Hamlin Valley
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Hamlin Valley
Hamlin Valley is a mostly north-south trending valley of the Great Basin located on both sides of the Nevada–Utah state line. It is about long. Its north-northeast end point adjacent the state line, is the southwest start region of the Snake Valley (Great Basin). Description Hamlin Valley lies between the Mountain Home Range on the east and Indian Peak Range on the southeast and south, and the Needle Mountains, White Rock Mountains, and Limestone Hills on the west. On the north, it merges with Snake Valley, about south of Garrison; the south of the Snake Range north-northwest, causes the north valley to narrow and change to northeasterly, as the valley merges into Snake Valley. The north end of the valley is located at , and the south end at . Rosencrans Well is located just southwest of the valley's center. The Hamlin Valley Wash is an ephemeral stream running through the valley, flowing north-northwest, then due north. It originates in the foothills north of Modena, Utah, ...
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Mountain Home Range
The Mountain Home Range is a north-south trending mountain range in western Beaver County in southwest Utah, United States. It is part of the Basin and Range Province. It is bound by Hamlin Valley to the west, Snake Valley (part of this area known as Antelope Valley on some maps) to the north, Pine Valley to the east, and trends into the Indian Peak Range to the south. Collectively, the Mountain Home Range and Indian Peak Range are known as the Needle Mountains due to their jagged nature. The highest peak in the range, known simply as the 'Needle benchmark,' is tall. The range is very uncommonly used by humans, and is more known for wildlife and wild horses. Geology The northern part of the range is made of Paleozoic carbonate rocks which are part of a long structural trend of rocks that go through the Burbank Hills, Conger Range, and Confusion Range. This is highlighted by a massive (30 by 50 mile) syncline. The southern part of the range is made of mid-Tertiary ignimbrite ...
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Endorheic Basin
An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes or swamps, permanent or seasonal, that equilibrate through evaporation. They are also called closed or terminal basins, internal drainage systems, or simply basins. Endorheic regions contrast with exorheic regions. Endorheic water bodies include some of the largest lakes in the world, such as the Caspian Sea, the world's largest inland body of water. Basins with subsurface outflows which eventually lead to the ocean are generally not considered endorheic; they are cryptorheic. Endorheic basins constitute local base levels, defining a limit of erosion and deposition processes of nearby areas. Etymology The term was borrowed from French ''endor(rh)éisme'', coined from the combining form ''endo-'' (from grc, ἔνδον ''éndon'' 'wit ...
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Valleys Of Iron County, Utah
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 ...
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Valleys Of Beaver County, Utah
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 ...
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Valleys Of White Pine 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 ...
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Valleys Of Lincoln 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 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 ...
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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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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 ...
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List Of Valleys Of Nevada
This is a list of valleys of Nevada. Valleys are ordered alphabetically, by county. Dramatic parallelism is shown in the landforms of central and eastern Nevada. The most common valley name is Antelope Valley which is used for 5 different areas in Douglas, Elko/White Pine, Eureka, Lander, and Washoe Counties. Churchill County * Carson Sink * Copper Valley (Churchill-Pershing Counties) * Dixie Valley (Churchill-Pershing Counties) * Edwards Creek Valley * Fairview Valley * Granite Springs Valley (Churchill-Pershing Counties) * Lahontan Valley * North Valley * Stingaree Valley * Wyemaha Valley Clark County * Bitter Spring Valley * Cottonwood Valley * Cottonwood Valley (Mojave Co., Arizona/Clark Co., Nevada) * Dry Lake Valley * Eldorado Valley * Goodsprings Valley * Green Valley * Hidden Valley * Indian Springs Valley (Nevada) (Clark-Lincoln Counties) * Ivanpah Valley * Las Vegas Valley * Mercury Valley * ''Moapa Valley'' * Pahrump Valley (Clark-Nye Counties) * Paradise Vall ...
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Nuclear Weapons Testing
Nuclear weapons tests are experiments carried out to determine nuclear weapons' effectiveness, Nuclear weapon yield, yield, and explosive capability. Testing nuclear weapons offers practical information about how the weapons function, how detonations are affected by different conditions, and how personnel, structures, and equipment are affected when subjected to Nuclear explosion, nuclear explosions. However, nuclear testing has often been used as an indicator of scientific and military strength. Many tests have been overtly political in their intention; most List of countries with nuclear weapons, nuclear weapons states publicly declared their nuclear status through a nuclear test. The first nuclear device was detonated as a test by the United States at the Trinity site in New Mexico on July 16, 1945, with a yield approximately TNT equivalent, equivalent to 20 kilotons of TNT. The first thermonuclear weapon technology test of an engineered device, codenamed "Ivy Mike", was teste ...
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