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El Romeral Mine
El Romeral is an iron mine in north-central Chile. The mine benefits from being located only 22 km NNE of the city of La Serena and being next to Guayacán, a port with conditions for high-tonnage cargo ships.Millán 1999, p. 153 The mine emerged as a replacement for the nearby mine of El Tofo that was close to depletion in the early 1950s. El Romeral was Bethehem Chile Iron Mines last major investment as Compañía de Acero del Pacífico obtained the ownership of El Tofo and El Romeral in the early 1971 when they were nationalized during the Presidency of Salvador Allende. Despite being initially an expensive mine in terms of infrastructure investment and having a troublesome geology El Romeral proved with time to host more iron than initially thought. Following an ownership restructuring Compañía Minera del Pacífico, now holds control of the mine. During the 1970s El Romeral would produce enough iron to fully supply the steel mill of Huachipato.Millán 1999, p. 154 From ...
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Coquimbo Region
The Coquimbo Region ( es, Región de Coquimbo, ) is one of Chile's 16 regions (first order administrative divisions). It is bordered by Atacama to the north, Valparaíso to the south, Argentina to the east, and the Pacific Ocean to the west. It is approximately north of the national capital, Santiago. The capital and largest city is La Serena. Other important cities include the seaport Coquimbo and the agricultural centre Ovalle. Geography and ecology The Coquimbo Region forms the narrowest part, or 'waist' of Chile, and is hence one of the country's more mountainous regions, as the Andes range runs closer to the sea than elsewhere. The region has notable marine species as well as taxa that are associated with the mountainous regions. With respect to marine organisms, the upwelling areas encourage bioproductivity off of this Pacific Coast area of Chile. In the southern mountainous areas of the Coquimbo Region, the rare and endangered Chilean Wine Palm is found, whose h ...
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Presidency Of Salvador Allende
Salvador Allende was the president of Chile from 1970 until his 1973 suicide, and head of the Popular Unity government; he was a Socialist and Marxist elected to the national presidency of a liberal democracy in Latin America.Don MabryAllende's Rise and Fall''. In August 1973 the Chilean Senate declared the Allende administration to be "unlawful," Allende's presidency was ended by a military coup before the end of his term. During Allende's three years, Chile gradually transitioned into a socialist state. During his tenure, Chilean politics reached a state of civil unrest amid, political polarization, hyperinflation, lockouts, economic sanctions, CIA-sponsored interventionism and a failed coup in June 1973. Allende's coalition, Unidad Popular, faced the problem of being a minority in the congress and it was plagued by factionalism. On 11 September 1973, a successful coup led by General Augusto Pinochet overthrew the government of Allende. During the bombing of the pres ...
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University Of Chile
The University of Chile ( es, Universidad de Chile) is a public research university in Santiago, Chile. It was founded on November 19, 1842, and inaugurated on September 17, 1843.Fuentes documentales y bibliográficas para el estudio de la historia de Chile. Capítulo III: "La Universidad de Chile 1842 – 1879". 1. La ley orgánica de 1842
www.uchile.cl
It is the oldest in the country. It was established as the continuation of the former colonial Royal University of San Felipe (1738)
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Editorial Universitaria
Editorial Universitaria is Chilean university press based in Santiago. It was established in 1947 with funds from private people and from the University of Chile. During its existence, it has published the works of generations influential Chilean scientists and intellectuals. The press publishes, among other things, children's literature Children's literature or juvenile literature includes stories, books, magazines, and poems that are created for children. Modern children's literature is classified in two different ways: genre or the intended age of the reader. Children's .... References 1947 establishments in Chile University of Chile Book publishing companies of Chile Book publishing companies based in Santiago University presses of Chile Publishing companies established in 1947 {{Chile-university-stub ...
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La Liga Formation
La Liga Formation ( es, Formación La Liga) is a geologic formation Late Jurassic and Early Cretaceous age cropping out in Coquimbo Region, Chile. Rocks of the formation are andesites. Locally the rocks of the formation present epidote alteration. The iron ores of El Romeral mine El Romeral is an iron mine in north-central Chile. The mine benefits from being located only 22 km NNE of the city of La Serena and being next to Guayacán, a port with conditions for high-tonnage cargo ships.Millán 1999, p. 153 The mine emerg ... are emplaced on La Liga Formation. References {{Geology of Chile Geologic formations of Chile Lower Cretaceous Series of South America Late Jurassic South America Mesozoic Chile Geology of Coquimbo Region Jurassic volcanism Cretaceous volcanism Andesite formations ...
