Pahrump Valley
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Pahrump Valley
Pahrump Valley is a Mojave Desert valley west of Las Vegas and the Spring Mountains massif in southern Nye County, Nevada, and eastern San Bernardino County, California. Pahrump, Nevada, is in the valley's center and the Tecopa and Chicago Valleys are immediately to the wesThe valley has routes to Death Valley and a route to Las Vegas. Pahrump Valley Dayis the annual event in February each year, along with the sanctioned JRH-HS Rodeo. History The Pahrump Valley was crossed by the Old Spanish Trail (trade route), Old Spanish Trail and later the Salt Lake Road. Geography The large block of the Spring Mountains borders Pahrump Valley on the northeast and east, with Nevada State Route 160 skirting parts of the mountain's south, and being the only due west route from Las Vegas. Route 160 turns northwest to Pahrump in the valley's center-north then meets U.S. Route 95 at the valley's north perimeter. Carpenter Canyon road starts near Pahrump and runs about 10 miles to Carpenter Canyo ...
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Nopah Range
The Nopah Range is a mountain range located in Inyo County, California, United States, near the eastern border with Nevada. Geography The mountain range lies east of the adjacent Resting Spring Range, the Owlshead Mountains and lower Death Valley, and are north of the Kingston Range. The Amargosa River is to the west. They are located directly east of Shoshone, California, and the Chicago Valley, northeast of Tecopa, California, southwest of Pahrump, Nevada, and west of Las Vegas, Nevada. The Nopah Range reaches an elevation of 6,395 feet above sea level at Nopah Peak, in the center of the range. The Nopah Range is approximately 26 miles long. Wilderness The Nopah Range Wilderness consists of 106,623 acres of the mountain range. Established in 1994 by the U.S. Congress, the wilderness area is managed by the U.S. Bureau of Land Management. Elevations range from 1,800 feet (548 m) to 6,395 feet (1949 m). The South Nopah Range Wilderness includes 17,059 acres of lower elevation fo ...
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Nevada State Route 160
State Route 160 (SR 160) is a state highway in southern Nevada, United States. It connects the southern Las Vegas Valley to U.S. Route 95 (US 95) northwest of the city via the Pahrump Valley. The southern part of the route sees heavy traffic, mostly due to Pahrump's continued growth as a Las Vegas bedroom community. The route is known as ''Blue Diamond Road'' within the Las Vegas area, with the remainder referred to as the ''Pahrump Valley Highway''. The route was originally part of State Route 16 prior to 1978. Route description State Route 160 begins in the southern Las Vegas metro area at the intersection of Las Vegas Boulevard (former SR 604) and East Windmill Lane. It runs west-southwest towards the Red Rock Canyon National Conservation Area and over Mountain Springs Summit (elevation ) before turning northwest towards Pahrump. Outside of Pahrump, SR 160 heads more north-northwest to reach its western terminus at US 95. History SR 160 was originally part of ...
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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 ...
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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 ...
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