Is Mount Tambora on a destructive plate boundary?
Is Mount Tambora on a destructive plate boundary?
Mount Tambora formed at a convergent plate boundary, where the Indo-Australian Plate subducts under the Eurasian Plate. Tambora is a stratovalcano, with an elevation of 2,850m (9,350ft). When the volcano erupted in 1815, it was given a volcanic explosion index (VEI) of 7.
What kind of damage did Mount Tambora cause?
The blast, pyroclastic flows, and tsunamis that followed killed at least 10,000 islanders and destroyed the homes of 35,000 more.
What type of eruption was Mount Tambora?
volcanic eruption
The 1815 eruption of Mount Tambora was the most powerful volcanic eruption in recorded human history, with a Volcanic Explosivity Index (VEI) of 7….
| 1815 eruption of Mount Tambora | |
|---|---|
| Volcano | Mount Tambora |
| Start date | 1815 |
| Type | Ultra Plinian |
Is Mount Tambora monitored?
An event as significant as the 1815 eruption would impact about eight million people. Seismic activity in Indonesia is monitored by the Directorate of Volcanology and Geological Hazard Mitigation with the monitoring post for Mount Tambora located at Doro Peti village.
What is the destructive legacy of Mount Tambora?
Destructive legacy: a NASA photograph of the huge caldera formed when Mount Tambora erupted in 1815. The volcano looms over the Java Sea from the northern shore of the island of Sumbawa, which lies towards the eastern end of the former Dutch East Indies, now Indonesia.
How tall was Mount Tambora before the 1815 eruption?
It has been estimated that Mount Tambora stood approximately 12,000 feet tall before the 1815 eruption when the top third of the mountain was completely obliterated.
What type of volcano is Tambora?
Tambora is classified by specialists as Ultraplinian, the most violent of all categories of volcanic eruption, named in honour of the Younger Pliny’s description of the destruction of Pompeii by Vesuvius in AD 79. Such eruptions propel quantities of sulphurous gases into the stratosphere,…
Are there active fumaroles on Mount Tambora?
Active fumaroles, or steam vents, still exist in the caldera. In 2004, scientists discovered the remains of a village, and two adults buried under approximately 3 meters (nearly 10 feet) of ash in a gully on Tambora’s flank—remnants of the former Kingdom of Tambora preserved by the 1815 eruption that destroyed it.