Volcanology
A collapse caldera is a large depression formed when a volcanic eruption leads to the emptying of a magma chamber, causing the ground above it to sink or collapse. This geological feature often occurs after a massive explosive eruption, which drains significant amounts of magma from the chamber, resulting in the roof of the chamber becoming unsupported and collapsing into it. The formation of collapse calderas can significantly alter the landscape and can lead to the development of new volcanic features.
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