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The geology of Chile is a characterized by … The geology of Chile is a characterized by processes linked to subduction such as volcanism, earthquakes and orogeny. The buildings blocks of Chile's geology assembled during the Paleozoic Era. Chile was by then the southwestern margin of the supercontinent Gondwana. In the Jurassic Gondwana began to split and the ongoing period of crustal deformation and mountain building known as the Andean orogeny began. In the Late Cenozoic Chile definitely separated from Antarctica, the Andes experienced a great rise accomplained by a cooling climate and the onset of glaciations. The subduction interactions shaped four main morphostructures of Chile: the Andes; the Intermediate Depression, the Coast Range, and the Peru–Chile Trench off the coast. Since Chile is on an active continental margin, it has many volcanoes. Almost the entire country is subject to earthquakes arising from strains in the Nazca and Antarctic Plates or shallow strike-slip faults. Northern Chilean mineral resources are a major economic resources, and the country is the leading producer of copper, lithium and molybdenum. Most of these mineral deposits were created from magmatic hydrothermal activity. The water required to form those deposits derived from the subducted slab of the oceanic crust beneath the Andes. The Chilean Easter Island and Juan Fernández Archipelago are volcanic hotspot islands in the eastward-moving Nazca plate. The geology of the Chilean Antarctic Territory has various commonalities with that of mainland Chile.commonalities with that of mainland Chile.
, Територія Чилі розташована в межах . Анди в країні розділяють на основний хребет Анд і прибережний хребет. Виділяють ґрабен Центральної долини. На півдні країни — та .
, La geología de Chile se caracteriza por lo … La geología de Chile se caracteriza por los efectos de la subducción que ha ocurrido en sus costas, en sentido oeste-este, desde tiempos precámbricos hasta tiempos geológicamente recientes. Tectónica y morfológicamente, Chile continental se puede subdividir en lonjas paralelas al océano Pacífico de sur a norte siendo las tres principales la cordillera de la Costa, la depresión intermedia y la cordillera de los Andes. Además de estas lonjas, en la Patagonia chilena también existen llanuras y mesetas trasandinas. Chile Insular corresponde a una serie de islas volcánicas que derivan de vulcanismo de puntos calientes y forman solamente las partes más altas de largas cadenas de volcanes extintos en la placa de Nazca. En cambio, el Territorio Chileno Antártico tiene una serie de similitudes geológicas con los Andes patagónicos. La subducción que ocurre a lo largo de la costa chilena hace que el país sea altamente sísmico y tenga una vigorosa actividad volcánica en torno a arcos continentales. La actividad volcánica y magmática en la zona norte de Chile, junto con el clima hiperárido que prevalece allí, han contribuido a formar depósitos minerales de fama mundial, incluidos pórfidos de cobre, salares y costras de caliche.os de cobre, salares y costras de caliche.
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The geology of Chile is a characterized by … The geology of Chile is a characterized by processes linked to subduction such as volcanism, earthquakes and orogeny. The buildings blocks of Chile's geology assembled during the Paleozoic Era. Chile was by then the southwestern margin of the supercontinent Gondwana. In the Jurassic Gondwana began to split and the ongoing period of crustal deformation and mountain building known as the Andean orogeny began. In the Late Cenozoic Chile definitely separated from Antarctica, the Andes experienced a great rise accomplained by a cooling climate and the onset of glaciations.ling climate and the onset of glaciations.
, La geología de Chile se caracteriza por lo … La geología de Chile se caracteriza por los efectos de la subducción que ha ocurrido en sus costas, en sentido oeste-este, desde tiempos precámbricos hasta tiempos geológicamente recientes. Tectónica y morfológicamente, Chile continental se puede subdividir en lonjas paralelas al océano Pacífico de sur a norte siendo las tres principales la cordillera de la Costa, la depresión intermedia y la cordillera de los Andes. Además de estas lonjas, en la Patagonia chilena también existen llanuras y mesetas trasandinas.én existen llanuras y mesetas trasandinas.
, Територія Чилі розташована в межах . Анди в країні розділяють на основний хребет Анд і прибережний хребет. Виділяють ґрабен Центральної долини. На півдні країни — та .
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Геологія Чилі
, Geology of Chile
, Geología de Chile
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