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タンクバン・プラフ山

Tangkuban Parahu

成層火山 · Indonesia · 2084m

The broad Tangkuban Parahu, known locally as the mountain of the "upturned boat," dominates the skyline immediately N of Indonesia's former capital city of Bandung. The volcano is truncated by the 6 x 8 km Pleistocene Sunda caldera. A series of nine overlapping craters form a 1 x 1.5 km wide elliptical depression at the summit of the post-caldera cone. Minor phreatic eruptions have occurred in historical time.
The broad Tangkuban Parahu, known locally as the mountain of the "upturned boat," dominates the skyline immediately N of Indonesia's former capital city of Bandung. The volcano is truncated by the 6 x 8 km Pleistocene Sunda caldera. A series of nine overlapping craters form a 1 x 1.5 km wide elliptical depression at the summit of the post-caldera cone. Minor phreatic eruptions have occurred in historical time. · 写真: Photo by Tom Casadevall, 1987 (U.S. Geological Survey). · Wikimedia Commons
タイプ
成層火山
国
Indonesia
地域
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
標高
2084m
座標
-6.770, 107.600
最終噴火
2019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

Gunung Tangkuban Parahu is a broad stratovolcano overlooking Indonesia's former capital city of Bandung. The volcano was constructed within the 6 x 8 km Pleistocene Sunda caldera, which formed about 190,000 years ago. The volcano's low profile is the subject of legends referring to the mountain of the "upturned boat." The Sunda caldera rim forms a prominent ridge on the western side; elsewhere the rim is largely buried by deposits of the current volcano. The dominantly small phreatic eruptions recorded since the 19th century have originated from several nested craters within an elliptical 1 x 1.5 km summit depression.

Wikipedia の要約

英語版の要約

Tangkuban Perahu is a stratovolcano in Lembang, West Bandung Regency, West Java, Indonesia. It erupted in 1826, 1829, 1842, 1846, 1896, 1910, 1926, 1929, 1952, 1957, 1961, 1965, 1967, 1969, 1983, 2013 and 2019. It is a popular tourist attraction where tourists hike or ride to the edge of the crater to view the hot water springs and boiling mud up close, and buy eggs cooked on the hot surface. Together with Mount Burangrang and Bukit Tunggul, it is a remnant of the ancient Mount Sunda after the plinian eruption caused the Caldera to collapse.

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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
8020 BCE~7685 BCE · 1件 · 最大 VEI ?7685 BCE~7351 BCE · 1件 · 最大 VEI ?1684~2019 · 20件 · 最大 VEI 28020 BCE5678 BCE3000 BCE658 BCE1684

詳細タイムライン

  1. 2019年VEI 1観測記録
    2019-07-26 ~ 2019-09-17
  2. 2013年VEI 1観測記録
    2013-02-21 ~ 2013-03-06
    Ratu Crater
  3. 2013年VEI 1観測記録
    2013-10-05 ~ 2013-10-05
    Ratu Crater
  4. 1985年VEI 1地質学的推定
    1985-11-15 ~ 1985-11-15
    Kawah Baru
  5. 1983年VEI 1観測記録
    1983-09-14 ~ 進行中
    Kawah Ratu
  6. 1969年VEI 1観測記録
    1969-07-20 ~ 1969-10-21
    Kawah Ecoma
  7. 1967年VEI 1観測記録
    1967-07-16 ~ 1967-07-16
    Kawah Ecoma
  8. 1965年VEI 1観測記録
    1965-02-16 ~ 1965-03-16
  9. 1965年VEI 1観測記録
    1965-10-16 ~ 1965-10-16
  10. 1961年VEI 1観測記録
    1961-07-16 ~ 1961-08-01
  11. 1957年VEI 1観測記録
    1957-01-16 ~ 1957-01-16
    Kawah Baru
  12. 1952年VEI 1観測記録
    1952-07-04 ~ 1952-07-11
    Kawah Ecoma
  13. 1929年VEI 0観測記録
    1929-05-20 ~ 1929-05-20
    Kawah Ecoma
  14. 1926年VEI 1観測記録
    1926-03-01 ~ 1926-07-09
    Kawah Ecoma
  15. 1910年VEI 2観測記録
    1910-04-07 ~ 1910-05
    Kawah Ratu B
  16. 1896年VEI 2観測記録
    1896-05-22 ~ 1896-05-23
    Kawah Baru
  17. 1846年VEI 2観測記録
    1846-05-27 ~ 進行中
    Kawah Ratu B
  18. 1842年VEI ?観測記録
    1842 ~ 進行中
  19. 1829年VEI 2観測記録
    1829-04-01 ~ 1829-04-04
    Kawah Ratu and Kawah Domas
  20. 1826年VEI 2観測記録
    1826-10-11 ~ 1826-10-11
  21. 紀元前 7500年 (±50年)VEI ?地質学的推定
    BCE 7500 ~ 進行中
  22. 紀元前 8020年 (±50年)VEI ?地質学的推定
    BCE 8020 ~ 進行中

外部リンク

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