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Perbakti-Gagak

성층화산 · Indonesia · 1726m

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. · 사진: Anonymous, 1989.
화산 유형
성층화산
국가
Indonesia
지역
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
해발
1726m
좌표
-6.750, 106.675
마지막 분화
1939년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

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.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
6450 BCE~6170 BCE · 1건 · 최고 VEI ?1659~1939 · 6건 · 최고 VEI 16450 BCE4493 BCE2255 BCE298 BCE1659

상세 타임라인

  1. 1939년VEI 1관측 기록
    1939-04-06 ~ 진행 중
    Kawah Parabakti
  2. 1938년VEI 1관측 기록
    1938-12 ~ 진행 중
    Kawah Parabakti
  3. 1936년VEI 1관측 기록
    1936-10-26 ~ 1936-10-28
    Cipanas Parabakti
  4. 1935년VEI 1관측 기록
    1935-05-31 ~ 진행 중
    Kawah Cibodas
  5. 1929년VEI 1관측 기록
    1929 ~ 진행 중
    Cibeureum West
  6. 1923년VEI 1관측 기록
    1923-06 ~ 진행 중
    Kawah Cibodas
  7. 기원전 6450년VEI ?지질학적 추정
    BCE 6450 ~ 진행 중
    Kiaraberes

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