San Emigdio Creek
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San Emigdio Creek
San Emigdio Creek, formerly Arroyo de San Emigdio (Spanish for Saint Emygdius Creek), is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed September 7, 2011 northward-flowing stream in western Kern County, central California. Geography The San Emigdio Creek headwaters are on the northeast slope of Mount Pinos, south of Tecuya Ridge in the San Emigdio Mountains. The creek flows north through San Emigdio Canyon to terminate southwest of Lakeview in the western San Joaquin Valley. In years of heavy rainfall it would be a tributary to the Connecting Slough, the slough between Kern Lake and Buena Vista Lake which has been dry for decades due to agricultural diversion, pumping, and a lowering groundwater table. History Arroyo San Emigdio was a stream whose canyon provided the route followed by the 18th-19th century ''El Camino Viejo'', through the San Emigdio Mountains between the Cuddy Valley and San Joaquin Valley. ...
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Spanish Language
Spanish ( or , Castilian) is a Romance language of the Indo-European language family that evolved from colloquial Latin spoken on the Iberian peninsula. Today, it is a global language with more than 500 million native speakers, mainly in the Americas and Spain. Spanish is the official language of 20 countries. It is the world's second-most spoken native language after Mandarin Chinese; the world's fourth-most spoken language overall after English, Mandarin Chinese, and Hindustani (Hindi-Urdu); and the world's most widely spoken Romance language. The largest population of native speakers is in Mexico. Spanish is part of the Ibero-Romance group of languages, which evolved from several dialects of Vulgar Latin in Iberia after the collapse of the Western Roman Empire in the 5th century. The oldest Latin texts with traces of Spanish come from mid-northern Iberia in the 9th century, and the first systematic written use of the language happened in Toledo, a prominent c ...
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Slough (hydrology)
A slough ( or ) is a wetland, usually a swamp or shallow lake, often a backwater to a larger body of water. Water tends to be stagnant or may flow slowly on a seasonal basis. In North America, "slough" may refer to a side-channel from or feeding a river, or an inlet or natural channel only sporadically filled with water. An example of this is Finn Slough on the Fraser River, whose lower reaches have dozens of notable sloughs. Some sloughs, like Elkhorn Slough, used to be mouths of rivers, but have become stagnant because tectonic activity cut off the river's source. In the Sacramento River, Steamboat Slough was an alternate branch of the river, a preferred shortcut route for steamboats passing between Sacramento and San Francisco. Georgiana Slough was a steamboat route through the Sacramento–San Joaquin River Delta, from the Sacramento River to the San Joaquin River and Stockton. Plants and animals A slough, also called a tidal channel, is a channel in a wetland. Typic ...
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Mission Santa Barbara
Mission Santa Barbara ( es, link=no, Misión de Santa Bárbara) is a Spanish mission in Santa Barbara, California. Often referred to as the ‘Queen of the Missions,’ it was founded by Padre Fermín Lasuén for the Franciscan order on December 4, 1786, the feast day of Saint Barbara, as the tenth mission of what would later become 21 missions in Alta California. Mission Santa Barbara, like other California missions, was built as part of a broader effort to consolidate the Spanish claim on Alta California in the face of threats from rival empires. In attempting to do this, Spain sought to turn local indigenous tribes into good Spanish citizens (for Mission Santa Barbara, this was the Chumash- Barbareño tribe). This required religious conversion and integration into the Spanish colonial economy – for the local Chumash people, the environmental changes wrought by the Mission's large herd of livestock, combined with epidemics and military force, meant that tribal members oft ...
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Alta California
Alta California ('Upper California'), also known as ('New California') among other names, was a province of New Spain, formally established in 1804. Along with the Baja California peninsula, it had previously comprised the province of , but was split off into a separate province in 1804 (named ). Following the Mexican War of Independence, it became a territory of Mexico in April 1822 and was renamed in 1824. The territory included all of the modern U.S. states of California, Nevada, and Utah, and parts of Arizona, Wyoming, Colorado, and New Mexico. In the 1836 Siete Leyes government reorganization, the two Californias were once again combined (as a single ). That change was undone in 1846, but rendered moot by the U.S. military occupation of California in the Mexican-American War. Neither Spain nor Mexico ever colonized the area beyond the southern and central coastal areas of present-day California and small areas of present-day Arizona, so they exerted no effective contro ...
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Rancho San Emidio
Rancho San Emidio was a Mexican land grant in present-day Kern County, California given in 1842 by Governor Juan Alvarado to José Antonio Dominguez. The grant was located along San Emigdio Creek in the northeastern foothills of the San Emigdio Mountains, between Santiago Creek on the west and Pleitito Creek on the east. There is speculation on the name. Either it is an alternative spelling of San Emigdio ( Saint Emygdius the protector Saint against earthquakes), or an intentional corruption, meant as a witticism since "emidio" means tired or weary. The rancho was established at a way stop at the foot of San Emigdio Canyon on ''El Camino Viejo'' ('the old road,' 18th-19th century) that ran along the eastern edge of the San Joaquin Valley from Pueblo de Los Angeles to the Mission Santa Clara de Asís and later on to Rancho San Antonio, on San Francisco Bay. History José Antonio Dominguez (1796–1844), was a soldier at the Presidio of Santa Barbara. In 1819 Dominguez m ...
