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Antelope Valley (southwest Millard County, Utah)
The Antelope Valley of southwest Millard County, Utah, United States, is a small long valley, adjacent the Ferguson Desert and southwest of Sevier Lake. The valley is just east of the Nevada border, with Snake Valley and the Burbank Hills. The other Antelope Valley of Utah occurs east in the Great Basin, in southeast Emery County and extending into adjacent Wayne County. The Desert Biosphere Reserve forms the entire southeast, central & south valley border, where the small, low elevation arid Tunnel Springs Mountains are located.Utah Atlas & Gazetteer, p. 40. Description The Antelope Valley is southwest-northeast trending with a drainage northeast into the Ferguson Desert area. The valley also drains from the northeast flank of the Mountain Home Range adjacent the Nevada border to the southwest. The valley is narrow, only about , at its widest. Access Utah State Route 21 transects the upper region of the valley at the alluvial fans of the Mountain Home Range. Route 21 crossi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Basin
The Great Basin is the largest area of contiguous endorheic basin, endorheic watersheds, those with no outlets, in North America. It spans nearly all of Nevada, much of Utah, and portions of California, Idaho, Oregon, Wyoming, and Baja California. It is noted for both its arid climate and the basin and range topography that varies from the North American low point at Badwater Basin in Death Valley to the highest point of the contiguous United States, less than away at the summit of Mount Whitney. The region spans several physical geography, physiographic divisions, biomes, ecoregions, and deserts. Definition The term "Great Basin" is applied to hydrography, hydrographic, ecology, biological, floristic province, floristic, physiographic, topography, topographic, and Ethnography, ethnographic geographic areas. The name was originally coined by John C. Frémont, who, based on information gleaned from Joseph R. Walker as well as his own travels, recognized the hydrographic nature o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Emery County, Utah
Emery County is a county in east-central Utah, United States. As of the 2010 United States Census, the population was 10,976. Its county seat is Castle Dale, and the largest city is Huntington. History Prehistory Occupation of the San Rafael region dates back thousands of years to include people of the Desert Archaic Culture who were followed by those of the Fremont culture who inhabited present-day Emery County through the sixth through thirteenth centuries AD. Evidence of these civilizations is extant in numerous pictograph and petroglyph panels, such as those in Temple Mountain Wash, Muddy Creek, Ferron Box, Black Dragon Canyon, and Buckhorn Wash - all sites listed in the National Register of Historic Places. Ute Indians also occupied sites in Castle Valley, Old Spanish Trail The first non-indigenous persons to view Castle Valley were Spanish Traders and Explorers. The first of record was Silvestre Vélez de Escalante; in 1776, he crossed northern Utah through the Uintah ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Utah
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Valleys Of Utah
This is a list of valleys of Utah. Valleys are ordered alphabetically by county and then for the entire state. Beaver County * Beaver Valley (Utah) * Hamlin Valley * Milford Valley * Pine Valley (Beaver, Millard, Iron counties, Utah) (in Beaver, north Iron, and south Millard counties) * Wah Wah Valley Box Elder County * Bear River Valley * Blue Creek Valley * Curlew Valley * Junction Valley * Upper Raft River Valley Cache County * Ant Valley * Cache Valley Carbon County * Castle Valley (Carbon, Emery, and Sevier counties, Utah) * Emma Park * Whitmore Park Daggett County * Lucerne Valley Davis County * Salt Lake Valley Duchesne County * Pleasant Valley * Roosevelt Valley Emery County * Antelope Valley (Wayne-Emery counties, Utah) * Castle Valley (Carbon, Emery, and Sevier counties, Utah) * Gunnison Valley (Emery and Grand counties, Utah) * Joe's Valley * San Rafael Valley Garfield County * Bear Valley Junction, Utah * Circle Valley' * Johns Valley ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Milford, Utah
Milford is a city in Beaver County, Utah, United States. The population was 1,409 at the 2010 census and 1,394 as of a 2019 Census Bureau estimate. History Although settlers had established ranches in the area in the 1870s, Milford was not developed until after construction of the San Pedro, Los Angeles and Salt Lake Railroad in 1880, which established a station here. Milford is a constructed name, an abbreviated form of mill and ford. During the Great Depression, workers from a nearby Civilian Conservation Corps camp constructed a road from Milford to Beaver, to improve connections. Milford Flat Wildfire Lightning caused a massive wildfire to start near Milford at 3:45 p.m. Friday, July 6, 2007. On July 8 the fire was declared the largest in Utah's history, having burned more than . Demographics As of the 2000 census, there were 1,451 people, 484 households, and 357 families residing in the city. The population density was 753.7 people per square mile (290.3/km2). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frisco, Utah
