Mount Tambora formed as a result of a subduction zone. Here, a section of the ocean floor that is part of the Indo-Australian Plate is sliding under part of the Eurasian Plate and into the mantle. The oceanic crust takes some water and other volatiles with it. This seeps into the superheated rock of the mantle, allowing it to melt. It then rises toward the surface and through the crust via cracks. This then emerges on the surface, forming volcanoes such as Mount Tambora.
The eruption of Mount Tambora occurred from April 5 to April 15, 1815.
The eruption of Mount Tambora happened on the island of Sumbawa in Indonesia in April 1815. It is considered one of the most powerful volcanic eruptions in recorded history.
Mount Tambora is a volcanic mountain in Indonesia, so it does not have a population since it is a geological feature.
The Mount Tambora eruption occurred in the state of West Nusa Tenggara in Indonesia.
No. Mount Tambora is in the shape of a caldera form from a stratovolcano.
The eruption of Mount Tambora occurred from April 5 to April 15, 1815.
Mount Tambora is in the Indonesian archipelago.
The eruption of Mount Tambora happened on the island of Sumbawa in Indonesia in April 1815. It is considered one of the most powerful volcanic eruptions in recorded history.
it erupted in the year 1815
The 1815 eruption of Mount Tambora was a V.E.I. 7.
Mount Tambora is 4,300 m (14,000 ft) high.
Mount Tambora is a stratovolcano and its over 5000 years old.
Mount Tambora erupted in 1815-16 April15-16
Mount Tambora is located on the Eurasian plate and another one these are converging plates
Mount Tambora is a volcanic mountain in Indonesia, so it does not have a population since it is a geological feature.
The Mount Tambora eruption occurred in the state of West Nusa Tenggara in Indonesia.
No. Mount Tambora is in the shape of a caldera form from a stratovolcano.