Altiplano–Puna volcanic complex | Wikipedia audio article
Channel: wikipedia tts
Date: 2019-02-08

This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Altiplano%E2%80%93Puna_volcanic_complex


00:01:24 1 Geography
00:03:06 2 Geology
00:06:49 3 Scientific investigation
00:07:31 4 Geologic history
00:10:34 5 Extent
00:12:59 6 Source of magmas
00:16:09 7 Tomographic studies
00:18:04 8 Subsystems
00:21:45 9 Ignimbrites



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SUMMARY
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The Altiplano–Puna volcanic complex (Spanish: Complejo volcánico Altiplano-Puna), also known as APVC, is a complex of volcanic systems in the Puna of the Andes. It is located in the Altiplano area, a highland bounded by the Bolivian Cordillera Real in the east and by the main chain of the Andes, the Western Cordillera, in the west. It results from the subduction of the Nazca Plate beneath the South American Plate. Melts caused by subduction have generated the volcanoes of the Andean Volcanic Belt including the APVC. The volcanic province is located between 21° S–24° S latitude. The APVC spans the countries of Argentina, Bolivia and Chile.In the Miocene–Pliocene (10-1 mya), calderas erupted felsic ignimbrites in four distinct pulses separated by periods of low levels of activity. At least three volcanic centres (Guacha caldera, La Pacana, Pastos Grandes, Vilama) had eruptions of a Volcanic Exposivity Index (VEI) of 8, as well as smaller scale eruptive centres. Activity waned after 2 mya, but present-day geothermal activity and volcanoes dated to the Holocene, as well as recent ground deformation at Uturunku volcano indicate still-extant present-day activity of the system.