Frisco is a ghost town in Beaver County, Utah, United States. It was an active mining camp from 1879 to 1929. At its peak in 1885, Frisco was a thriving town of 6,000 people. History Frisco developed as the post office and commercial center for the San Francisco Mining District, and was the terminus of the Utah Southern Railroad extension from Milford. The Horn Silver Mine was discovered in 1875, and had produced $20,267,078 worth of ore by 1885. By 1885, over $60,000,000 worth of zinc, copper, lead, silver, and gold had been transported from Frisco from the many mines in the area. With 23 saloons, Frisco was known as the wildest town in the Great Basin. Murder was common, and drinking water had to be freighted in. Frisco's fortunes changed suddenly on February 13, 1885, when the Horn Silver Mine caved in completely. It was an unconventional mine, an open pit deep braced with timbers, and could have collapsed at any time. In 1905 a Mormon ward was organized, but in 1911, w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where flow emerges from a confined channel and is free to spread out and infiltrate the surface. This reduces the carrying capacity of the flow and results in deposition of sediments. The flow can take the form of infrequent debris flows or one or more ephemeral or perennial streams. Alluvial fans are common in the geologic record, such as in the Triassic basins of eastern North America and the New Red Sandstone of south Devon. Such fan deposits likely contain the largest accumulations of gravel in the geologic record. Alluvial fans have also been found on Mars ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah State Route 21
State Route 21 (SR-21) is a state highway in western Utah, running for in Millard and Beaver Counties from the Nevada state line near Garrison to Beaver. Route description SR-21 begins at the Nevada state line as a continuation of Nevada State Route 487 and heads southeast through Garrison. It continues southeast past Pruess Lake and continues through Mormon Gap and Halfway Summit. It turns east around Lime Point into Corral Canyon and over Wah Wah Summit. It then heads southeast between Grampian Hill and Squaw Peak into Squaw Gulch, where it turns northeast over Frisco Summit and east through the ghost town of Frisco. It then turns southeast and continues to Milford. SR-21 leaves Milford heading southeast across an agricultural area to Minersville. In Minersville, it turns east past Yellow Mountain, then turns northeast past Minersville Lake State Park. It continues through Adamsville, then turns east around Little Bald Hill through Greenville into Beaver. In Bea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Desert Biosphere Reserve
The Desert Biosphere Reserve and Experimental Range is a biosphere reserve and experimental range in western Millard County, Utah, United States, that is listed as a historic district on the National Register of Historic Places. Description The experimental range was established in 1933 when of public lands were designated "as an agricultural range experiment station" by President Herbert Hoover. The range is maintained by the U.S. Forest Service's Rocky Mountain Research Station. It was declared a biosphere reserve by UNESCO in 1976 but was withdrawn from the program as of June 14, 2017. It is located in the northwest of Pine Valley, a valley section in southwest Millard County, about west of Milford; the north section of the reserve covers the southern half of the Tunnel Springs Mountains. It protects a landscape typical of the Great Basin, with its typical geography of north–south aligned mountain ranges separated by desert basins. Vegetation is typical of the Great Basi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wayne County, Utah
Wayne County is a county in the U.S. state of Utah. As of the 2010 census, the population was 2,778, making it the fourth-least populous county in Utah. Its county seat is Loa. History Due to its remoteness and harsh terrain, settlements did not appear in the future Wayne County until the 1880s. By 1892, there was enough settlement and enough interest in a separate county (due mainly to the difficulty of accessing the Piute County seat), that Utah Territory passed an act (effective date March 10, 1892) to separate the east portion of Piute into a separate county. The county was named for Wayne County, Tennessee, itself named for Anthony Wayne. The county boundaries have remained unchanged since its creation. Geography The eastern border of Wayne County is delineated by the meanders of the Green River, which flows southward to discharge into the Colorado River. After the two rivers join, the combined southwestern flow forms the remaining portion of the county's eastern border. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Millard County, Utah
Millard County ( ) is a county in the U.S. state of Utah. As of the 2010 United States Census, the population was 12,503. Its county seat is Fillmore, and the largest city is Delta. History The Utah Territory legislature created the county on October 4, 1851, with territory not previously covered by county creations and including some area in the future state of Nevada. It was named for the thirteenth US President Millard Fillmore, who was in office then. Fillmore was designated as the county seat. The county boundaries were altered in 1852 and again in 1854. On March 2, 1861, the US government created the Nevada Territory, which effectively de-annexed the described portion of Millard County falling in that Territorial Proclamation. The county boundary was further altered in 1862, 1866, 1888, and in 1919. In 1921 a boundary adjustment with Sevier brought Millard to its present configuration. Fillmore, located near the geographic center of the territory, was originally built a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
