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The Phlegraean Fields are an active volcanic area with a structure called \"caldera\" : a low-lying area with an almost circular shape that was formed as a result of large explosive eruptions. The Phlegraean Fields 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 ground deformation (bradyseism) and earthquakes.
The Phlegraean Fields are an active volcanic area with a structure called \"caldera\" : a low-lying area with an almost circular shape that was formed as a result of large explosive eruptions. The Phlegraean Fields 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 ground deformation (bradyseism) and earthquakes.
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 volcanic gas emissions (fumaroles), and bradyseism.
\n","value":"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 volcanic gas emissions (fumaroles), and bradyseism.
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\nShare what you know with family, at school, friends, and colleagues: spreading information about volcanic risk is a collective responsibility, and we all must contribute.
\n","value":"Awareness of risk and knowledge of the Civil Protection Plan is a responsibility for all of us. With simple actions you can better prepare for an emergency.
\r\n\r\nShare what you know with family, at school, friends, and colleagues: spreading information about volcanic risk is a collective responsibility, and we all must contribute.
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