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Gunung Taal

Taal

Kaldera · Philippines · 311 m

Taal caldera, seen here from its NW rim, is a 15 x 20 km caldera of Pleistocene and Holocene age. Volcano Island, in the north-central part of Lake Taal, is constructed of coalescing small tuff and scoria cones. Powerful phreatomagmatic explosive eruptions from several locations on the 5-km-wide island have produced deadly pyroclastic surges.
Taal caldera, seen here from its NW rim, is a 15 x 20 km caldera of Pleistocene and Holocene age. Volcano Island, in the north-central part of Lake Taal, is constructed of coalescing small tuff and scoria cones. Powerful phreatomagmatic explosive eruptions from several locations on the 5-km-wide island have produced deadly pyroclastic surges. · Foto: Photo by Chris Newhall, 1978 (U.S. Geological Survey). · Wikimedia Commons
Tipe
Kaldera
Negara
Philippines
Wilayah
Pasifik Barat / Luzon Volcanic Arc
Ketinggian
311 m
Koordinat
14.011, 120.998
Letusan terakhir
2026
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Caldera
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

Taal is one of the most active volcanoes in the Philippines and has produced some powerful eruptions. The 15 x 20 km Talisay (Taal) caldera is largely filled by Lake Taal, whose 267 km2 surface lies only 3 m above sea level. The maximum depth of the lake is 160 m, with several submerged eruptive centers. The 5-km-wide Volcano Island in north-central Lake Taal is the location of all observed eruptions. The island is composed of coalescing small stratovolcanoes, tuff rings, and scoria cones. Powerful pyroclastic flows and surges have caused many fatalities.

Ringkasan Wikipedia

Ringkasan Inggris

Taal Volcano, also known as Taal Caldera, is a large caldera filled by Taal Lake in the Philippines. Located in the province of Batangas about 50 kilometers (31 mi) south of Manila, the volcano is the second most active volcano in the country, with 39 recorded historical eruptions, all concentrated on Volcano Island, near the middle of Taal Lake. The caldera was formed by prehistoric eruptions between less than 670,000 and less than 6,000 years ago. The cones Batulao, Macolod, and Sungay are remnants of the early pre-caldera Taal system, with Batulao being the earliest known cone.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
3580 BCE~3387 BCE · 1 letusan · VEI maks. 61444~1638 · 5 letusan · VEI maks. 31638~1831 · 13 letusan · VEI maks. 41831~2024 · 21 letusan · VEI maks. 43580 BCE2227 BCE875 BCE4781831

Garis waktu rinci

  1. 2024VEI 2Teramati
    2024-04-12 – 2026-03-16
  2. 2022VEI 1Teramati
    2022-10-05 – 2022-10-29
  3. 2021VEI 1Teramati
    2021-07-01 – 2021-07-09
  4. 2021VEI 2Teramati
    2021-11-15 – 2022-04-01
    Main Crater
  5. 2020VEI 4Teramati
    2020-01-12 – 2020-01-22
  6. 1977VEI 2Teramati
    1977-10-03 – 1977-11-12
    SW flank (near Mt. Tabaro)
  7. 1976VEI 2Teramati
    1976-09-03 – 1976-10-17
    SW flank (near Mt. Tabaro)
  8. 1970VEI 1Teramati
    1970-11-09 – 1970-11-13
    SW flank (near Mt. Tabaro)
  9. 1969VEI 2Teramati
    1969-10-29 – 1969-12-10
    SW flank (near Mt. Tabaro)
  10. 1968VEI 2Teramati
    1968-01-31 – 1968-04-02
    SW flank (near Mt. Tabaro)
  11. 1967VEI 1Teramati
    1967-08-16 – 1967-08-19
    SW flank (near Mt. Tabaro)
  12. 1966VEI 3Teramati
    1966-07-05 – 1966-08-04
    SW flank (near Mt. Tabaro)
  13. 1965VEI 4Teramati
    1965-09-28 – 1965-09-30
    SW flank (near Mt. Tabaro)
  14. 1911VEI 3Teramati
    1911-01-27 – 1911-02-08
  15. 1904VEI 1Teramati
    1904-04-16 – 1904-07-15
    Base of south wall of main crater
  16. 1903VEI 2Teramati
    1903-04-16 – Berlangsung
  17. 1885VEI ?Perkiraan geologi
    1885-07-02 – Berlangsung
  18. 1878VEI 2Teramati
    1878-11-12 – 1878-11-15
  19. 1874VEI 2Teramati
    1874-07-19 – Berlangsung
  20. 1873VEI 2Teramati
    1873-07-02 – Berlangsung
  21. 1842VEI 2Teramati
    1842-07-02 – Berlangsung
  22. 1825VEI 2Teramati
    1825-07-02 – Berlangsung
  23. 1808VEI 2Teramati
    1808-02-16 – 1808-04-16
  24. 1790VEI 2Teramati
    1790 – Berlangsung
  25. 1754VEI 4Teramati
    1754-05-15 – 1754-12-04
    Summit crater and SE flank
  26. 1749VEI 4Teramati
    1749-08-11 – 1749-09
  27. 1731VEI 2Teramati
    1731 – Berlangsung
    Pira-piraso (NE flank)
  28. 1729VEI 2Teramati
    1729 – Berlangsung
    Binintiang Munti
  29. 1716VEI 4Teramati
    1716-09-24 – 1716-09-27
    Calauit (sublacustral SE flank)
  30. 1715VEI 2Teramati
    1715 – Berlangsung
    Binintiang Malaki
  31. 1709VEI 2Teramati
    1709 – Berlangsung
    Binintiang Munti
  32. 1707VEI 2Teramati
    1707 – Berlangsung
    Binintiang Malaki
  33. 1645VEI 3Teramati
    1645 – Berlangsung
  34. 1641VEI 3Teramati
    1641 – Berlangsung
  35. 1635VEI 3Teramati
    1635 – Berlangsung
  36. 1634VEI 3Teramati
    1634 – Berlangsung
  37. 1608 (±3 tahun)VEI 2Teramati
    1608 – Berlangsung
  38. 1591VEI 3Teramati
    1591 – Berlangsung
  39. 1572VEI 3Teramati
    1572 – Berlangsung
  40. 3580 SM (±200 tahun)VEI 6Perkiraan geologi
    BCE 3580 – Berlangsung

Tautan eksternal

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