A powerful earthquake measuring 4.7 magnitude struck a region near Naples in southern Italy on Friday evening at 7:46pm, resulting in at least 26 injuries and widespread disruption across the area. The tremor, which occurred at a depth of 3 kilometers, was the strongest to affect the region in the past 40 years and was felt across Naples, the island of Ischia, and as far as the Sorrento peninsula. The quake triggered power outages affecting approximately 100,000 households, disrupted public transportation including high-speed rail services experiencing delays of up to six hours, and caused structural damage to buildings and infrastructure.
The epicenter was located near Pozzuoli in the Campi Flegrei area, home to Europe’s largest volcanic crater. The seismic event triggered landslides and prompted the evacuation of roughly 300 residents from their homes due to safety concerns. At least five injured individuals required hospitalization, while numerous residents spent the night outdoors fearing additional collapses. Structural inspections subsequently deemed nine buildings unsafe for occupancy. One rescuer described a survivor as alive “by a miracle” after part of a cliff collapsed, and portions of buildings fell, crushing parked vehicles though causing no fatalities from that particular incident.
The earthquake was part of an ongoing seismic swarm affecting the region, with approximately 60 additional tremors recorded following the main quake. A secondary earthquake measuring 3.1 magnitude struck at 5:47am and was felt by residents across Bacoli, Pozzuoli, and Naples. Italy’s national institute of geophysics and volcanology confirmed the activity represented continued seismic disturbance in the area. Civil protection minister Nello Musumeci cautioned residents that volcanic activity had not yet concluded and urged continued vigilance.
The Pozzuoli pier sustained damage rendering it unusable, leading authorities to suspend ferry and hydrofoil service to nearby islands. Rescue personnel highlighted concerns about ongoing geological instability, noting that ground movement in the area had been documented for an extended period prior to the earthquake. Questions emerged regarding advance preparation and preventive measures that might have been implemented to mitigate the impacts of the foreseeable seismic risk in the densely populated region.
Article Attribution | Read More at Article Source
Article summary produced by Claude AI