Tippett Canyon
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Tippett Canyon
Tippett Canyon, is a valley whose creek drains the northwest watershed of the South Mountains in White Pine County, Nevada. Its mouth is at an elevation of . Its source Source may refer to: Research * Historical document * Historical source * Source (intelligence) or sub source, typically a confidential provider of non open-source intelligence * Source (journalism), a person, publication, publishing institute o ... is at the head of the canyon near Cedar Pass, at an elevation of at . References Valleys of Nevada Valleys of White Pine County, Nevada {{WhitePineCountyNV-geo-stub ...
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Valley
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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South Mountains (Nevada/Utah)
South Mountains are a range of mountains primarily in White Pine County, Nevada and partially to the east in Juab County, Utah. The range is sometimes referred to as the Deep Creek Mountains, or the Ibenpah Mountains. The South Mountains are divided from the Kern Mountains to the south by Tippett Canyon on the west and Pleasant Valley to the east. They are divided from the Deep Creek Range to the east in Utah by Johnson Canyon, on the north, and by Water Canyon on the south. The range is bounded on the north by Spring Creek Flat and on the west by Antelope Valley The Antelope Valley is located in northern Los Angeles County, California, and the southeast portion of Kern County, California, and constitutes the western tip of the Mojave Desert. It is situated between the Tehachapi, Sierra Pelona, and the .... The highest elevation of the range is an unnamed peak with an elevation of at in Nevada.
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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 ...
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Mouth
In animal anatomy, the mouth, also known as the oral cavity, or in Latin cavum oris, is the opening through which many animals take in food and issue vocal sounds. It is also the cavity lying at the upper end of the alimentary canal, bounded on the outside by the lips and inside by the pharynx. In tetrapods, it contains the tongue and, except for some like birds, teeth. This cavity is also known as the buccal cavity, from the Latin ''bucca'' ("cheek"). Some animal phyla, including arthropods, molluscs and chordates, have a complete digestive system, with a mouth at one end and an anus at the other. Which end forms first in ontogeny is a criterion used to classify bilaterian animals into protostomes and deuterostomes. Development In the first multicellular animals, there was probably no mouth or gut and food particles were engulfed by the cells on the exterior surface by a process known as endocytosis. The particles became enclosed in vacuoles into which enzymes were secr ...
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River Source
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest ...
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Cedar Pass
Cedar Pass is a gap between Tippett Canyon and Pleasant Valley in White Pine County, Nevada. These valleys divide the South Mountains from the Kern Mountains The Kern Mountains are a mountain range primarily on the eastern edge of White Pine County, Nevada, United States, but extending slightly east into western Juab County, Utah. Description The range lies between the Antelope Valley on the northwest .... It is lies at an altitude of . References Landforms of White Pine County, Nevada {{WhitePineCountyNV-geo-stub ...
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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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