{"componentChunkName":"component---src-templates-pagina-foglia-completa-template-en-jsx","path":"/en/get-ready/volcanoes/phlegraen-fields/what-know/","result":{"data":{"node":{"title":"What to know - Volcanic risk","field_titolo_esteso":"What to know - Volcanic risk","field_data":"2022-09-26T09:35:47+02:00","drupal_internal__nid":900005598,"field_id_contenuto_originale":900005597,"field_categoria_primaria":"pagina","field_streaming_homepage":false,"field_link":null,"body":{"processed":"

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.

\n"},"fields":{"slug":"/get-ready/volcanoes/phlegraen-fields/what-know/"},"field_link_esterni":[{"title":"Vesuvius Observatory - INGV","uri":"https://www.ov.ingv.it/"}],"field_tabella":null,"relationships":{"field_immagine_dettaglio":{"field_alt":"What to know?","field_titolo_esteso":"Cosa sapere - immagine evidenza versione inglese","relationships":{"image":{"localFile":{"publicURL":"/static/c812d3a3b329f4b26846be30eb17df8b/what-know.jpg","childImageSharp":{"fluid":{"aspectRatio":1.5027322404371584,"src":"/static/c812d3a3b329f4b26846be30eb17df8b/14b42/what-know.jpg","srcSet":"/static/c812d3a3b329f4b26846be30eb17df8b/cf463/what-know.jpg 275w,\n/static/c812d3a3b329f4b26846be30eb17df8b/dee3b/what-know.jpg 550w,\n/static/c812d3a3b329f4b26846be30eb17df8b/14b42/what-know.jpg 800w","sizes":"(max-width: 800px) 100vw, 800px"}}}}}},"field_sottodominio":{"name":"Io Non Rischio"},"field_immagine_singola":null,"field_mappa":null,"field_riferimento_traduzione":{"fields":{"slug":"/preparati/vulcani/campi-flegrei/cosa-sapere/"}},"field_box_social":null,"field_accordion":[{"field_titolo":"The phenomenon of bradyseism","field_tabella":null,"field_testo":{"processed":"

The caldera of the Phlegraean Fields is featured by the phenomenon of bradyseism, which shows slow lowering (subsidence) and more rapid uplift phases. The most recent major bradyseism crises occurred between 1969-1972 and 1982-1984, resulting in a total ground uplift of more than three meters and hundreds of earthquakes. During these crises, Pozzuoli's historic center residents were evacuated and relocated to neighborhoods on the city's outskirts.

\n

Since 2006, a new phase of ground uplift has been ongoing. In 16 years, the ground has risen by about one meter and caused many earthquakes.

\n

Since 2012, the prolonged variations in some geophysical and geochemical parameters recorded by the monitoring networks of the INGV—Vesuvius Observatory (increased seismicity, changes in the geochemical composition of fumaroles and gases from the ground, and, of course, soil uplift) have required raising the warning to yellow level and activating the operational phase of \"attention.\"

\n","value":"

The caldera of the Phlegraean Fields is featured by the phenomenon of bradyseism, which shows slow lowering (subsidence) and more rapid uplift phases. The most recent major bradyseism crises occurred between 1969-1972 and 1982-1984, resulting in a total ground uplift of more than three meters and hundreds of earthquakes. During these crises, Pozzuoli's historic center residents were evacuated and relocated to neighborhoods on the city's outskirts.

\r\n\r\n

Since 2006, a new phase of ground uplift has been ongoing. In 16 years, the ground has risen by about one meter and caused many earthquakes.

\r\n\r\n

Since 2012, the prolonged variations in some geophysical and geochemical parameters recorded by the monitoring networks of the INGV—Vesuvius Observatory (increased seismicity, changes in the geochemical composition of fumaroles and gases from the ground, and, of course, soil uplift) have required raising the warning to yellow level and activating the operational phase of \"attention.\"

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In the past, the volcanic activity of the Phlegraean Fields has been mainly characterized by explosive eruptions. This type of eruption, and the following phenomena, could also be expected in the future:

\n","value":"

In the past, the volcanic activity of the Phlegraean Fields has been mainly characterized by explosive eruptions. This type of eruption, and the following phenomena, could also be expected in the future:

\r\n\r\n\r\n"},"relationships":{"field_immagine":null,"field_video":null,"field_link_interni":[]},"drupal_internal__id":19615},{"field_titolo":"Can eruption in the Phlegraean Fields be predicted?","field_tabella":null,"field_testo":{"processed":"

Phlegraean Fields are among the most monitored volcanoes in the world because eruptions are often preceded by “precursor” phenomena (earthquakes, soil deformations, changes in composition and temperature of fumaroles, etc.).

