Indonesia · Stratovolkan
Gunung Tambora
Tambora
- Tipe
- Stratovolkan
- Ketinggian
- 2850 m
- Letusan terakhir
- 1967

- Tipe
- Stratovolkan
- Negara
- Indonesia
- Wilayah
- Sunda & Banda / Sunda Volcanic Arc
- Ketinggian
- 2850 m
- Koordinat
- -8.250, 118.000
- Letusan terakhir
- 1967
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Trakibasal / Tefrit basanit
Ringkasan geologi
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.
Riwayat letusan
7 tercatatGlosariumGaris waktu rinci
- 1967 (±20 tahun)VEI 0Teramati1967-07-02 – akhir tidak diketahuiNE part of caldera floor
- 1880 (±30 tahun)VEI 2Teramati1880-07-02 – akhir tidak diketahuiSW part of caldera (Doro Afi Toi)
- 1819VEI 2Teramati1819-08-16 – akhir tidak diketahui
- 1812VEI 7Teramati1812-07-02 – 1815-07-15
- 740 (±150 tahun)VEI ?Perkiraan geologi740 – akhir tidak diketahui
- 3050 SMVEI ?Perkiraan geologi3050 SM – akhir tidak diketahui
- 3910 SM (±200 tahun)VEI ?Perkiraan geologi3910 SM – akhir tidak diketahui
Gunung api terdekat
Tautan eksternal
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