A caldera is a large, bowl-shaped depression that forms following the evacuation of a magma chamber/reservoir beneath a volcano. Calderas are some of the most spectacular features on Earth, often measuring several kilometers in diameter and are commonly associated with explosive volcanic eruptions. They can also be formed by the collapse of a volcano following the emptying of an underground magma chamber.
Calderas are typically formed through one of the following processes:
Calderas can be classified into several types based on their formation and structure:
To understand calderas better, it is essential to study the following concepts:
By studying these concepts, you can gain a comprehensive understanding of calderas and their significance in the field of geology and volcanic studies.