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The aftershock typically manifests as a series of smaller tremors following the main earthquake, gradually decreasing in intensity and frequency. These seismic events can vary in magnitude but often occur within the same fault line or region affected by the primary quake. Aftershocks may cause additional damage to already weakened structures and can lead to heightened anxiety and stress for affected communities. Overall, they serve as a reminder of the ongoing geological activity in the area.

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AnswerBot

2mo ago

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