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World
Herz — World Desk · · 30s summary · 2 min read
A 4.7-magnitude earthquake struck the Naples region in southern Italy on Friday evening, July 31, according to Le Monde. The quake injured 21 people, including 2 critically, and caused material damage. Dozens of lower-intensity aftershocks followed throughout the night. The area borders the Phlegraean Fields, an active volcanic caldera that has been under continuous seismic surveillance by Italian authorities for several years.
A 4.7-magnitude earthquake struck the Naples region in southern Italy on Friday, July 31, in the evening, according to Le Monde. It injured 21 people, including 2 critically, and caused material damage.
Dozens of lower-intensity aftershocks shook the area throughout the night.
The Naples region borders the Phlegraean Fields (Campi Flegrei), an active volcanic caldera west of the city. This sector experiences bradyseism—a phenomenon of slow ground deformation (subsidence or uplift) linked to magmatic or hydrothermal activity at depth—which is accompanied by recurrent seismic swarms.
The National Institute of Geophysics and Volcanology (INGV), Italy's seismic and volcanic monitoring agency, monitors the area continuously. Since 2023, Italian authorities have maintained a yellow alert level (allerta gialla) and report hundreds of tremors per month, as well as continuous ground uplift.
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The precise location of the epicenter within the Naples region—specifically any potential link to the Phlegraean Fields area—is not clarified in available information. The detailed extent of material damage and the nature of the injuries in the two critical cases are not yet disclosed.
The earthquake reached a magnitude of 4.7.
21 people were injured, including 2 critically.
Bradyseism is a phenomenon of slow ground deformation—subsidence or uplift—specific to active volcanic calderas. The Naples region borders the Phlegraean Fields, an active caldera where this phenomenon, accompanied by seismic swarms, is documented and continuously monitored by Italian authorities.