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Cerro Bravo

Bravo, Cerro

Stratovulcano · Colombia · 3985 m

Cerro Bravo is seen from the east. The summit dome was extruded during the most recent eruption and has a spine (a steep dome) near the top. An older lava dome and cone complex is situated to the left. Multiple collapse events sent block-and-ash flows down over lava flows (center) and onto the Plan de Arriba (lower left). The low tree-covered slope (left foreground) is the remnant of the pre-Cerro Bravo edifice that was destroyed by a Pleistocene caldera-forming event.
Cerro Bravo is seen from the east. The summit dome was extruded during the most recent eruption and has a spine (a steep dome) near the top. An older lava dome and cone complex is situated to the left. Multiple collapse events sent block-and-ash flows down over lava flows (center) and onto the Plan de Arriba (lower left). The low tree-covered slope (left foreground) is the remnant of the pre-Cerro Bravo edifice that was destroyed by a Pleistocene caldera-forming event. · Foto: Photo by David Lescinsky, 1988 (University of Western Ontario). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Colombia
Regione
South America Volcanic Regions / Northern Andean Volcanic Arc
Altitudine
3985 m
Coordinate
5.091, -75.293
Ultima eruzione
1720
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Dacite
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
4280 BCE~4080 BCE · 1 eruzioni · VEI max. 41480 BCE~1280 BCE · 1 eruzioni · VEI max. 41080 BCE~880 BCE · 1 eruzioni · VEI max. 4880 BCE~680 BCE · 1 eruzioni · VEI max. 4720~920 · 1 eruzioni · VEI max. 4920~1120 · 1 eruzioni · VEI max. 41320~1520 · 1 eruzioni · VEI max. 41520~1720 · 1 eruzioni · VEI max. 44280 BCE2880 BCE1280 BCE1201520

Cronologia dettagliata

  1. 1720 (±150 anni)VEI 4Stima geologica
    1720 – In corso
  2. 1330 (±75 anni)VEI 4Stima geologica
    1330 – In corso
  3. 1050 (±75 anni)VEI 4Stima geologica
    1050 – In corso
  4. 750 (±150 anni)VEI 4Stima geologica
    750 – In corso
  5. 730 a.C. (±75 anni)VEI 4Stima geologica
    BCE 730 – In corso
  6. 1050 a.C. (±200 anni)VEI 4Stima geologica
    BCE 1050 – In corso
  7. 1310 a.C. (±150 anni)VEI 4Stima geologica
    BCE 1310 – In corso
  8. 4280 a.C. (±150 anni)VEI 4Stima geologica
    BCE 4280 – In corso

Link esterni

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