This story is from September 27, 2023

Quake shakes Italy's volcanic Campi Flegrei

A 4.2-magnitude earthquake hit Italy's Campi Flegrei region without causing any injuries or damage. Campi Flegrei is a flat volcano located west of Naples. Although less known than Vesuvius, recent increased activity has raised concerns. The earthquake occurred at a depth of three kilometers and was felt across Naples. The mayor of Bacoli, a town near Naples, assured residents that they must learn to live with the volcanic activity and stay calm. The spike in activity is believed to be caused by gas bubbling up, making the probability of an eruption relatively low.
Quake shakes Italy's volcanic Campi Flegrei
Representative Image
ROME: A 4.2-magnitude earthquake shook Italy's Campi Flegrei region west of Naples in the early hours Wednesday, scaring residents but causing no injuries or damage, according to the civil protection agency.
The Campi Flegrei (Phlegraean Fields) is a vast volcano, though it is flat rather than cone-shaped. While less well-known than nearby Vesuvius, a recent increase in activity has rattled nerves.
The quake struck at 3:35 am (0135 GMT) at a depth of around three kilometres (nearly two miles), and was felt across much of Naples.

Josi Gerardo Della Ragione, mayor of Bacoli, a coastal town on the outskirts of the southern Italian city, said it had been "the strongest of this long earthquake swarm... and among the longest".
"We have always been living on a volcanic caldera," he said, using the term for a large, cauldron-like hollow that forms after an eruption.
"We have to learn to live with this phase. Stay calm," Della Ragione told locals in a social media message.
Half a million people live on the Campi Flegrei, which last spewed lava, ashes and rocks in 1538.
The volcano's eruption 30,000 years ago is reported to have contributed to the extinction of Neanderthal man.
But Italy's National Institute of Geophysics and Volcanology (INGV) said earlier this month that it believes the spike in activity could be caused by gas bubbling up, rather than magma, making "the probability of an eruption relatively low".
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