Route 488, which is connected to U.S. Routes 6 and 50 by Nevada State Route 487 via the small town of Baker, the closest settlement. The park derives its name from the Great Basin, the dry and mountainous region between the Sierra Nevada and the Wasatch Mountains. Topographically, this area is known as the Basin and Range Province. The park is located about north of Las Vegas and protects . The park is notable for its groves of ancient bristlecone pines, the oldest known living non-clonal organisms; Lehman Caves; Wheeler Peak Glacier, below Wheeler Peak; and some of the darkest night skies in the contiguous United States. President Warren G. Harding created Lehman Caves National Monument by presidential proclamation on January 24, 1922. The monument and its surroundi ...
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Deep Creek Range
The Deep Creek Range, (often refereed to as the Deep Creek Mountains (Goshute: Pi'a-roi-ya-bi), are a mountain range in the Great Basin located in extreme western Tooele and Juab counties in Utah, United States. The range trends north-south (with a curl to the west at the southern end, 16% of range in White Pine County, Nevada), and is composed of granite in its central highest portion. The valley to the east is Snake Valley, and to the west is Deep Creek Valley. Nearby communities include Callao, Utah to the east and the community of Ibapah and the lands of the Confederated Tribes of the Goshute Reservation to the west. The highest point in the Deep Creek Range is Ibapah Peak, an ultra prominent peak, which rises to . Other peaks include Haystack Peak at and Red Mountain at . The range is the source of several perennial streams and supports a diverse coniferous forest, with an "island" of alpine tundra on the highest summits. The range has a vertical relief of above the salt ...
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Snake Range
The Snake Range is a mountain range in White Pine County, Nevada, United States. The south-central portion of the range is included within Great Basin National Park, with most of the remainder included within the Humboldt-Toiyabe National Forest. The range reaches a maximum elevation of at the summit of Wheeler Peak, the tallest independent mountain within Nevada and the second highest point within the state (the highest point being Boundary Peak). The range also contains four of the five highest mountain peaks in Nevada, including all peaks greater than except for Boundary Peak. Geography Typical of other ranges in the Basin and Range Province, the Snake Range runs in a north-south direction, for approximately . To the west are Spring Valley and the Schell Creek Range, and to the east across the Utah border are Snake Valley and the Confusion Range. Sacramento Pass () is where U.S. Route 6- 50, the "Loneliest Highway in America", crosses the range. It is the principal me ...
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Groundwater
Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, perma ...
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Snake Valley (Great Basin)
Snake Valley is a north-south trending valley that straddles the Nevada–Utah border in the central Great Basin. It is bound by the Snake Range and the Deep Creek Mountains to the west and the Confusion Range to the east. The valley is the gateway to Great Basin National Park and Lehman Caves, which are located in the western part of the valley and on the southern Snake Range. People Though it is relatively isolated from civilization today, the human presence in Snake Valley goes back 12,000 years. The oldest accessible evidence of this is the Baker Archeological Site, a Fremont culture habitat maintained by the BLM. Current communities in the valley include Baker in Nevada and Garrison, Burbank, Eskdale, Callao, Partoun, Trout Creek, Gandy, and Border in Utah. Today, the main industries in the valley are farming and ranching, especially sheep ranching. Water Snake Valley is noted for a water project involving the Las Vegas Valley, that would target the underlying Basin ...
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Great Salt Lake Desert
The Great Salt Lake Desert (colloquially referred to as the West Desert) is a large dry lake in northern Utah, United States, between the Great Salt Lake and the Nevada border. It is a subregion of the larger Great Basin Desert, and noted for white evaporite Lake Bonneville salt deposits including the Bonneville Salt Flats. Description Several small mountain ranges occupy the edges of the desert, such as the Cedar Mountains, Lakeside Mountains, Silver Island Mountains, Hogup Mountains, Grassy Mountains, and Newfoundland Mountains. On the western edge of the desert, just across the border in Nevada, stands Pilot Peak in the Pilot Range. The desert is cool during the winter and includes unusual plants adapted to the dry conditions. Most of the desert receives less than of annual precipitation. The salt crust covering the desert reforms yearly when the rain evaporates. The military's Utah Test and Training Range is in the northern portion of the desert. The lowest part of ...
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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 km²), 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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University Of Utah Press
The University of Utah Press is the independent publishing branch of the University of Utah and is a division of the J. Willard Marriott Library. Founded in 1949 by A. Ray Olpin, it is also the oldest university press in Utah. The mission of the press is to "publish and disseminate scholarly books in selected fields, as well as other printed and recorded materials of significance to Utah, the region, the country, and the world." The University of Utah Press publishes in the following general subject areas: anthropology, archaeology, Mesoamerican studies, American Indian studies, natural history, nature writing, poetry, Utah and Western history, Mormon studies, Utah and regional guidebooks, and regional titles. The press employs seven people full-time and publishes 25 to 35 titles per year. The press has over 450 books currently in print. Prizes The University of Utah Press awards five annual or biennial prizes for scholarly and/or literary manuscripts. *The Wallace Stegner ...
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Rush Lake (Tooele County, Utah)
Rush Lake (also known as Rush Reservoir) is a shallow saline lake in Tooele County in the United States, U.S. U.S. state, state of Utah. It is a remnant of Lake Bonneville, an ancient postglacial inland sea (geology), inland sea that covered much of the western United States during the last glacial period, Ice Ages. The lake is a natural impoundment of a stream that drains into the Great Salt Lake. Rush Lake varies in size, evaporating at about per year, although occasional floods refill the lake. The average surface elevation is . Geography The lake is located in a broad valley named Rush Valley near the town of Stockton, Utah, Stockton and several miles south of Tooele, and is fed by snowmelt from six mountain ranges. These are the Sheeprock Mountains in the south, the East Tintic Mountains to the southeast, the Oquirrh Mountains to the east, South Mountain to the north, the Stansbury Mountains to the northwest and west, and the Onaqui Mountains to the southwest. The runoff from ...
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Sevier Lake
Sevier Lake is an intermittent and endorheic lake which lies in the lowest part of the Sevier Desert, Millard County, Utah. Like Great Salt Lake and Utah Lake, it is a remnant of Pleistocene Lake Bonneville. Sevier Lake is fed primarily by the Beaver River (Utah), Beaver and Sevier River, Sevier rivers, and the additional inflow is from the lake's watershed that is part of the :Escalante-Sevier region, Escalante–Sevier hydrologic subregion. The lake has been mostly dry throughout recorded history and is a source of wind-blown dust. History The first recorded observation was in 1872, which stated that the lake's surface area was , salinity was measured at 86 parts per thousand, two and a half times that of the ocean, and maximum depth was . In January 1880, the lake was nearly dry and had been so for the past one or two years. The Sevier River, which once flowed to the lake, is now largely diverted for irrigation. In 1987 however, the lake was again similar to the recorded desc ...
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