In 1812, the mountain began to emit small amounts of ash and steam. It caused some tsunamis when the pyroclastic flows hit the water. It was formed due to the active subduction zones beneath it, and before its 1815 eruption, it was more than 4,300 metres (14,100 feet) high, making it one of the tallest peaks in the Indonesian archipelago.
The tremendous eruption of Mount Tambora in April 1815 was the most powerful volcanic eruption of the 19th century. Its 1815 explosion was possibly the most destructive ever recorded. Tambora stood over 14,000 feet high in 1815, but when it blew its stack it hurled more than 4,000 feet off the top of it, leaving a crater more than four miles across and 2,000 feet deep. Every now and again Mount Tambora erupts. About 90,000 people in total died. Mount Tambora, or Tomboro, is an active stratovolcano in the northern part of Sumbawa, one of the Lesser Sunda Islands of Indonesia. The Eruption The Tambora eruption was caused by ocean water penetrating cracks and fissures in the mountain. It also generated some earthquakes and whirlwinds. Tambora’s catastrophic eruption began on April 5, 1815, with small tremors and pyroclastic flows. When it reacted with magma deep inside the volcano, massive pressure built up, causing the mountain to blow itself apart.
Mount Tambora is an active volcano on the island of Sumbawa in Indonesia. A shattering blast blew the mountain apart on the evening of April 10. The Eruption of Mount Tambora: Causes, Event, Effect Mount Tambora, is an active stratovolcano famous for its eruption in 1815 which was considered one of the most explosive volcanic eruptions in Earthʼs history. Its eruption in 1815 is the most powerful volcanic eruption in recorded history and is considered one of the greatest natural disasters ever to befall mankind. The 1815 eruption of Mount Tambora was the most powerful Volcanic eruption in human recorded history, with a Volcanic Explosivity Index (VEI) of 7. The blast, pyroclastic flows, and tsunamis that followed killed at least 10,000 islanders and destroyed the homes of 35,000 more. The eruptionand the tsunamisit triggered killed tens of thousands of people. The magnitude of the explosion itself is difficult to fathom.
It is the most recently known VEI-7 event and the only unambiguously confirmed VEI-7 eruption since the Lake Taupo eruption in about 180 AD. A stratovolcano is a volcano characterized by its steepness and periodic explosive eruptions and quiet eruptions. A lot of damage was caused.
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