Aguas Calientes caldera | |
---|---|
Highest point | |
Elevation | 4,473 m (14,675 ft)[1] |
Coordinates | 24°15′S 66°30′W / 24.250°S 66.500°W[2] |
Geography | |
Location | northwest Argentina |
Parent range | Andes |
Geology | |
Mountain type | caldera |
Volcanic belt | Andean Volcanic Belt |
Aguas Calientes is a major Miocene 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.[3]
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 350 cubic kilometres (84 cu mi). The second was erupted 17.2 Ma ago and has a volume of 140–300 cubic kilometres (34–72 cu mi).
PetrinovicMartí2010
was invoked but never defined (see the help page).