Pinatubo
Stratovulcano · Philippines · 1486 m
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- Tipo
- Stratovulcano
- Paese
- Philippines
- Regione
- Pacifico occidentale / Luzon Volcanic Arc
- Altitudine
- 1486 m
- Coordinate
- 15.130, 120.350
- Ultima eruzione
- 2021
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Dacite
Sintesi geologica
Prior to 1991 Pinatubo volcano was a relatively unknown, heavily forested lava dome complex located 100 km NW of Manila with no records of historical eruptions. The 1991 eruption, one of the world's largest of the 20th century, ejected massive amounts of tephra and produced voluminous pyroclastic flows, forming a small, 2.5-km-wide summit caldera whose floor is now covered by a lake. Caldera formation lowered the height of the summit by more than 300 m. Although the eruption caused hundreds of fatalities and major damage with severe social and economic impact, successful monitoring efforts greatly reduced the number of fatalities. Widespread lahars that redistributed products of the 1991 eruption have continued to cause severe disruption. Previous major eruptive periods, interrupted by lengthy quiescent periods, have produced pyroclastic flows and lahars that were even more extensive than in 1991.
Sintesi da Wikipedia
Riassunto in ingleseMount Pinatubo is an active stratovolcano in the Zambales Mountains in Luzon in the Philippines. Located on the tripoint of Zambales, Tarlac and Pampanga provinces, most people were unaware of its eruptive history before the pre-eruption volcanic activity in early 1991. Dense forests, which supported a population of several thousand indigenous Aetas, heavily eroded and obscured Pinatubo.
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Storia delle eruzioni
Cronologia dettagliata
- 2021VEI 1Osservata2021-11-30 – 2021-11-30
- 1993VEI 1Osservata1993-02-16 – 1993-07-16Caldera floor
- 1992VEI 1Osservata1992-07-09 – 1992-10-30Center of caldera lake
- 1991VEI 6Osservata1991-04-02 – 1991-09-02Lower north flank and summit
- 1450 (±50 anni)VEI 5Stima geologica1450 – In corso
- 1050 a.C. (±500 anni)VEI 6Stima geologicaBCE 1050 – In corso
- 3550 a.C.VEI 6Stima geologicaBCE 3550 – In corso
- 7030 a.C. (±300 anni)VEI ?Stima geologicaBCE 7030 – In corso
- 7460 a.C. (±150 anni)VEI 6Stima geologicaBCE 7460 – In corsoTayawan caldera
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.