Brava

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 14.85°N
  • 24.72°W

  • 900 m
    2952 ft

  • 384020
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Brava.



 Available Weekly Reports

There are no Weekly Reports available for Brava.

There are no Holocene eruptions known for Brava. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Heleno S I N, Fonseca J F B D, 1999. A seismological investigation of the Fogo volcano, Cape Verde Islands: preliminary results. Volc Seism, 20: 199-217 (English translation).

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Mitchell-Thome R C, 1976. Geology of the Middle Atlantic Islands. Berlin: Gebruder Borntraeger, 382 p.

Wolff J A, Turbeville B N, 1985. Recent pyroclastic deposits on Brava, Cape Verde Islands (abs). Eos, Trans Amer Geophys Union, 66: 1152.

Brava Island, 20 km west of Fogo, is the westernmost of the southern Cape Verde islands. The 10-km-wide island contains 15 morphologically youthful craters located along two or three lineaments intersecting along the crest of the island. The youthfulness of the craters and numerous minor earthquakes in recent years indicate that a significant volcanic hazard still exists (Wolff and Turbeville, 1985). Most of the younger eruptions originated from the interaction of phonolitic magmas with a large groundwater reservoir contained within an older volcanic series characterized by thick welded ignimbrites and block-and-ash flow deposits. Carbonatitic lavas are also found on Brava.