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탕쿠반 프라후산

Tangkuban Parahu

성층화산 · 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. · 사진: Photo by Tom Casadevall, 1987 (U.S. Geological Survey). · Wikimedia Commons
화산 유형
성층화산
국가
Indonesia
지역
순다·반다 / Sunda Volcanic Arc
해발
2084m
좌표
-6.770, 107.600
마지막 분화
2019년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

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 요약

영어 요약

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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분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
8020 BCE~7685 BCE · 1건 · 최고 VEI ?7685 BCE~7351 BCE · 1건 · 최고 VEI ?1684~2019 · 20건 · 최고 VEI 28020 BCE5678 BCE3000 BCE658 BCE1684

상세 타임라인

  1. 2019년VEI 1관측 기록
    2019-07-26 ~ 2019-09-17
  2. 2013년VEI 1관측 기록
    2013-02-21 ~ 2013-03-06
    Ratu Crater
  3. 2013년VEI 1관측 기록
    2013-10-05 ~ 2013-10-05
    Ratu Crater
  4. 1985년VEI 1지질학적 추정
    1985-11-15 ~ 1985-11-15
    Kawah Baru
  5. 1983년VEI 1관측 기록
    1983-09-14 ~ 진행 중
    Kawah Ratu
  6. 1969년VEI 1관측 기록
    1969-07-20 ~ 1969-10-21
    Kawah Ecoma
  7. 1967년VEI 1관측 기록
    1967-07-16 ~ 1967-07-16
    Kawah Ecoma
  8. 1965년VEI 1관측 기록
    1965-02-16 ~ 1965-03-16
  9. 1965년VEI 1관측 기록
    1965-10-16 ~ 1965-10-16
  10. 1961년VEI 1관측 기록
    1961-07-16 ~ 1961-08-01
  11. 1957년VEI 1관측 기록
    1957-01-16 ~ 1957-01-16
    Kawah Baru
  12. 1952년VEI 1관측 기록
    1952-07-04 ~ 1952-07-11
    Kawah Ecoma
  13. 1929년VEI 0관측 기록
    1929-05-20 ~ 1929-05-20
    Kawah Ecoma
  14. 1926년VEI 1관측 기록
    1926-03-01 ~ 1926-07-09
    Kawah Ecoma
  15. 1910년VEI 2관측 기록
    1910-04-07 ~ 1910-05-16
    Kawah Ratu B
  16. 1896년VEI 2관측 기록
    1896-05-22 ~ 1896-05-23
    Kawah Baru
  17. 1846년VEI 2관측 기록
    1846-05-27 ~ 진행 중
    Kawah Ratu B
  18. 1842년VEI ?관측 기록
    1842-07-02 ~ 진행 중
  19. 1829년VEI 2관측 기록
    1829-04-01 ~ 1829-04-04
    Kawah Ratu and Kawah Domas
  20. 1826년VEI 2관측 기록
    1826-10-11 ~ 1826-10-11
  21. 기원전 7500년 (±50년)VEI ?지질학적 추정
    BCE 7500 ~ 진행 중
  22. 기원전 8020년 (±50년)VEI ?지질학적 추정
    BCE 8020 ~ 진행 중

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