The 62 AD earthquake in Pompeii is attributed to the tectonic activity in the region, which is situated near the boundary of the African and Eurasian tectonic plates. This seismic event resulted from the movement and stress along faults in the earth's crust. The earthquake caused significant damage to structures in Pompeii and surrounding areas, highlighting the vulnerability of the region to geological hazards. Additionally, it served as a precursor to the more catastrophic eruption of Mount Vesuvius in 79 AD.
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