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Indonesia · Estratovolcán

Perbakti-Gagak

Tipo
Estratovolcán
Altitud
1726 m
Última erupción
1939
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 y Banda / Sunda Volcanic Arc
Altitud
1726 m
Coordenadas
-6.750, 106.675
Última erupción
1939
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Compuesto
Roca principal
Andesita / Andesita basáltica
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

7 registradasGlosario
Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales · Usa las flechas para moverte entre barras y Enter para abrir
6450 a. C.~6170 a. C. · 1 erupciones · VEI máx. ?1659~1939 · 6 erupciones · VEI máx. 16450 a. C.4493 a. C.2255 a. C.298 a. C.1659

Línea de tiempo detallada

  1. 1939VEI 1Observado
    1939-04-06 – fin desconocido
    Kawah Parabakti
  2. 1938VEI 1Observado
    1938-12-16 – fin desconocido
    Kawah Parabakti
  3. 1936VEI 1Observado
    1936-10-26 – 1936-10-28
    Cipanas Parabakti
  4. 1935VEI 1Observado
    1935-05-31 – fin desconocido
    Kawah Cibodas
  5. 1929VEI 1Observado
    1929-07-02 – fin desconocido
    Cibeureum West
  6. 1923VEI 1Observado
    1923-06-16 – fin desconocido
    Kawah Cibodas
  7. 6450 a. C.VEI ?Estimación geológica
    6450 a. C. – fin desconocido
    Kiaraberes

Volcanes cercanos

Enlaces externos

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