Nevado del Huila
Huila, Nevado del
Estratovolcán · Colombia · 5364 m
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- Tipo
- Estratovolcán
- País
- Colombia
- Región
- South America Volcanic Regions / Northern Andean Volcanic Arc
- Altitud
- 5364 m
- Coordenadas
- 2.930, -76.030
- Última erupción
- 2012
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Composite
- Roca principal
- Andesite / Basaltic Andesite
Resumen geológico
Nevado del Huila, the highest peak in the Colombian Andes, is an elongated N-S-trending volcanic chain mantled by a glacier icecap. The andesitic-dacitic volcano was constructed within a 10-km-wide caldera. Volcanism at Nevado del Huila has produced six volcanic cones whose ages in general migrated from south to north. The high point of the complex is Pico Central. Two glacier-free lava domes lie at the southern end of the volcanic complex. The first historical activity was an explosive eruption in the mid-16th century. Long-term, persistent steam columns had risen from Pico Central prior to the next eruption in 2007, when explosive activity was accompanied by damaging mudflows.
Resumen de Wikipedia
Resumen en inglésNevado del Huila at 5,364 metres (17,598 ft) is the highest volcano in Colombia, located at the tripoint of the departments of Huila, Tolima and Cauca. It is visible from the city of Cali. The andesitic volcano is located on top of the Ibagué Batholith.
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Historial de erupciones
Línea de tiempo detallada
- 2008VEI 2Observado2008-01-02 – 2008-04-16
- 2008VEI 3Observado2008-10-26 – 2012-01-14Upper SW side of Pico Central
- 2007VEI 3Observado2007-02-19 – 2007-05-28
- 1555 (±5 años)VEI ?Observado1555 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.