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Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of ...
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Atacama Fault
The Atacama Fault Zone (AFZ) is an extensive system of faults cutting across the Chilean Coastal Cordillera in Northern Chile between the Andean Mountain range and the Pacific Ocean. The fault system is North-South striking and runs for more than 1100 km North and up to 50 km in width through the Andean forearc region. The zone is a direct result of the ongoing subduction of the Eastward moving Nazca Plate beneath the South American Plate and is believed to have formed in the Early Jurassic during the beginnings of the Andean orogeny. The zone can be split into 3 regions: the North, Central and South. Tectonic history and formation The AFZ has gone through periods of inactivity and reactivation since its inception in the Cretaceous. The fault series was formed through a complex series of tectonic regimes dating back to the Early Jurassic, when the Andean back-arc basin separated from the Pacific Ocean. Intra-arc ductile deformation occurred in the Late Jurassic, crea ...
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Chañaral
Chañaral is a small coastal city and commune in the Atacama Region, Chile and capital of the Chañaral Province. It is largely unknown by tourists, who generally head straight for towns such as San Pedro de Atacama. The town has no high rise buildings. On the arid hills nearby is a lighthouse which casts a beam over the town during the night. Throughout the day and night, there is a lively atmosphere on the narrow streets. Despite it being coastal, it is not a typical seaside resort, partly because the ocean is contaminated by the copper mining industry. Situated a short distance to the north is the Pan de Azúcar National Park. History In 1824, Diego de Almeyda discovered large natural deposits of copper in the area, and was the first in the mining industry in Chile to export it. For this reason, the town was founded in October 26,1833 as ''Chañaral de las Ánimas'' (" Chañar field of the Souls"). A few years later, Pedro Lujan discovered ore at El Salado, where a mine wa ...
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Mineralium Deposita
''Mineralium Deposita, International Journal for Geology, Mineralogy and Geochemistry of Mineral Deposits '' is a peer-reviewed scientific journal published by Springer Science+Business Media. It is the official journal of the Society for Geology Applied to Mineral Deposits. The journal covers economic geology, experimental and applied geochemistry, mineral deposits research, and ore deposit exploration. The editors-in-chief are Georges Beaudoin (Université Laval) and Bernd Lehmann ( Technical University of Clausthal). According to the ''Journal Citation Reports'', the journal has a 2015 impact factor The impact factor (IF) or journal impact factor (JIF) of an academic journal is a scientometric index calculated by Clarivate that reflects the yearly mean number of citations of articles published in the last two years in a given journal, as ... of 3.467. Mineralium Deposita is a hybrid open-access journal and publishes both subscription and open access articles. Reference ...
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Chilean Iron Belt
The Chilean Iron Belt is a geological province rich in iron ore deposits in northern Chile. It extends as a north-south beld along the western part of the Chilean regions of Coquimbo and Atacama, chiefly between the cities of La Serena and Taltal. The belt follows much of the Atacama Fault System and is about 600 km long and 25 km broad. Iron oxide-apatite, iron oxide copper gold ore deposits (IOCG) and manto-type copper and silver are the main types of deposits. Iron-apatite and IOCG are considered to have different origins. Manto-type deposits are concentrated in the northern part of the belt and are chiefly emplaced on rocks of La Negra Formation. The ores of the Chilean Iron Belt formed in separate pulses in the Cretaceous period as result of magmatic and hydrothermal processes. At least part of the iron oxide-apatite rock originated from molten iron in the form of lava, tephra. and intrusions. Thus iron oxide apatite magma cooled into rock variously from surface volcano ...
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Iron Oxide-apatite
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron Age. In ...
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El Algarrobo
El Algarrobo is an iron mine in north-central Chile. Geologically it is an iron oxide-apatite (IOA) type of deposit. El Algarrobo is part of a wider province of iron ores known as the Chilean Iron Belt The Chilean Iron Belt is a geological province rich in iron ore deposits in northern Chile. It extends as a north-south beld along the western part of the Chilean regions of Coquimbo and Atacama, chiefly between the cities of La Serena and Talta .... From the 1970s onward El Romeral have come to overshadow El Algarrobo in iron ore production.Millán 1999, p. 155 References Bibliography * Iron ore mines in Chile Mines in Atacama Region Surface mines in Chile {{atacama-geo-stub ...
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