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Aguas Calientes caldera
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Aguas Calientes caldera : ウィキペディア英語版
Aguas Calientes caldera

Aguas Calientes is a major Quaternary caldera in Salta Province, Argentina. It is in the Central Volcanic Zone of the Andes, a zone of volcanism covering southern Peru, Bolivia, northwest Argentina and northern Chile. This zone contains stratovolcanoes and calderas.
The activity of the Central Volcanic Zone is linked to the subduction of the Farallon Plate and later its splinter, the Nazca Plate, below the South American Plate. The Aguas Calientes caldera is located on a Precambrian basement that was thrust over more recent (Cretaceous and younger) layers of sediment.〔
Aguas Calientes caldera was the source of two major ignimbrites; the Tajamar Ignimbrite (including the Chorrillos Ignimbrite inside the caldera) and the Verde Ignimbrite. The first was erupted 10.5–10.1 Ma ago and is a body of ignimbrite of about . The second was erupted 17.2 Ma ago and has a volume of .
== Geography and structure ==

Aguas Calientes caldera lies in the northwestern Salta Province of Argentina, in the San Antonio de los Cobres district to the southeast of the town of the same name.〔
Aguas Calientes caldera is part of the Central Volcanic Zone (CVC), which is located in southern Peru, northern Chile, southwestern Bolivia and northwestern Argentina in highlands over high. At least six potentially active calderas, 44 active major and 18 active minor volcanoes lie in this area, of which Lascar volcano is the most active. The largest eruption in historical times in the CVZ occurred in 1600 on Huaynaputina volcano in Peru.
Aguas Calientes caldera is a roughly circular caldera limited on the western and eastern side by north-south trending fault systems. Two superimposed calderas form the volcanic system.
Cerro Verde inside the caldera is a dome formed by the uplifting of the Verde ignimbrites in the caldera after their deposition and cooling. Cerro Aguas Calientes was formed in the same way from the Tajmar ignimbrites, conclusions based in both cases on the outward dip of the ignimbrites contained in the domes.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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