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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 Joaquin Va ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spanish Language
Spanish ( or , Castilian) is a Romance languages, Romance language of the Indo-European language family that evolved from colloquial Latin spoken on the Iberian peninsula. Today, it is a world language, global language with more than 500 million native speakers, mainly in the Americas and Spain. Spanish is the official language of List of countries where Spanish is an official language, 20 countries. It is the world's list of languages by number of native speakers, second-most spoken native language after Mandarin Chinese; the world's list of languages by total number of speakers, fourth-most spoken language overall after English language, English, Mandarin Chinese, and Hindustani language, Hindustani (Hindi-Urdu); and the world's most widely spoken Romance languages, Romance language. The largest population of native speakers is in Mexico. Spanish is part of the Iberian Romance languages, Ibero-Romance group of languages, which evolved from several dialects of Vulgar Latin in I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift Zone
A rift zone is a feature of some volcanoes, especially shield volcanoes, in which a set of linear cracks (or rifts) develops in a volcanic edifice, typically forming into two or three well-defined regions along the flanks of the vent. Believed to be primarily caused by internal and gravitational stresses generated by magma emplacement within and across various regions of the volcano, rift zones allow the intrusion of magmatic dykes into the slopes of the volcano itself. The addition of these magmatic materials usually contributes to the further rifting of the slope, in addition to generating fissure eruptions from those dykes that reach the surface. It is the grouping of these fissures, and the dykes that feed them, that serves to delineate where and whether a rift zone is to be defined. The accumulated lava of repeated eruptions from rift zones along with the endogenous growth created by magma intrusions causes these volcanoes to have an elongated shape. Perhaps the best ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Kern County, California
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San Joaquin Valley
The San Joaquin Valley ( ; es, Valle de San Joaquín) is the area of the Central Valley of the U.S. state of California that lies south of the Sacramento–San Joaquin River Delta and is drained by the San Joaquin River. It comprises seven counties of Northern and one of Southern California, including, in the north, all of San Joaquin and Kings counties, most of Stanislaus, Merced, and Fresno counties, and parts of Madera and Tulare counties, along with a majority of Kern County, in Southern California. Although the valley is predominantly rural, it has densely populated urban centers: Fresno, Bakersfield, Stockton, Modesto, Tulare, Visalia, Hanford, and Merced. The first European to enter the valley was Pedro Fages in 1772. The San Joaquin Valley was originally inhabited by the Yokuts and Miwok peoples. The Tejon Indian Tribe of California is a federally recognized tribe of Kitanemuk, Yokuts, and Chumash indigenous people of California. Their ances ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Californio
Californio (plural Californios) is a term used to designate a Hispanic Californians, Hispanic Californian, especially those descended from Spanish and Mexican settlers of the 17th through 19th centuries. California's Spanish language, Spanish-speaking community has resided there since 1683 and is made up of varying Spaniards, Spanish and Mexicans, Mexican origins, including Criollo people, criollos, Mestizos, Indigenous peoples of California, Indigenous Californian peoples, and small numbers of Mulatos. Alongside the Tejanos of Texas and Hispanos of New Mexico, Neomexicanos of New Mexico and Colorado, Californios are part of the larger Spanish-American/Mexican-American/Hispanos, Hispano community of the United States, which has inhabited the American Southwest and the U.S. West Coast, West Coast since the 16th century. Some may also identify as Chicanos, a term that came about in the 1960’s. The term ''Californio'' (historical, regional Spanish for 'Californian') was originall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Las Tinajas De Los Indios
Las Tinajas de Los Indios, or "Indian Tanks", are tinajas located in the sandstone heights of the Point of Rocks on the north side of Antelope Valley in Kern County, California.Frank F. Latta, ''El Camino Viejo á Los Angeles - The Oldest Road of the San Joaquin Valley''; Bear State Books, Exeter, 2006, pp. 10-11; Reprint of the 1936 work by Frank F. Latta, of an address he delivered before the Kern County Historical Society, February 20, 1933, and published by it as its second annual publication, in 1936. History ''Las Tinajas de Los Indios'' (The Jars of the Indians), later called "Indian Tanks", was as its name suggests, the site of an Indian encampment. The tops of the Point of Rocks, sandstone rock formations, have ''tinajas'', (''jars'' in Spanish), natural basins that acted as reservoirs or cisterns to hold the water that collected during the winter rains and held it throughout the summer. These tinajas bear evidence of having been improved by the Indians. Deeply worn st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aguaje Del Diablo
Devilwater Creek, originally Arroyo Del Diablo, a stream with its source on the east slope of the Temblor Range in Kern County, California, that flows northeast to terminate just a mile west southwest of the mouth of Media Aqua Creek. It was officially named Devilwater Creek in 1909. History Aguaje Del Diablo (Devil's Watering Place) was an aguaje or watering place on 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 Cali ... along the Arroyo del Diablo in the foothills on the east slope of the Temblor Range between Arroyo de Los Carneros in the south and Arroyo de Matarano to the north. References Rivers of Kern County, California Temblor Range El Camino Viejo {{KernCountyCA-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 cont ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Point Of Rocks (Kern County, California)
Point of Rocks is a mountain range in Kern County, California. Its sandstone peaks were a landmark for travelers crossing the Antelope Valley on El Camino Viejo and a guide to the water to be found on their heights, at Las Tinajas de Los Indios. Nearby to the southeast is the location of the Point of Rocks oilfield A petroleum reservoir or oil and gas reservoir is a subsurface accumulation of hydrocarbons contained in porous or fractured rock formations. Such reservoirs form when kerogen (ancient plant matter) is created in surrounding rock by the presence .... The deepest oil well drilled in California was here in 1987. Its total depth: 24426 feet. References Mountain ranges of Kern County, California Mountain ranges of Southern California {{KernCountyCA-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temblor Range
The Temblor Range is a mountain range within the California Coast Ranges, at the southwestern extremity of the San Joaquin Valley in California in the United States. It runs in a northwest-southeasterly direction along the borders of Kern County and San Luis Obispo County. The name of the range is from Spanish ''temblor'' meaning "tremor", referring to earthquakes. The San Andreas Fault Zone runs parallel to the range at the base of its western slope, on the eastern side of the Carrizo Plain, while the Antelope Plain, location of the enormous Midway Sunset, South Belridge, and Cymric oil fields, lies to the northeast. Peaks within the Temblor Range average about above sea level. The highest point is McKittrick Summit at , located in the center of the range about west of Bakersfield. The summit on State Route 58, which crosses the range, is at above sea level. The lowest crossing of the range is at Polonio Pass at by State Route 46 at its northern end and is separate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San Andreas Fault
The San Andreas Fault is a continental transform fault that extends roughly through California. It forms the tectonic boundary between the Pacific Plate and the North American Plate, and its motion is right-lateral strike-slip (horizontal). The fault divides into three segments, each with different characteristics and a different degree of earthquake risk. The slip rate along the fault ranges from /yr. It was formed by a transform boundary. The fault was identified in 1895 by Professor Andrew Lawson of UC Berkeley, who discovered the northern zone. It is often described as having been named after San Andreas Lake, a small body of water that was formed in a valley between the two plates. However, according to some of his reports from 1895 and 1908, Lawson actually named it after the surrounding San Andreas Valley. Following the 1906 San Francisco earthquake, Lawson concluded that the fault extended all the way into southern California. In 1953, geologist Thomas Dibblee co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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