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Indonesia · Stratovulcano

Perbakti-Gagak

Tipo
Stratovulcano
Altitudine
1726 m
Ultima eruzione
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
Stratovulcano
Paese
Indonesia
Regione
Sunda e Banda / Sunda Volcanic Arc
Altitudine
1726 m
Coordinate
-6.750, 106.675
Ultima eruzione
1939
Contesto tettonico
Zona di subduzione / Crosta continentale (> 25 km)
Forma vulcanica
Composito
Roccia principale
Andesite / Andesite basaltica
Sintesi geologica

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.

Storia delle eruzioni

7 registrateGlossario
Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni · Usa le frecce per spostarti tra le barre, Invio per aprire
6450 a.C.~6170 a.C. · 1 eruzioni · VEI max. ?1659~1939 · 6 eruzioni · VEI max. 16450 a.C.4493 a.C.2255 a.C.298 a.C.1659

Cronologia dettagliata

  1. 1939VEI 1Osservata
    1939-04-06 – fine sconosciuta
    Kawah Parabakti
  2. 1938VEI 1Osservata
    1938-12-16 – fine sconosciuta
    Kawah Parabakti
  3. 1936VEI 1Osservata
    1936-10-26 – 1936-10-28
    Cipanas Parabakti
  4. 1935VEI 1Osservata
    1935-05-31 – fine sconosciuta
    Kawah Cibodas
  5. 1929VEI 1Osservata
    1929-07-02 – fine sconosciuta
    Cibeureum West
  6. 1923VEI 1Osservata
    1923-06-16 – fine sconosciuta
    Kawah Cibodas
  7. 6450 a.C.VEI ?Stima geologica
    6450 a.C. – fine sconosciuta
    Kiaraberes

Vulcani nelle vicinanze

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