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Perbakti-Gagak

Estratovolcán · Indonesia · 1726 m

The deeply eroded Gunung Perbakti (center) rises above forests to its N, flanked by Gunung Endut (left) and Gunung Salak (right) volcanoes. Perbakti and Endut are part of the Perbatkti-Gagak volcanic complex. The summit ridge of Perbakti is elongated in a NW-SE direction, and Endut volcano rises to the SW of Perbakti. Phreatic explosions have occurred during historical time at the Perbakti-Gagak complex as well as geothermal activity.
The deeply eroded Gunung Perbakti (center) rises above forests to its N, flanked by Gunung Endut (left) and Gunung Salak (right) volcanoes. Perbakti and Endut are part of the Perbatkti-Gagak volcanic complex. The summit ridge of Perbakti is elongated in a NW-SE direction, and Endut volcano rises to the SW of Perbakti. Phreatic explosions have occurred during historical time at the Perbakti-Gagak complex as well as geothermal activity. · Foto: Anonymous, 1989.
Tipo
Estratovolcán
País
Indonesia
Región
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Altitud
1726 m
Coordenadas
-6.750, 106.675
Última erupción
1939
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The Perbakti-Gagak volcanic complex, also known as Kiaraberes-Gagak, is a cluster of deeply eroded stratovolcanoes situated immediately SW of Salak volcano. The summit ridge of Gunung Perbakti is elongated in a NW-SE direction, and Gunung Endut volcano rises above a saddle to its SW. Gunung Gagak, to the NW, is capped by pumice and obsidian, with obsidian lava flows extending N and NE. Quaternary rhyolitic lava domes form a NNE-trending chain at the eastern side of the complex. Two 2-km-wide depressions on the northern and southern sides of Perbakti form the headwaters of the Kaluwung Herang and Pamatutan rivers, respectively. The complex is marked by vigorous geothermal activity. Fumaroles, mud pots, and hot springs are located on the S and SE flanks of Perbakti and at the Kiaraberes area, which includes the commercial geothermal field of Awibengkok. Mild phreatic eruptions took place during the Holocene into historical time from flank fumarolic fields.

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
6450 BCE~6170 BCE · 1 erupciones · VEI máx. ?1659~1939 · 6 erupciones · VEI máx. 16450 BCE4493 BCE2255 BCE298 BCE1659

Línea de tiempo detallada

  1. 1939VEI 1Observado
    1939-04-06 – En curso
    Kawah Parabakti
  2. 1938VEI 1Observado
    1938-12 – En curso
    Kawah Parabakti
  3. 1936VEI 1Observado
    1936-10-26 – 1936-10-28
    Cipanas Parabakti
  4. 1935VEI 1Observado
    1935-05-31 – En curso
    Kawah Cibodas
  5. 1929VEI 1Observado
    1929 – En curso
    Cibeureum West
  6. 1923VEI 1Observado
    1923-06 – En curso
    Kawah Cibodas
  7. 6450 a. C.VEI ?Estimación geológica
    BCE 6450 – En curso
    Kiaraberes

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.