Volcán Cerro Bravo

It consists of dominantly dacitic lava-domes. Características generales. In the past 4000 years, the volcano has had at least 7 violent (plinian) explosive eruptions, producing pumice layers and pyroclastic flows. In the past 4000 years, the volcano has had at least 7 violent (plinian) explosive eruptions, producing pumice layers and pyroclastic flows. It consists of dominantly dacitic lava-domes.

El volcán Azufral es un estrato-volcán, con un diámetro del cráter estimado en 3 Km, en donde se encuentra la laguna cratérica llamada Laguna Verde, no registra la presencia de glaciares, y presenta el registro de depósitos asociados con flujos de lava, flujos piroclásticos de gran magnitud y depósitos de caída (cenizas y pumitas). Cerro Bravo volcano is located 145 km NW of Bogota, Colombia, north of Nevado del Ruiz volcano. Generalidades Volcán Cerro Bravo La historia geológica del volcán Cerro Bravo probablemente comenzó hace 50.000 años, cuando se construyó un edificio antiguo, sobre el cual, en los últimos 14.000 años, se ha estado construyendo el edificio moderno.

Eruptive history. Cerro Bravo is a stratovolcano located in Tolima, Colombia, north of the Nevado del Ruiz volcano. El volcán Cerro Bravo está construido sobre rocas intrusivas terciarias de composición granodiorítica, pertenecientes al Stock de Manizales, y rocas metamorficas paleozoicas del Grupo Cajamarca, en intersección de fallas del Sistema Palestina con otras de dirección transversal. The rock type of the volcano is andesite. Cerro Bravo volcano is located 145 km NW of Bogota, Colombia, north of Nevado del Ruiz volcano.


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