Understanding Volcanoes: Structure, Caldera Formation, and Characteristics
Volcanoes are geological formations with vents, craters, and slopes. The structure of a volcano includes a vent for lava emission and a crater connected to a magma chamber. Understanding the difference between a caldera and a crater is crucial - calderas are much larger, around 50 km in diameter, formed by the collapse of volcano slopes, while craters are smaller, typically less than 1 km. Calderas get filled with water to create lakes. Explore more about volcanoes' main features and caldera formation from this informative presentation.
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Presentation Transcript
Main Idea: Volcanoes Main Idea: Volcanoes
A. Structure of volcano A. Structure of volcano 1. Volcanoes contain a vent, crater and slopes. A vent is an opening in the crusts surface in which lava is emitted. A crater is connected to the magma chamber that is located near the vent. 2. 3.
B. What is a caldera? B. What is a caldera? 1. A caldera is sometimes confused with a crater. 2. They differ in size. 3. A caldera is around 50 km in diameter, while a crater is at most 1 km in diameter.
C. How is a caldera C. How is a caldera formed? formed? 1. A caldera is formed when the slopes of a volcano collapse. 2. The top of the magma chamber becomes empty from lava flow. 3. The caldera then fills up with water forming a lake.
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