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  1. El Mont Tambora és un volcà actiu, situat a l'illa de Sumbawa, una de les Illes Petites de la Sonda . És de tipus estratovolcà, mesura 60 quilòmetres de diàmetre, assoleix una altitud de 2.722 metres i el seu cràter caldera fa 8 quilòmetres de diàmetre i 1 quilòmetre de profunditat.

  2. Mount Tambora (8°14’41”S, 117°59’35”E) is an active volcano in Indonesia. It is on top of a subduction zone. Tambora was taller before its explosive volcanic eruption in 1815. This killed tens of thousands of people around the world. Later eruptions have been smaller.

  3. O monte Tambora entrou em erupção entre 5 e 10 de abril de 1815, atingindo o nível 7 no Índice de Explosividade Vulcânica (IEV), realizando a maior erupção desde a erupção do lago Taupo no ano 181 d.C. Esta erupção é considerada a maior registrada na Terra, detendo o recorde do volume de matéria expelida: 180 000 000 000 m³ ou 180 ...

  4. Monte Tambura is a mountain (1,891 m) in the Alpi Apuane, in Tuscany, central Italy. It is the second highest peak in the chain after Monte Pisanino . Located on the boundary between the province of Lucca and the province of Massa-Carrara , the Tambura is part of the Natural Regional Park of the Alpi Apuane.

  5. 2 de nov. de 2023 · Media in category "Mount Tambora". The following 30 files are in this category, out of 30 total. Blick OstrandIMG 6537.jpg 4,320 × 3,240; 1.41 MB. Caldera Mt Tambora Sumbawa Indonesia.jpg 900 × 600; 151 KB. Calderaboden des Tambora.jpg 4,320 × 3,240; 1.91 MB. FMIB 50001 Eruption of Tomboro in 1821.jpeg 657 × 640; 146 KB.

  6. 27 de dic. de 2021 · Según el Índice de Explosividad Volcánica del Estudio Geológico de Estados Unidos, Tambora recibe una calificación de 7 en una escala de 8, y es del tipo Ultra Pliniana. Eso es diez veces más potente que la erupción del Monte Pinatubo en 1991, y cien veces mayor que el estallido del Monte Santa Helena en 1981.

  7. Mount Tambora, or Tomboro, is an active stratovolcano in West Nusa Tenggara, Indonesia. Located on Sumbawa in the Lesser Sunda Islands, it was formed by the active subduction zones beneath it. Before 1815, its elevation reached more than 4,300 metres high, making it one of the tallest peaks in the Indonesian archipelago.