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Taitao granites and Taitao ophiolites would be mainly focused on in this part. Chile ridge is located west of the Taitao Peninsula, and the geology of Chile Ridge is closely associated with that of Taitao Peninsula. [1] [2] [3] Taitao ophiolite (Spanish: Ofiolita de Taitao) is an ophiolite in Taitao Peninsula of western Patagonia, Chile.
The Taitao Peninsula is situated in the Aysén del General Carlos Ibáñez del Campo Region, and part of the landmass is located inside the boundaries of Laguna San Rafael National Park. The Presidente Ríos Lake , with a surface area of 352 square kilometres (136 sq mi), lies in the center of the peninsula.
The Chile triple junction, a geologic junction off the southern coast of Chile where the South American, Nazca and Antarctic tectonic plates meet. The Chile triple junction (or Chile margin triple junction) is a geologic triple junction located on the seafloor of the Pacific Ocean off Taitao and Tres Montes Peninsula on the southern coast of Chile.
Chaicayán Group is a group of poorly defined sedimentary rock strata found in Taitao Peninsula in the west coast of Patagonia. The most common rock types are siltstone and sandstone. Conglomerate occur but is less common. [1] Study of fossils and uranium–lead dating of detrital zircons indicate a Miocene age, at least for the upper sequences.
Chile ridge is located west of the Taitao Peninsula, and the geology of Chile Ridge is closely associated with that of Taitao Peninsula. [ 5 ] [ 6 ] [ 4 ] Adakite is a felsic to intermediate rock and are usually calc-alkaline in composition.
Between 1880 and 1930, "Chile literally lived off one product: saltpetre," historian Julio Pinto told BBC News in 2015. It brought in about half of the country's fiscal revenue, he said.
The geology of Chile is a characterized by processes linked to subduction, such as volcanism, earthquakes, and orogeny. The building blocks of Chile's geology were assembled during the Paleozoic Era when Chile was the southwestern margin of the supercontinent Gondwana .
The Gulf of Penas (Golfo de Penas in Spanish, meaning "gulf of distress") is a body of water located south of the Taitao Peninsula, Chile. Geography