Philippines · Caldera
Volcano Island
Taal
- Type
- Caldera
- Elevation
- 311m
- Last eruption
- 2026

- Type
- Caldera
- Country
- Philippines
- Region
- Western Pacific / Luzon Volcanic Arc
- Elevation
- 311m
- Coordinates
- 14.011, 120.998
- Last eruption
- 2026
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Andesite / Basaltic andesite
Geological summary
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.
From Wikipedia
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 confirmed historical eruptions, 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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Eruption history
40 recordedGlossaryDetailed timeline
- 2024VEI 2Observed2024-04-12 – 2026-03-16
- 2022VEI 1Observed2022-10-05 – 2022-10-29
- 2021VEI 1Observed2021-07-01 – 2021-07-09
- 2021VEI 2Observed2021-11-15 – 2022-04-01Main Crater
- 2020VEI 4Observed2020-01-12 – 2020-01-22
- 1977VEI 2Observed1977-10-03 – 1977-11-12SW flank (near Mt. Tabaro)
- 1976VEI 2Observed1976-09-03 – 1976-10-17SW flank (near Mt. Tabaro)
- 1970VEI 1Observed1970-11-09 – 1970-11-13SW flank (near Mt. Tabaro)
- 1969VEI 2Observed1969-10-29 – 1969-12-10SW flank (near Mt. Tabaro)
- 1968VEI 2Observed1968-01-31 – 1968-04-02SW flank (near Mt. Tabaro)
- 1967VEI 1Observed1967-08-16 – 1967-08-19SW flank (near Mt. Tabaro)
- 1966VEI 3Observed1966-07-05 – 1966-08-04SW flank (near Mt. Tabaro)
- 1965VEI 4Observed1965-09-28 – 1965-09-30SW flank (near Mt. Tabaro)
- 1911VEI 3Observed1911-01-27 – 1911-02-08
- 1904VEI 1Observed1904-04-16 – 1904-07-15Base of south wall of main crater
- 1903VEI 2Observed1903-04-16 – end unknown
- 1885VEI ?Method not stated1885-07-02 – end unknown
- 1878VEI 2Observed1878-11-12 – 1878-11-15
- 1874VEI 2Observed1874-07-19 – end unknown
- 1873VEI 2Observed1873-07-02 – end unknown
- 1842VEI 2Observed1842-07-02 – end unknown
- 1825VEI 2Observed1825-07-02 – end unknown
- 1808VEI 2Observed1808-02-16 – 1808-04-16
- 1790VEI 2Observed1790 – end unknown
- 1754VEI 4Observed1754-05-15 – 1754-12-04Summit crater and SE flank
- 1749VEI 4Observed1749-08-11 – 1749-09
- 1731VEI 2Observed1731 – end unknownPira-piraso (NE flank)
- 1729VEI 2Observed1729 – end unknownBinintiang Munti
- 1716VEI 4Observed1716-09-24 – 1716-09-27Calauit (sublacustral SE flank)
- 1715VEI 2Observed1715 – end unknownBinintiang Malaki
- 1709VEI 2Observed1709 – end unknownBinintiang Munti
- 1707VEI 2Observed1707 – end unknownBinintiang Malaki
- 1645VEI 3Observed1645 – end unknown
- 1641VEI 3Observed1641 – end unknown
- 1635VEI 3Observed1635 – end unknown
- 1634VEI 3Observed1634 – end unknown
- 1608 (±3 yrs)VEI 2Observed1608 – end unknown
- 1591VEI 3Observed1591 – end unknown
- 1572VEI 3Observed1572 – end unknown
- 3580 BCE (±200 yrs)VEI 6Geological estimate3580 BCE – end unknown
Nearby volcanoes
External links
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