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Perbakti-Gagak

Stratovolkan · 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.
Tipe
Stratovolkan
Negara
Indonesia
Wilayah
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Ketinggian
1726 m
Koordinat
-6.750, 106.675
Letusan terakhir
1939
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
6450 BCE~6170 BCE · 1 letusan · VEI maks. ?1659~1939 · 6 letusan · VEI maks. 16450 BCE4493 BCE2255 BCE298 BCE1659

Garis waktu rinci

  1. 1939VEI 1Teramati
    1939-04-06 – Berlangsung
    Kawah Parabakti
  2. 1938VEI 1Teramati
    1938-12 – Berlangsung
    Kawah Parabakti
  3. 1936VEI 1Teramati
    1936-10-26 – 1936-10-28
    Cipanas Parabakti
  4. 1935VEI 1Teramati
    1935-05-31 – Berlangsung
    Kawah Cibodas
  5. 1929VEI 1Teramati
    1929 – Berlangsung
    Cibeureum West
  6. 1923VEI 1Teramati
    1923-06 – Berlangsung
    Kawah Cibodas
  7. 6450 SMVEI ?Perkiraan geologi
    BCE 6450 – Berlangsung
    Kiaraberes

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.