Colombia · Stratovolcano
Cerro Bravo
Bravo, Cerro
- Type
- Stratovolcano
- Elevation
- 3985m
- Last eruption
- 1720

- Type
- Stratovolcano
- Country
- Colombia
- Region
- South America / Northern Andean Volcanic Arc
- Elevation
- 3985m
- Coordinates
- 5.091, -75.293
- Last eruption
- 1720
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Dacite
Geological summary
Cerro Bravo is a relatively low dominantly dacitic lava-dome complex north of Nevado del Ruiz that was constructed within the Pleistocene Quebrada Seca caldera. A series of moderate plinian eruptions during the Holocene were accompanied by pyroclastic flows and lava dome growth. Although historical records of the roughly 4000-m-high Cerro Bravo eruptions have not been found, stratigraphic evidence indicates that it last erupted sometime between the 1595 and 1845 eruptions of Ruiz.
From Wikipedia
Cerro Bravo is a stratovolcano located in Tolima, Colombia, north of the Nevado del Ruiz volcano. The rock type of the volcano is andesite.
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Eruption history
8 recordedGlossaryDetailed timeline
- 1720 (±150 yrs)VEI 4Geological estimate1720 – end unknown
- 1330 (±75 yrs)VEI 4Geological estimate1330 – end unknown
- 1050 (±75 yrs)VEI 4Geological estimate1050 – end unknown
- 750 (±150 yrs)VEI 4Geological estimate750 – end unknown
- 730 BCE (±75 yrs)VEI 4Geological estimate730 BCE – end unknown
- 1050 BCE (±200 yrs)VEI 4Geological estimate1050 BCE – end unknown
- 1310 BCE (±150 yrs)VEI 4Geological estimate1310 BCE – end unknown
- 4280 BCE (±150 yrs)VEI 4Geological estimate4280 BCE – end unknown
Nearby volcanoes
External links
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