Lewati ke konten utama

Indonesia · Stratovolkan

Perbakti-Gagak

Tipe
Stratovolkan
Ketinggian
1726 m
Letusan terakhir
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.
Tipe
Stratovolkan
Negara
Indonesia
Wilayah
Sunda & Banda / Sunda Volcanic Arc
Ketinggian
1726 m
Koordinat
-6.750, 106.675
Letusan terakhir
1939
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Andesit / Andesit basaltik
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

7 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu · Gunakan tombol panah untuk berpindah batang, Enter untuk membuka
6450 SM~6170 SM · 1 letusan · VEI maks. ?1659~1939 · 6 letusan · VEI maks. 16450 SM4493 SM2255 SM298 SM1659

Garis waktu rinci

  1. 1939VEI 1Teramati
    1939-04-06 – akhir tidak diketahui
    Kawah Parabakti
  2. 1938VEI 1Teramati
    1938-12-16 – akhir tidak diketahui
    Kawah Parabakti
  3. 1936VEI 1Teramati
    1936-10-26 – 1936-10-28
    Cipanas Parabakti
  4. 1935VEI 1Teramati
    1935-05-31 – akhir tidak diketahui
    Kawah Cibodas
  5. 1929VEI 1Teramati
    1929-07-02 – akhir tidak diketahui
    Cibeureum West
  6. 1923VEI 1Teramati
    1923-06-16 – akhir tidak diketahui
    Kawah Cibodas
  7. 6450 SMVEI ?Perkiraan geologi
    6450 SM – akhir tidak diketahui
    Kiaraberes

Gunung api terdekat

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.