Huaynaputina
Volcano in southern Peru
Volcano in southern Peru
Huaynaputina ( WY-nə-puu-TEE-nə; Spanish: [wajnapuˈtina]) is a volcano in a volcanic high plateau in southern Peru. Lying in the Central Volcanic Zone of the Andes, it was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate. Huaynaputina is a large volcanic crater, which lacks an identifiable mountain profile, with an outer stratovolcano and three younger volcanic vents within an amphitheatre-shaped structure that is either a former caldera or a remnant of glacial erosion. The volcano has erupted dacitic magma. Huaynaputina has erupted several times during the Holocene, including on 19 February 1600 – the largest recorded eruption ever witnessed in South America – which continued with a series of events into March. Witnessed by people in the city of Arequipa, it killed perhaps 1,000–1,500 people in the region, wiped out vegetation, buried the surrounding area with 2 metres (7 ft) of volcanic rock, and damaged infrastructure and economic resources...
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