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Fractures in bedrock along which movement has taken place are known as faults. These geological structures occur when stress on the Earth's crust exceeds the strength of the rock, causing it to break and move. Faults can lead to significant geological events, such as earthquakes, and can vary in size and type, including normal, reverse, and strike-slip faults. The movement along these fractures can result in displacement of the rock layers on either side.

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