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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, with 2 in critical condition, and caused material damage. Dozens of lower-intensity aftershocks shook the area throughout the night. The region borders the Campi Flegrei (Phlegrean Fields), an active volcanic caldera that has been under continuous seismic monitoring by Italian authorities due to persistent seismic activity in recent years.
A 4.7-magnitude earthquake struck the Naples region in southern Italy on Friday evening, July 31, according to Le Monde. It injured 21 people, with 2 in critical condition, and caused material damage.
Dozens of lower-intensity aftershocks shook the area throughout the night.
The Naples region borders the Campi Flegrei (Phlegrean Fields), an active volcanic caldera west of the city. This sector is subject to bradyseism — a geological phenomenon involving slow ground deformation (uplift or subsidence) linked to magmatic or hydrothermal activity at depth — which is accompanied by recurrent seismic swarms.
The Istituto Nazionale di Geofisica e Vulcanologia (INGV), Italy's seismic and volcanic monitoring agency, continuously monitors the zone. Since 2023, Italian authorities have maintained a yellow alert level (allerta gialla) and report hundreds of tremors per month, along with continuous ground uplift.
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The precise location of the epicenter within the Naples region — in particular, its potential connection to the Campi Flegrei zone — has not been clearly specified in available information. The full extent of material damage and the specific nature of the two critical injuries remain unclear at this stage.
The tremor reached a magnitude of 4.7.
21 people were injured, with 2 in critical condition.
Bradyseism is a geological phenomenon involving slow ground deformation — uplift or subsidence — characteristic of active volcanic calderas. The Naples region borders the Campi Flegrei, an active caldera where this phenomenon, accompanied by seismic swarms, is documented and continuously monitored by Italian authorities.