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Little Smoky Valley
Little Smoky Valley is one of the Central Nevada Desert Basins and an eponym for the larger Little Smoky-Newark Watershed. The valley spans three counties in Nevada, namely Eureka, Nye, and White Pine. The valley's numerous springs include Cool Tank, Mahogany, Moody, Little Nevada, Pogue Wells, and Soda Springs. Places in the valley include the Warm Springs, Nevada Warm Springs is a former town in the Tonopah Basin in Nye County, Nevada, near the mountain pass which divides the Kawich Range, Kawich and Hot Creek Range, Hot Creek ranges (at ). It is located at the junction of U.S. Route 6 in Nevada, U.S. Rou ..., community and the Little Smoky Valley Use Area for grazing. Little Smoky Valley was so named on account of frequently foggy conditions. References Valleys of Nevada Valleys of Eureka County, Nevada Valleys of Nye County, Nevada Valleys of White Pine County, Nevada {{WhitePineCountyNV-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Basin Desert
The Great Basin Desert is part of the Great Basin between the Sierra Nevada and the Wasatch Range. The desert is a geographical region that largely overlaps the Great Basin shrub steppe defined by the World Wildlife Fund, and the Central Basin and Range ecoregion defined by the U.S. Environmental Protection Agency and United States Geological Survey. It is a temperate desert with hot, dry summers and snowy winters. The desert spans large portions of Nevada and Utah, and extends into eastern California. The desert is one of the four biologically defined deserts in North America, in addition to the Mojave, Sonoran, and Chihuahuan Deserts. Basin and range topography characterizes the desert: wide valleys bordered by parallel mountain ranges generally oriented north–south. There are more than 33 peaks within the desert with summits higher than , but valleys in the region are also high, most with elevations above . The biological communities of the Great Basin Desert vary accordi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eponym
An eponym is a person, a place, or a thing after whom or which someone or something is, or is believed to be, named. The adjectives which are derived from the word eponym include ''eponymous'' and ''eponymic''. Usage of the word The term ''eponym'' functions in multiple related ways, all based on an explicit relationship between two named things. A person, place, or thing named after a particular person share an eponymous relationship. In this way, Elizabeth I of England is the eponym of the Elizabethan era. When Henry Ford is referred to as "the ''eponymous'' founder of the Ford Motor Company", his surname "Ford" serves as the eponym. The term also refers to the title character of a fictional work (such as Rocky Balboa of the Rocky film series, ''Rocky'' film series), as well as to ''self-titled'' works named after their creators (such as the album The Doors (album), ''The Doors'' by the band the Doors). Walt Disney created the eponymous The Walt Disney Company, Walt Disney Com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eureka County, Nevada
Eureka County is a county in the U.S. state of Nevada. As of the 2020 census, the population was 1,855, making it the second-least populous county in Nevada. Its county seat is Eureka. Eureka County is part of the Elko Micropolitan Statistical Area. History Eureka County was established in 1873 and formed from Lander County after silver was discovered more than east of Austin. The new mining camp's residents complained Austin was too far to go for county business and a new county was created. It was named for the ancient Greek term, ''Eureka'', meaning, "I have found it." This term was used earlier in California and other locations. Eureka has always been the county seat. Geography According to the U.S. Census Bureau, the county has an area of , of which is land and (0.1%) is water. The county's highest point is the 10,631 ft (3240 m) summit of Diamond Peak in the Diamond Mountains along the border with White Pine County. Adjacent counties *Elko County - northe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nye County, Nevada
Nye County is a county in the U.S. state of Nevada. As of the 2020 census, the population was 51,591. Its county seat is Tonopah. At , Nye is Nevada's largest county by area and the third-largest county in the contiguous United States, behind Coconino County of Arizona and San Bernardino County of California. Nye County comprises the Pahrump Micropolitan Statistical Area, which is included in the Las Vegas-Henderson Combined Statistical Area. In 2010, Nevada's center of population was in southern Nye County, near Yucca Mountain. The Nevada Test Site and proposed Yucca Mountain nuclear waste repository are in southwestern Nye County, and are the focus of a great deal of controversy. The federal government manages 92% of the county's land. A 1987 attempt to stop the nuclear waste site resulted in the creation of Bullfrog County, Nevada, which was dissolved two years later. The county has several environmentally sensitive areas, including Ash Meadows National Wildlife Refu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White Pine County, Nevada
White Pine County is a largely rural, mountain county along the central eastern boundary of the U.S. state of Nevada. As of the 2010 census, the population was 10,030. Its county seat is Ely. The name "(Rocky Mountain) white pine" is an old name for the limber pine (''Pinus flexilis''), a common tree in the county's mountains. The county boasts dark skies, clean air and millions of acres of unspoiled public land. It is the home of Great Basin National Park, one of America's most remote and least visited national parks. It is also home to no less than 14 federally designated wilderness areas, offering an abundance of terrain available to explore for hikers, backpackers, skiers, hunters and anglers. The Ely Shoshone Indian Reservation is located in the county, on the south side of the City of Ely. The reservation has a land area of 104.99 acres (0.4249 km2) and a 2000 census official resident population of 133 people. History European settlement in White Pine County be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warm Springs, Nevada
Warm Springs is a former town in the Tonopah Basin in Nye County, Nevada, near the mountain pass which divides the Kawich Range, Kawich and Hot Creek Range, Hot Creek ranges (at ). It is located at the junction of U.S. Route 6 in Nevada, U.S. Route 6 and Nevada State Route 375, State Route 375 (the "Extraterrestrial Highway"), around 50 miles east of Tonopah, Nevada, Tonopah. Only two abandoned buildings remain. History The first white settlement in Warm Springs was in 1866, when it served as a stopover for stagecoaches and other travellers. The post office was in operation from January 1924 through June 1929. In 1947, the springs was purchased by the Fallini brothers and it was reported that Thomas Hurt had been operating the springs for several years. Never more than a tiny settlement, Warm Springs' population dwindled until it became a ghost town. All that remained was a single streetlight, a telephone box, and several huts built over pools filled by the warm springs that give ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Nevada
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] |
Valleys Of Eureka County, Nevada
A valley is an elongated low area often running between hills or 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 glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these 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 areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Nye County, Nevada
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] |
