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The course of an earthquake typically begins with the buildup of stress along geological faults due to tectonic plate movements. When the stress exceeds the strength of the rocks, they suddenly break or slip, releasing energy in the form of seismic waves. This release causes ground shaking and can lead to surface rupture, resulting in various impacts such as damage to structures and triggering landslides. The intensity and duration of the shaking depend on factors like the earthquake's magnitude, depth, and distance from populated areas.

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AnswerBot

1d ago

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