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Tambora

Stratovulcano · Indonesia · 2850 m

Tambora volcano on Indonesia's Sumbawa Island produced of the world's largest historical eruption in April 1815. This NASA Landsat mosaic shows the 6-km-wide caldera at the top of the 2,850-m-high summit. Pyroclastic flows during the 1815 eruption reached the sea on all sides of the 60-km-wide volcanic peninsula, and the ejection of large amounts of volcanic gas (aerosols) caused world-wide temperature declines in 1815 and 1816.
Tambora volcano on Indonesia's Sumbawa Island produced of the world's largest historical eruption in April 1815. This NASA Landsat mosaic shows the 6-km-wide caldera at the top of the 2,850-m-high summit. Pyroclastic flows during the 1815 eruption reached the sea on all sides of the 60-km-wide volcanic peninsula, and the ejection of large amounts of volcanic gas (aerosols) caused world-wide temperature declines in 1815 and 1816. · Foto: NASA Landsat 7 image (worldwind.arc.nasa.gov) · Wikimedia Commons
Tipo
Stratovulcano
Paese
Indonesia
Regione
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Altitudine
2850 m
Coordinate
-8.250, 118.000
Ultima eruzione
1967
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Trachybasalt / Tephrite Basanite
Sintesi geologica

The massive Tambora stratovolcano forms the entire 60-km-wide Sanggar Peninsula on northern Sumbawa Island. The largely trachybasaltic-to-trachyandesitic volcano grew to about 4,000 m elevation before forming a caldera more than 43,000 years ago. Late-Pleistocene lava flows largely filled the early caldera, after which activity changed to dominantly explosive eruptions during the early Holocene. Tambora was the source of history's largest explosive eruption, in April 1815. Pyroclastic flows reached the sea on all sides of the peninsula, and heavy tephra fall devastated croplands, causing an estimated 60,000 fatalities. The eruption of an estimated more than 150 km3 of tephra formed a 6-km-wide, 1250-m-deep caldera and produced global climatic effects. Minor lava domes and flows have been extruded on the caldera floor at Tambora during the 19th and 20th centuries.

Sintesi da Wikipedia

Il Tambora o Tomboro è uno stratovulcano dell'isola di Sumbawa, situata nell'arcipelago indonesiano della Sonda. Il vulcano è conosciuto per la devastante eruzione del 1815, una delle poche VEI-7 a memoria storica. Deve la sua origine alla subduzione della placca australiana al di sotto della placca della Sonda.

Wikipedia · CC BY-SA · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
3910 BCE~3714 BCE · 1 eruzioni · VEI max. ?3126 BCE~2930 BCE · 1 eruzioni · VEI max. ?596~792 · 1 eruzioni · VEI max. ?1771~1967 · 4 eruzioni · VEI max. 73910 BCE2539 BCE971 BCE4001771

Cronologia dettagliata

  1. 1967 (±20 anni)VEI 0Osservata
    1967-07-02 – In corso
    NE part of caldera floor
  2. 1880 (±30 anni)VEI 2Osservata
    1880 – In corso
    SW part of caldera (Doro Afi Toi)
  3. 1819VEI 2Osservata
    1819-08 – In corso
  4. 1812VEI 7Osservata
    1812 – 1815-07-15
  5. 740 (±150 anni)VEI ?Stima geologica
    740 – In corso
  6. 3050 a.C.VEI ?Stima geologica
    BCE 3050 – In corso
  7. 3910 a.C. (±200 anni)VEI ?Stima geologica
    BCE 3910 – In corso

Link esterni

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