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Quilotoa

Caldera · Ecuador · 3914 m

Quilotoa is a truncated, forested dacitic cone containing a steep-walled, 3-km-wide caldera filled by a 250-m-deep lake.  Lava domes form the caldera's perimeter and occupy its floor.  Its most recent large eruption about 800 years ago produced voluminous pyroclastic flows, lahars that reached the Pacific Ocean, and one of the largest airfall-tephra deposits of the northern Andes.  Reports of historical eruptions from the caldera lake are somewhat ambiguous.  Fumaroles are present on the lake floor and hot springs occur on the eastern flank.
Quilotoa is a truncated, forested dacitic cone containing a steep-walled, 3-km-wide caldera filled by a 250-m-deep lake. Lava domes form the caldera's perimeter and occupy its floor. Its most recent large eruption about 800 years ago produced voluminous pyroclastic flows, lahars that reached the Pacific Ocean, and one of the largest airfall-tephra deposits of the northern Andes. Reports of historical eruptions from the caldera lake are somewhat ambiguous. Fumaroles are present on the lake floor and hot springs occur on the eastern flank. · Foto: Photo by Minard Hall, 1973 (Escuela Politécnica Nacional, Quito). · Wikimedia Commons
Tipo
Caldera
País
Ecuador
Región
South America Volcanic Regions / Northern Andean Volcanic Arc
Altitud
3914 m
Coordenadas
-0.859, -78.904
Última erupción
1280
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Caldera
Roca principal
Dacite
Resumen geológico

Quilotoa is a truncated, dacitic cone in the Western Cordillera of Ecuador, 35 km WNW of the city of Latacunga, that contains a 3-km-wide caldera with steep-sided walls that rise 400 m above the surface of 240-m-deep caldera lake. Multiple lava domes are present along the caldera's perimeter. This small volcano has produced eight major explosive eruptions during the past 200,000 years. Its most recent major eruption about 800 radiocarbon years ago produced voluminous pyroclastic flows, lahars that reached the Pacific Ocean, and one of the largest airfall-tephra deposits of the northern Andes. Formation of the caldera was followed by extrusion of a small lava dome. Reports of observed eruptions from the caldera lake are somewhat ambiguous. Fumaroles are present on the lake floor and hot springs occur on the E flank.

Resumen de Wikipedia

El Quilotoa es un volcán lleno de agua en su cráter de 3 kilómetros (2 mi) de diámetro en su borde que se formó por el colapso de este volcán de dacita seguido por una erupción de VEI-6 hace aproximadamente 800 años, lo que produjo un flujo piroclástico y lahares que alcanzaron el Océano Pacífico, que lanzó cenizas volcánicas a todo lo largo de los Andes septentrionales.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1280~1332 · 1 erupciones · VEI máx. 61694~1745 · 2 erupciones · VEI máx. 21745~1797 · 2 erupciones · VEI máx. 212801383153916421745

Línea de tiempo detallada

  1. 1797VEI ?Estimación geológica
    1797-02-04 – En curso
  2. 1759VEI 2Estimación geológica
    1759 – En curso
  3. 1740VEI 2Estimación geológica
    1740-12 – En curso
  4. 1725VEI 2Estimación geológica
    1725 – En curso
  5. 1280VEI 6Estimación geológica
    1280 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.