Define 'aftershock' and explain why aftershocks occur after the main event.

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Multiple Choice

Define 'aftershock' and explain why aftershocks occur after the main event.

Explanation:
Aftershocks are smaller earthquakes that occur after a larger mainshock as the crust settles into a new balance. When the main rupture happens, it redistributes stress in the surrounding rocks, so nearby faults or patches of the same fault may fail in quick succession as they adjust to the new conditions. This sequence is typically strongest soon after the main event and tends to decrease in both size and frequency over time. Aftershocks stay tied to the same region and fault system as the initial quake, unlike random tremors with no relation or events caused by volcanic activity.

Aftershocks are smaller earthquakes that occur after a larger mainshock as the crust settles into a new balance. When the main rupture happens, it redistributes stress in the surrounding rocks, so nearby faults or patches of the same fault may fail in quick succession as they adjust to the new conditions. This sequence is typically strongest soon after the main event and tends to decrease in both size and frequency over time. Aftershocks stay tied to the same region and fault system as the initial quake, unlike random tremors with no relation or events caused by volcanic activity.

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