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Ranchos Of California
The Spanish and Mexican governments made many concessions and land grants in Alta California (now known as California) and Baja California from 1775 to 1846. The Spanish Concessions of land were made to retired soldiers as an inducement for them to remain in the frontier. These Concessions reverted to the Spanish crown upon the death of the recipient. The Mexican government later encouraged settlement by issuing much larger land grants to both native-born and naturalized Mexican citizens. The grants were usually two or more square leagues, or in size. Unlike Spanish Concessions, Mexican land grants provided permanent, unencumbered ownership rights. Most ranchos granted by Mexico were located along the California coast around San Francisco Bay, inland along the Sacramento River, and within the San Joaquin Valley. When the government secularized the Mission churches in 1833, they required that land be set aside for each Neophyte family. But the Native Americans were quickl ...
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Bitterwater Creek
Bitterwater Creek, originally named Arroyo de Matarano ("Matarano Creek" in Spanish), is a stream in eastern San Luis Obispo County and northwestern Kern County, central California. Geography The creek's source located at the confluence of Walnut Creek and Yeguas Creek in San Luis Obispo County, west of the Temblor Range and east of the Carrizo Plain in the San Andreas Fault rift zone. It flows northwest in the rift zone, then northeast through the Temblor Range and passing south of the Shale Hills, into Antelope Valley 4 miles southeast of Point of Rocks. History Arroyo de Matarano was a water stop on the 19th century El Camino Viejo in Alta California, between the stops of Aguaje Del Diablo to the south and Las Tinajas de Los Indios to the north, and east of Point of Rocks. This stream was named for Juan Matarano, a well known mid 19th century Mexican '' Californio'' ''mesteñero'' or "mustang runner" of the west side of the southern San Joaquin Valley The San Joaq ...
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Cuddy Valley
Cuddy Valley is a valley in the San Andreas Rift Zone south of the San Emigdio Mountains west of Tejon Pass, part of the Mountain Communities. It lies at an elevation of 5,282 feet 1610 m). History What is now the Cuddy Valley was a water and grazing place along El Camino Viejo (18th-19th century). The Old Road came over what is now the Tejon Pass from what would become Gorman then turned west up Cuddy Creek to Cuddy Valley its spring. Afterward the road descended to the north, through the San Emigdio Mountains, via San Emigdio Canyon along San Emigdio Creek to the San Joaquin Valley. At the foot of the mountains at the creek's mouth was the next stop, that became the 1842 Mexican land grant of '' Rancho San Emidio''. John Fletcher Cuddy Cuddy Valley, Cuddy Creek and Cuddy Canyon are named for John Fletcher Cuddy, who came to the United States from Ireland during the Great Famine. He joined the U. S. Army and after being discharged in 1853, followed his former unit, the ...
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El Camino Viejo
El Camino Viejo a Los Ángeles ( en, the Old Road to Los Angeles), also known as El Camino Viejo and the Old Los Angeles Trail, was the oldest north-south trail in the interior of Spanish colonial Las Californias (1769–1822) and Mexican Alta California (1822–1848), present day California. It became a well established inland route, and an alternative to the coastal El Camino Real trail used since the 1770s in the period. It ran from San Pedro Bay and the Pueblo de Los Ángeles, over the Transverse Ranges through Tejon Pass and down through the San Emigdio Mountains to the San Joaquin Valley, where it followed a route along the eastern slopes of the Coast Ranges between '' aguaje'' (watering places) and '' arroyos''. It passed west out of the valley, over the Diablo Range at Corral Hollow Pass into the Livermore Valley, to end at the Oakland Estuary on the eastern San Francisco Bay. History The route of El Camino Viejo was well established by the 1820s, and the route was in ...
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Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ...
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Aquifer
An aquifer is an underground layer of water-bearing, permeable rock, rock fractures, or unconsolidated materials ( gravel, sand, or silt). Groundwater from aquifers can be extracted using a water well. Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), which is a solid, impermeable area underlying or overlying an aquifer, the pressure of which could create a confined aquifer. The classification of aquifers is as follows: Saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; transboundary aquifer. Challenges for using groundwater include: overdrafting (extracting groundwater beyond the equilibrium yield of the aquifer), groundwater-related subsidence of land, groundwater becoming ...
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Buena Vista Lake
Buena Vista Lake was a fresh-water lake in Kern County, California, in the Tulare Lake Basin in the southern San Joaquin Valley, California. Buena Vista Lake was the second largest of several similar lakes in the Tulare Lake basin, and was fed by the waters of the Kern River. The Kern River's flow went into Buena Vista Lake southwest through the site of Bakersfield via its main distributary channels or south through the Kern River Slough distributary into Kern Lake and then into Buena Vista Lake via Connecting Slough. In times when Buena Vista Lake overflowed it first backed up into Kern Lake making one large lake. When this larger lake overflowed it flowed out through the Buena Vista Slough and Kern River channel northwest of Buena Vista Lake through tule marshland and Goose Lake, into Tulare Lake. Today Lake Webb and Lake Evans occupy the lakebed on the northern shore of the former Buena Vista Lake. Tulamniu Indian Site On Buena Vista Lake south shores was the s ...
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