description Tambora fumaroles Overview
The fumaroles of Mount Tambora are steam and gas vents produced by geothermal activity within the volcano's caldera on Sumbawa Island, Indonesia. Tambora is known for its exceptionally large eruption in 1815, which caused widespread local destruction and significant climatic effects around the world. The fumaroles are later surface expressions of heat and volcanic gases beneath the caldera. They are part of the active volcanic landscape monitored for changes in temperature, gas release, and seismic activity.
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