Ragged Valley
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Ragged Valley
Ragged Valley is a valley in the Diablo Range of Fresno County, California, named for the ragged appearance of its surface. It is bound on the east by the Big Blue Hills and on the west by Joaquin Ridge, extending northwesterly from its large mouth at Domengine Creek to the divide between Salt Creek and Cantua Creek where it heads A head is the part of an organism which usually includes the ears, brain, forehead, cheeks, chin, eyes, nose, and mouth, each of which aid in various sensory functions such as sight, hearing, smell, and taste. Some very simple animals may no ... at . References {{coord, 36, 19, 42, N, 120, 21, 55, W, display=title Valleys of Fresno County, California Diablo Range ...
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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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Diablo Range
The Diablo Range is a mountain range in the California Coast Ranges subdivision of the Pacific Coast Ranges in northern California, United States. It stretches from the eastern San Francisco Bay area at its northern end to the Salinas Valley area at its southern end. Geography The Diablo Range extends from the Carquinez Strait in the north to Orchard Peak and Polonio Pass in the south, near the point where State Route 46 crosses over the Coast Ranges at Cholame, as described by the United States Geological Survey (USGS). It is bordered on the northeast by the San Joaquin River, on the southeast by the San Joaquin Valley, on the southwest by the Salinas River, and on the northwest by the Santa Clara Valley. The USGS designation is somewhat ambiguous north of the Santa Clara Valley, but on USGS maps, the range is shown as the ridgeline which runs between its namesake Mount Diablo southeastward past Mount Hamilton. Geologically, the range corresponds to the California Coast R ...
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Fresno County, California
Fresno County (), officially the County of Fresno, is a county located in the central portion of the U.S. state of California. As of the 2020 Census, the population was 1,008,654. The county seat is Fresno, the fifth-most populous city in California. Fresno County comprises the Fresno, CA Metropolitan Statistical Area, which is part of the Fresno- Madera, CA Combined Statistical Area. It is located in the Central Valley, south of Stockton and north of Bakersfield. Since 2010, statewide droughts in California have further strained both Fresno County's and the entire Central Valley's water security. History The area now known as Fresno County was the traditional homeland of Yokuts and Mono peoples, and was later settled by Spaniards during a search for suitable mission sites. In 1846, this area became part of the United States as a result of the Mexican War. Fresno County was formed in 1856 from parts of Mariposa, Merced and Tulare counties. ''Fresno'' is Spanish for "ash ...
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Big Blue Hills
The Big Blue Hills are a low mountain range in west Fresno County, in the western San Joaquin Valley of central California. Interstate 5 runs parallel to the hills on the east. Geography The Big Blue Hills are in the Southern Inner California Coast Ranges System, adjacent to the Diablo Range on the west. Their highest point is in elevation. Cantua Creek and its Arroyo de Cantúa canyon divides them from the Ciervo Hills The Ciervo Hills are a low mountain range in west Fresno County, in the western San Joaquin Valley of central California. Interstate 5 runs parallel to the hills on the east. Geography The Ciervo Hills are in the Southern Inner California Coast .... References Mountain ranges of Fresno County, California California Coast Ranges Diablo Range Geography of the San Joaquin Valley Mountain ranges of Northern California {{FresnoCountyCA-geo-stub ...
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Joaquin Ridge
Joaquin Ridge is a ridge in the Diablo Range in Fresno County, California. The ridge is named for Joaquin Murietta (1830-1853), a California Gold Rush bandit, leader of the Five Joaquins Gang, who used this region as a rendezvous and camp that overlooked the gangs base at the Rancho de Cantua. The ridge is ten miles long, running from its high point at , east of Spanish Lake, eastward to Joaquin Rocks , and then southwestward to near 3,629-foot Black Mountain at the high point on the south southeast trending Anticline Ridge. Joaquin Ridge is bound on the northeast by the Ragged Valley and the Big Blue Hills and on the southwest by Portuguese Canyon. Its highest elevation is , east of Spanish Lake. The most distinguishing feature of Joaquin Ridge is Joaquin Rocks, originally known as "Las Tres Piedras" (The Three Rocks). These three pillars of rock on the ridge are clearly visible on the ridge for many miles from many directions in the San Joaquin Valley and from their ...
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Salt Creek (Fresno County)
Salt Creek may refer to: Streams *Salt Creek (Amargosa River tributary), California *Salt Creek (Orange County), California * Salt Creek (Sacramento River tributary), California *Salt Creek (Salton Sea), California *Salt Creek (Des Plaines River tributary), Illinois * Salt Creek (Little Wabash River tributary), Illinois *Salt Creek (Sangamon River tributary), Illinois * Salt Creek (Little Calumet River tributary), Indiana * Salt Creek (White River tributary), Indiana * Salt Creek (Osage River), Missouri *Salt Creek (Platte River), Nebraska *Salt Creek (Muskingum County, Ohio), a stream located entirely within Muskingum County, Ohio *Salt Creek (Middle Fork Willamette River tributary), Oregon * Salt Creek (Juab County), Utah Settlements *Salt Creek, Colorado * Salt Creek, Oregon *Salt Creek, South Australia *Salt Creek, Panama, a village on Bastimentos Island, Panama Other * ''Salt Creek'' (2015), a novel by Australian author Lucy Treloar * Salt Creek Bay, on which Edithburgh is l ...
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Cantua Creek (Fresno Slough Tributary)
Cantua Creek, formerly in Spanish Arroyo de Cantúa, was named for José de Guadalupe Cantúa, a prominent Californio Ranchero in the 19th-century Mexican era of Alta California. The creek was formerly a tributary of the Fresno Slough, in years of very heavy winter rains. Course Its source is on the northern slope of Santa Rita Peak in the Diablo Range, 5.9 miles southeast of Idria within San Benito County. It flows north then east into Fresno County, emerging from its ''Arroyo de Cantúa'' canyon, that divides the Big Blue Hills from the Ciervo Hills, into the western San Joaquin Valley. Continuing toward the Fresno Slough to the northeast, but no longer reaching it, Cantua Creek ends shortly after passing under Interstate 5, 4 miles south of the census-designated place of Cantua Creek and just west of the California Aqueduct. History The ''Arroyo de Cantúa'' was first explored by a detachment of troops under José de Guadalupe Cantúa (1786–1860) who served in the ...
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Head Of The Valley
The head of the valley or, less commonly, the valley head, refers to the uppermost part of a valley.Leser (2005), p. 935. Description The head of a valley may take widely differing forms; for example, in highland regions the valley often ends in a broad, evenly sloping hollow. The higher the head of the valley, the more likely it is to resemble the geomorphological shape of a cirque. In glacial valleys or trough valleys, it may be referred to as the trough head or trough end.Leser (2005), p. 978. In mountains with predominantly crystalline rock the heads of the valleys are generally very wet, sometimes boggy and often support lush alpine meadows, whilst those made of limestone are usually dry and covered in talus or gravel. Where there has been ice age glaciation, the valley bottoms are modified by moraines and mountain lakes are common. See also * Structural basin * U-shaped or trough valley * Landform * Valley step A valley step (german: Talstufe or ''Talschwelle'') i ...
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Valleys Of Fresno County, California
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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