Earthquake a little while ago in Naples and in the Phlegraean Fields. magnitude 1.6
Shock in the Campi Flegrei area. No damage but distinctly felt by the population.
An earthquake was distinctly felt by the population of the western area of Naples shortly before 11 pm today, Sunday 27 March. It is once again the seismic activity that falls in the Phlegraean caldera, so the telluric event was felt in Naples between Bagnoli and Agnano and in the Pozzuoli area, between the solfatara and the center of Puteola. Many reports especially on social networks and neighborhood groups. The magnitude of the earthquake is 1.6 Richter scale even if the roar and the subsequent tremor were distinctly felt in the western quadrant of Naples, in the middle of the Flegrean area. The quake was 2 kilometers deep.
Writes the mayor of Pozzuoli, Vincenzo Figliolia:
The Vesuvian Observatory has communicated the occurrence of a seismic event of magnitude 1.6 located in the Solfatara-Pisciarelli area. The quake occurred at 10:49 pm local time at a depth of 1.5 kilometers.
At the moment they are not due to accidents or inconveniences on the part of the population or to the Municipal Police or to the Night Presidium at the Civil Protection Office and during the checks no damages or other significant derivative effects were found.
The event may have been accompanied by a roar felt by the inhabitants of the area at the epicenter.
More information on the phenomena in progress and on the evolution of lifting bradyseism that has been affecting the municipal area for several decades can be found on the Vesuvian Observatory – INGV website (http://www.ov.ingv.it/ov/ ).
The quake of March 16
In recent days, precisely on March 16, in the same area one of the strongest tremors in recent years, magnitude 3.5.
Earthquake in Naples magnitude 3.5 between Bagnoli and Pozzuoli on March 16, 2022
For Francesca Whitedirector of the Naples section of the National Institute of Geophysics and Volcanology, it is however a seismic activity attributable to the phenomenon of bradyseism, typical of the Phlegraean Fields.
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