nevado del cumbal
Cumbal
Estratovolcán · Colombia · 4764 m

- Tipo
- Estratovolcán
- País
- Colombia
- Región
- América del Sur / Northern Andean Volcanic Arc
- Altitud
- 4764 m
- Coordenadas
- 0.950, -77.870
- Última erupción
- 1926
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Composite
- Roca principal
- Andesite / Basaltic Andesite
Resumen geológico
Many youthful lava flows extend from the glacier-capped Cumbal volcano, the southernmost historically active volcano of Colombia. The volcano is elongated in a NE-SW direction and is composed primarily of andesitic-dacitic lava flows. Two fumarolically active craters occupy the summit ridge: the main crater on the NE side and Mundo Nuevo crater on the SW. A young lava dome occupies the 250-m-wide summit crater, and eruptions from the upper E flank produced a 6-km-long lava field. The oldest crater lies NNE of the summit crater, suggesting SW-ward migration of activity. Explosive eruptions in 1877 and 1926 are the only known historical activity. Thermal springs are located on the SE flanks.
Resumen de Wikipedia
Resumen en inglésCumbal is a stratovolcano of the Caribe Terrane, located at the Nudo de los Pastos in Nariño, Colombia. It is the southernmost historically active volcano of Colombia and is together with Chiles and Azufral one of the few volcanoes of the Western Ranges. The volcano is dominated by andesites.
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Historial de erupciones
Línea de tiempo detallada
- 1926VEI 2Observado1926-12-20 – 1926-12-21
- 1877VEI 2Observado1877-12-16 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.