Tambora
Stratovolcano · Indonesia · 2850m

- Type
- Stratovolcano
- Country
- Indonesia
- Region
- Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
- Elevation
- 2850m
- Coordinates
- -8.250, 118.000
- Last eruption
- 1967
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Trachybasalt / Tephrite Basanite
Geological summary
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.
From Wikipedia
Mount Tambora, or Tomboro, is an active stratovolcano in West Nusa Tenggara, Indonesia. Located on Sumbawa in the Lesser Sunda Islands, volcanism is the result of subduction zones. The 1815 eruption was the largest in recorded history, erupting up to 150 cubic kilometers of volcanic material, making it a VEI-7 on the Volcanic Explosivity Index. This caused the summer of 1816 to become known as the "Year Without a Summer" due to global cooling from the eruption.
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Eruption history
Detailed timeline
- 1967 (±20 yrs)VEI 0Observed1967-07-02 – OngoingNE part of caldera floor
- 1880 (±30 yrs)VEI 2Observed1880 – OngoingSW part of caldera (Doro Afi Toi)
- 1819VEI 2Observed1819-08 – Ongoing
- 1812VEI 7Observed1812 – 1815-07-15
- 740 (±150 yrs)VEI ?Geological estimate740 – Ongoing
- 3050 BCEVEI ?Geological estimateBCE 3050 – Ongoing
- 3910 BCE (±200 yrs)VEI ?Geological estimateBCE 3910 – Ongoing
External links
⚠ For reference only. Not for emergency response.