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Perbakti-Gagak

成層火山 · 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. · 写真: Anonymous, 1989.
タイプ
成層火山
Indonesia
地域
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
標高
1726m
座標
-6.750, 106.675
最終噴火
1939年
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Andesite / Basaltic Andesite
地質学的概要

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.

噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
6450 BCE~6170 BCE · 1件 · 最大 VEI ?1659~1939 · 6件 · 最大 VEI 16450 BCE4493 BCE2255 BCE298 BCE1659

詳細タイムライン

  1. 1939年VEI 1観測記録
    1939-04-06 ~ 進行中
    Kawah Parabakti
  2. 1938年VEI 1観測記録
    1938-12 ~ 進行中
    Kawah Parabakti
  3. 1936年VEI 1観測記録
    1936-10-26 ~ 1936-10-28
    Cipanas Parabakti
  4. 1935年VEI 1観測記録
    1935-05-31 ~ 進行中
    Kawah Cibodas
  5. 1929年VEI 1観測記録
    1929 ~ 進行中
    Cibeureum West
  6. 1923年VEI 1観測記録
    1923-06 ~ 進行中
    Kawah Cibodas
  7. 紀元前 6450年VEI ?地質学的推定
    BCE 6450 ~ 進行中
    Kiaraberes

外部リンク

⚠ 参考情報です。緊急対応には使用しないでください。