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Beyond the initial shaking, the aftershocks are a critical factor in understanding the **_overall duration of the seismic event_**. These are smaller earthquakes that occur in the same general area as the mainshock, following the initial rupture. They happen because the main earthquake changes the stress levels in the surrounding rocks, causing them to readjust and sometimes fracture further. Aftershocks can continue for days, weeks, or even months after the main quake, and while they are generally weaker, they can still be strong enough to cause additional damage, especially to buildings already weakened by the initial earthquake. They also pose a significant risk to rescue workers and survivors, making the already difficult task of searching for victims and providing aid even more dangerous. The psychological impact of these ongoing tremors cannot be overstated either, as they keep people in a constant state of anxiety and fear.
