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Caldera del Atuel

Atuel, Caldera del

Caldera · Argentina · 5189 m

A complex of snow-covered cones (left-center) partially fills the 30 x 45 km wide Caldera del Atuel, which lies just east of the Argentina-Chile border.  The headwaters of the Río del Atuel drain to the SE through a wide breach in the caldera rim (top center) in this NASA International Space Station image (with north to the bottom left).  The snow-covered Volcán Overo and Sosneado complexes in the eastern part of the caldera contain numerous very youthful basaltic-to-andesitic pyroclastic cones and lava flows.
A complex of snow-covered cones (left-center) partially fills the 30 x 45 km wide Caldera del Atuel, which lies just east of the Argentina-Chile border. The headwaters of the Río del Atuel drain to the SE through a wide breach in the caldera rim (top center) in this NASA International Space Station image (with north to the bottom left). The snow-covered Volcán Overo and Sosneado complexes in the eastern part of the caldera contain numerous very youthful basaltic-to-andesitic pyroclastic cones and lava flows. · Foto: NASA International Space Station image ISS010-E-19060, 2005 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
Tipo
Caldera
Paese
Argentina
Regione
South America Volcanic Regions / Southern Andean Volcanic Arc
Altitudine
5189 m
Coordinate
-34.592, -69.921
Ultima eruzione
Sconosciuto
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Caldera
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

The 30 x 45 km Caldera del Atuel complex, ~30 km NW-SE and 45 km NE-SW, lies just east of the Argentina-Chile border and 18 km SSW of the rim of the Pleistocene Diamante caldera. The western rim in part follows the international border, and the headwaters of the Río del Atuel drain to the SE through a wide breach in the caldera rim. The broad floor of the caldera contains with 15 dacitic lava domes and 25 basaltic andesite to andesitic stratovolcanoes and cinder cones. A group of cones known as Las Lágrimas overlies the SW rim of the caldera, and Volcán Guanaqueros on the NE flank of the caldera is a group of young basaltic-to-andesitic cinder cones. The Volcán Overo complex in the E-central part of the caldera and the Volcán Sosneado complex in the S part of the caldera contain numerous very youthful basaltic-to-andesitic pyroclastic cones and lava flows. The Overo complex contains 20 centers, and lava flows of the Sosneado complex cover an area of 200 km2.

Sintesi da Wikipedia

Riassunto in inglese

Caldera del Atuel is a caldera in Argentina. It is the source of the Rio Atuel and has dimensions of 30 by 45 kilometres. Cerro Sosneado is a volcano located outside of the Atuel caldera, Volcan Overo and Las Lágrimas complex are located within the caldera. Holocene activity may have formed the cinder cones on the northeastern side of the caldera. After the 2010 Maule earthquake, the caldera was one of the volcanic centres that underwent subsidence, along with secondary earthquake activity.

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