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Orcutt Oil Field
The Orcutt Oil Field is a large oil field in the Solomon Hills south of Orcutt, in Santa Barbara County, California. Discovered in 1901 by William Warren Orcutt, it was the first giant field (over in ultimate recovery) to be found in Santa Barbara County, and its development led to the boom town of Orcutt, now the major unincorporated southern suburb of Santa Maria. With a cumulative production in 2008 of of oil, it is the largest onshore producing field in Santa Barbara County. The Orcutt field was called the "Santa Maria Field" until the discovery of the larger Santa Maria Valley Oil Field on the plain to the north, an area which is now largely covered with the urban and suburban development. Several oil companies, including Breitburn Energy and Phoenix Energy, LLC are still actively producing from the Orcutt field. p. 94 The field, mostly located on the old Careaga family ranch, also contains the remains of the ghost town of Bicknell, a company town built for oil worker ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first epoch (geology), geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pliocene
The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58See the 2014 version of the ICS geologic time scale million years ago. It is the second and most recent epoch of the Neogene Period in the Cenozoic Era. The Pliocene follows the Epoch and is followed by the Epoch. Prior to the 2009 revision of the geologic time sca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foxen Formation
Foxen is a surname. Notable people with the surname include: *Alex Foxen William Alex Foxen (born February 1, 1991) is an American poker player from Huntington, New York. Foxen attended Boston College, where he played tight end on the school's football team. In 2012, at the age of 21, he won the first World Series o ... (born 1991), American poker player * Bill Foxen (1879–1937), American baseball pitcher * James Foxen ( 1769–1829), English hangman {{surname Patronymic surnames English-language surnames ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Careaga Formation
The Careaga family is a Californio family of Central California. History Colonel Satornino Careaga was the first of the family to immigrate to California. He was son of Sinforiano Careaga, a Spanish nobleman descended from the famous Captain Juan de Careaga (of the Vizcayan Armada) and later sent to Mexico as a military man by the King of Spain. He was a member of Captain Muñoz's command who risked his life and suffered great pains to protect an exposed and seemingly doomed San Jose Mission. He was survived by two sons, Ramon Francis Careaga and Juan B. Careaga. Along with a mutual friend, Daniel Harris, the brothers bought approximately of land formerly belonging to the De la Guerra family (early Spaniards who figured prominently in the state history). Later, in the division, Harris took some while the Careaga brothers held 10,500. This land was later split again in a settlement between Juan's only progeny and the five children of Ramon F Careaga I. It was on Ramon Careaga's land ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sisquoc Formation
The Sisquoc Formation is a sedimentary geologic unit widespread in Southern California, both on the coast and in mountains near the coast. Overlying the Monterey Formation, it is of upper Miocene and lower Pliocene age (from about 4 to 6 million years old).Isaacs, Caroline M. and Rullkötter, Jürgen. ''The Monterey Formation: From Rocks to Molecules.'' Columbia University Press, 2001. p. 211. The formation consists of claystone, mudstone, siltstone, shale, diatomite, and conglomerates, with considerable regional variation, and was deposited in a moderately deep marine environment at a depth of approximately . Since some of its diatomites, along with those of the underlying Monterey Formation, are of unusual purity and extent, they can be mined as diatomaceous earth. France-based Imerys operates a mine in the Sisquoc and Monterey Formations in the hills south of Lompoc, California, the largest such operation in the world. Type locality, description, and occurrence ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diatomite
Diatomaceous earth (), diatomite (), or kieselgur/kieselguhr is a naturally occurring, soft, siliceous sedimentary rock that can be crumbled into a fine white to off-white powder. It has a particle size ranging from more than 3 μm to less than 1 mm, but typically 10 to 200 μm. Depending on the granularity, this powder can have an abrasive feel, similar to pumice powder, and has a low density as a result of its high porosity. The typical chemical composition of oven-dried diatomaceous earth is 80–90% silica, with 2–4% alumina (attributed mostly to clay minerals), and 0.5–2% iron oxide. Diatomaceous earth consists of the fossilized remains of diatoms, a type of hard-shelled microalgae. It is used as a filtration aid, mild abrasive in products including metal polishes and toothpaste, mechanical insecticide, absorbent for liquids, matting agent for coatings, reinforcing filler in plastics and rubber, anti-block in plastic films, porous support for chemic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticline
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various rock strata are unknown, the term antiform should be used. The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guadalupe, California
Guadalupe is a small city located in Santa Barbara County, California. According to the U.S. Census of 2010, the city has a population of 7,080. Guadalupe is economically and socially tied to the city of Santa Maria, which is about 8 miles (13 km) to the east. It is located at the intersection of Highway 1 and Highway 166, immediately south of the Santa Maria River, and 5 miles (8 km) east of the Pacific Ocean.McCormack, Don (1999). ''McCormack's Guides Santa Barbara and Ventura 2000''. Mccormacks Guides. Page 53. . History The first European land exploration of Alta California, the Spanish Portolá expedition, camped near today's Guadalupe on September 1, 1769. Franciscan missionary and expedition member Juan Crespí noted in his diary that they found "a very large lake". The lake has since mostly filled in, leaving a low-lying plain traversed by the Santa Maria River and several tributaries. When Mission La Purisima was established in 1787, the area became p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Santa Maria River (California)
Santa Maria River on the Central Coast of California, is formed at the confluence of the Sisquoc River and Cuyama River, just east of the city of Santa Maria, and flows U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed March 15, 2011 to its delta at the Pacific Ocean. The entire river defines the border between northern Santa Barbara County and southern San Luis Obispo County, up to the Sisquoc River, with a major bridge on Highway 101 passing over it. The Santa Maria River Fault is a tectonic fault that roughly corresponds with the course of the river. There are no dams or lakes on the Santa Maria River itself, although Twitchell Reservoir is formed by a dam on the tributary Cuyama River. Twitchell Dam was built by the United States Bureau of Reclamation and provides flood control and groundwater recharge of the aquifer. The Sisquoc River is also free-flowing, and a National Wild and Scenic Rivers System. During much ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
