Final answer:
Mt. Tambora was formed by the interaction between the Eurasian Plate and the Indo-Australian Plate. The Earth's plate tectonics driven by mantle convection cause the Earth's crust to buckle and fold, forming volcanic mountains such as Mt. Tambora.
Step-by-step explanation:
Mt. Tambora, a volcano located on the island of Sumbawa in Indonesia, formed as a result of the interaction between two tectonic plates. The Eurasian Plate and the Indo-Australian Plate are responsible for its formation. The Earth's crust and upper mantle, consisting of many tectonic plates, facilitate various geological phenomena including the formation of volcanic mountains like Mt. Tambora.
Earth experiences global plate tectonics, driven by mantle convection, continually reworking its surface. When these plates are forced together, as with the case of Mt. Tambora, the Earth buckles and folds, causing some rock to be dragged deep below the surface while other areas are thrust upwards. It’s this thrust that forms massive volcanic mountains.
This process is different from that which occurs on other celestial bodies, such as Venus and Mars, due to the differing behavior and characteristics of plate tectonics on these planets. Unlike Earth, they haven't had similar plate tectonic activity. This understanding is crucial for geologists as they attempt to compare and contrast terrestrial processes with those of other planets.
Learn more about Plate Tectonics