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Volcano Attractions In Province of Catamarca

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Catamarca is a province of Argentina, located in the northwest of the country. The province had a population of 334,568 as per the 2001 census [INDEC], and covers an area of 102,602 km2. Its literacy rate is 95.5%. Neighboring provinces are : Salta, Tucumán, Santiago del Estero, Córdoba, and La Rioja. To the west it borders the country of Chile. The capital is San Fernando del Valle de Catamarca, usually shortened to Catamarca. Other important cities include Andalgalá, Tinogasta, and Belén.
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Volcano Attractions In Province of Catamarca

  • 1. Galan Volcano Antofagasta De La Sierra
    Cerro Galán is a caldera in the Catamarca Province of Argentina. It is one of the largest exposed calderas in the world. It is part of the Central Volcanic Zone of the Andes, one out of several volcanic belts found in South America. It is one of several major caldera systems in the Central Volcanic Zone, some of which are grouped into the Altiplano–Puna volcanic complex. Volcanic activity at Galán is the indirect consequence of the subduction of the Nazca Plate beneath the South America Plate, and involves the infiltration of melts into the crust and the formation of secondary magmas which after storage in the crust give rise to the dacitic to rhyodacitic rocks erupted by the volcano. Galán was active between 5.6 and 4.51 million years ago, when it generated a number of ignimbrites kn...
    From Wikipedia, the free encyclopedia.
  • 2. Volcan Antofagasta Antofagasta De La Sierra
    Socompa is a large stratovolcano at the border of Argentina and Chile. Part of the Chilean and Argentine Andean Volcanic Belt , it is part of the Central Volcanic Zone, one of the various segments of the AVB. This part of the Andean volcanic arc begins in Peru and runs first through Bolivia and Chile, and then through Argentina and Chile, and contains about 44 active volcanoes. Socompa lies close to the pass of the same name, where the Salta-Antofagasta railway crosses the border. Socompa is known for its large debris avalanche, which was formed 7,200 years ago when most of the northwestern slope collapsed and slid down, forming an extensive deposit. It was at first considered to be either a moraine or a nuee ardende deposit, until the 1980 eruption of Mount St. Helens prompted awareness o...
    From Wikipedia, the free encyclopedia.

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