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Gunung Tangkuban Perahu

Tangkuban Parahu

Stratovolkan · Indonesia · 2084 m

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. · Foto: Photo by Tom Casadevall, 1987 (U.S. Geological Survey). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Indonesia
Wilayah
Sunda & Banda / Sunda Volcanic Arc
Ketinggian
2084 m
Koordinat
-6.770, 107.600
Letusan terakhir
2019
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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8020 BCE~7685 BCE · 1 letusan · VEI maks. ?7685 BCE~7351 BCE · 1 letusan · VEI maks. ?1684~2019 · 20 letusan · VEI maks. 28020 BCE5678 BCE3000 BCE658 BCE1684

Garis waktu rinci

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

Tautan eksternal

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