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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 (14,100 feet) high, making it one of the tallest peaks in the Indonesian archipelago.
Mount Tambora [92] Indonesia 1815 71,000–250,100+ Largest and deadliest volcanic eruption in recorded history. Caused the "Year Without a Summer" in 1816. 4 Mount Mayon [71] Philippines 1814 1,200 The town of Cagsawa was buried and approximately 1,200 people were killed. [93] 4 Suwanosejima [74] Japan 1813 4 Mount Awu [28] Indonesia 1812 4 La ...
This cooling directly or indirectly caused 90,000 deaths. The eruption of Mount Tambora was the largest cause of this climate anomaly. [22] While there were other eruptions in 1815, Tambora is classified as a VEI-7 eruption with a column 45 km (148,000 ft) tall, eclipsing all others by at least one order of magnitude.
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The 1815 eruption of Mount Tambora on Sumbawa and the 1257 eruption of Mount Samalas on Lombok were among the largest in the last two millennia, ranking 7 on the VEI scale. [14] The Sunda Arc subduction zone was also the site of one of the largest known eruptions of the Cenozoic , the VEI 8 Toba supereruption on Sumatra , which expelled 2,800 ...
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The peak after 1815 was caused by the Mount Tambora eruption. The 1808 mystery eruption is one or potentially multiple unidentified volcanic eruptions that resulted in a significant rise in stratospheric sulfur aerosols, leading to a period of global cooling analogous to the Year Without a Summer in 1816. [2] [3] [4]
The eruption is believed to have contributed to the accumulation of atmospheric ash, [citation needed] capped by the catastrophic eruption of Mount Tambora in 1815, that led to the Year Without a Summer in 1816. Pinatubo eruption: 1500 to 2021: Reawakened in 1991 producing the 2nd largest eruption in the 20th century.