The Phlegraean Fields are an active volcanic area with a \"caldera\" structure: a lowered area with an almost circular shape which formed as a result of large explosive eruptions. The Campi Flegrei caldera extends from Monte di Procida to Posillipo and also includes an underwater part in the Gulf of Pozzuoli. More than 70 eruptions have occurred over the past 15,000 years, forming volcanic edifices, craters and volcanic lakes that are still clearly visible, such as Astroni, the Solfatara and Lake Averno.
\r\nThe last eruption dates back to 1538. Since then, the area has been characterised by fumaroles, repeated episodes of slow soil deformation (bradyseism) and earthquakes.
The Phlegraean Fields are an active volcanic area with a \"caldera\" structure: a lowered area with an almost circular shape which formed as a result of large explosive eruptions. The Campi Flegrei caldera extends from Monte di Procida to Posillipo and also includes an underwater part in the Gulf of Pozzuoli. More than 70 eruptions have occurred over the past 15,000 years, forming volcanic edifices, craters and volcanic lakes that are still clearly visible, such as Astroni, the Solfatara and Lake Averno.
\nThe last eruption dates back to 1538. Since then, the area has been characterised by fumaroles, repeated episodes of slow soil deformation (bradyseism) and earthquakes.
The Phlegraean Fields is a vast active volcanic area with a structure called a \"caldera,\" that is, a lowered area with an almost circular shape that was formed by large explosive eruptions. The caldera of the Phlegraean Fields extends from Monte di Procida to Posillipo and also includes an underwater part in the Gulf of Pozzuoli. Within the caldera, more than 70 eruptions have occurred over the past 15,000 years, forming volcanic buildings, craters and volcanic lakes that are still visible, such as Astroni, Solfatara and Lake Averno. The last eruption, in 1538, was preceded by a ground uplift that reached 19 meters in two years and gave rise to the volcano Monte Nuovo. Since then, the caldera has been quiescent, \"dormant,\" but now shows signs of activity such as seismicity, fumaroles, and ground deformation.
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\r\n\r\nShare what you know with family, school, friends and colleagues: spreading information about volcanic risk is a collective responsibility, and we all have to contribute.
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\n","value":"Bradyseism consists of phases of slow ground lowering, alternating with phases of more rapid ground uplift. The uplift can be accompanied by seismic activity with events that usually do not reach high magnitudes. However, since they are very shallow, they are easily perceived and can damage infrastructure and buildings. Therefore, knowing what to do in case of an earthquake is essential.
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