Huaynaputina
Estratovolcán · Peru · 4679 m

- Tipo
- Estratovolcán
- País
- Peru
- Región
- América del Sur / Central Andean Volcanic Arc
- Altitud
- 4679 m
- Coordenadas
- -16.614, -70.854
- Última erupción
- 1600
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Composite
- Roca principal
- Dacite
Resumen geológico
Huaynaputina (whose name means "new volcano") was the source of the largest historical eruption of South America in 1600 CE. It has no prominent topographic expression and lies within a 2.5-km-wide collapse depression and further excavated by glaciers within a Tertiary to Pleistocene edifice. Three overlapping ash cones with craters up to 100 m deep were constructed during the 1600 CE eruption on the floor of the older crater, whose outer flanks are heavily mantled by ash deposits from the 1600 eruption. This powerful fissure-fed eruption may have produced nearly 30 km3 of dacitic tephra, including pyroclastic flows and surges that traveled 13 km to the E and SE. Lahars reached the Pacific Ocean, 120 km away. The eruption caused substantial damage to the major cities of Arequipa and Moquengua.
Resumen de Wikipedia
Resumen en inglésHuaynaputina 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.
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Historial de erupciones
Línea de tiempo detallada
- 1600VEI 6Observado1600-02-17 – 1600-03-06Summit and south flank
- 7750 a. C. (±200 años)VEI ?Estimación geológicaBCE 7750 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.