\n

The monitoring of these phenomena is fundamental to determine the state of activity of the volcano, the alert level, and also for the implementation of the measures provided for in the Civil Protection Plan. However, the present scientific knowledge does not allow to predict with certainty when, how and where the next eruption will occur, also because of the peculiarities of the caldera. Also, it is not possible to predict the duration of the eruption.

\n","value":"

Phlegraean Fields are among the most monitored volcanoes in the world because eruptions are often preceded by “precursor” phenomena (earthquakes, soil deformations, changes in composition and temperature of fumaroles, etc.).

\r\n\r\n

The monitoring of these phenomena is fundamental to determine the state of activity of the volcano, the alert level, and also for the implementation of the measures provided for in the Civil Protection Plan. However, the present scientific knowledge does not allow to predict with certainty when, how and where the next eruption will occur, also because of the peculiarities of the caldera. Also, it is not possible to predict the duration of the eruption.

\r\n"},"relationships":{"field_immagine":null,"field_video":null,"field_link_interni":[]},"drupal_internal__id":19616},{"field_titolo":"How does the warning work?","field_tabella":null,"field_testo":{"processed":"

The alert system provides specific “alert levels” describing the state of activity of the volcano, based on the parameters of monitoring and any ongoing phenomena. The green alert level corresponds to the ordinary activity of the volcano while the yellow, orange and red alert levels represent increasing stages of unbalance of the volcano towards a possible eruption. The duration of each alert level can be extremely variable.

\n

The alert levels are declared by the Department of Civil Protection, in conjunction with the regional civil protection. A possible change in level is assessed on the basis of the indications provided by the Vesuvian Observatory of the National Institute of Geophysics and Volcanology and the opinion of the National Commission for the Forecasting and Prevention of Major Risks. Actions to be implemented by the National Civil Protection Service are defined in the operational phases (attention phase, pre-alarm and alarm) provided for in the civil protection plans. The President of the Council of Ministers declares the pre-alarm and the alarm phase.

\n","value":"

The alert system provides specific “alert levels” describing the state of activity of the volcano, based on the parameters of monitoring and any ongoing phenomena. The green alert level corresponds to the ordinary activity of the volcano while the yellow, orange and red alert levels represent increasing stages of unbalance of the volcano towards a possible eruption. The duration of each alert level can be extremely variable.

\r\n\r\n

The alert levels are declared by the Department of Civil Protection, in conjunction with the regional civil protection. A possible change in level is assessed on the basis of the indications provided by the Vesuvian Observatory of the National Institute of Geophysics and Volcanology and the opinion of the National Commission for the Forecasting and Prevention of Major Risks. Actions to be implemented by the National Civil Protection Service are defined in the operational phases (attention phase, pre-alarm and alarm) provided for in the civil protection plans. The President of the Council of Ministers declares the pre-alarm and the alarm phase.

\r\n"},"relationships":{"field_immagine":null,"field_video":null,"field_link_interni":[]},"drupal_internal__id":19617},{"field_titolo":"What does the civil protection plan provide?","field_tabella":null,"field_testo":{"processed":"

For the red zone, the only preventive measure is to remove the population before the eruption begins. People can decide whether to find accommodation outside the risk zones or to benefit from accommodation offered by the State in the Autonomous Region or Province twinned with their Municipality.

\n

For the yellow zone, the removal of the population will be assessed on the basis of the current event, the direction of the winds and the extent of the eruption. The Plan for volcanic risk at the Phlegraean Fields is set at national level, therefore it must be drawn up by the entire National Service of Civil Protection starting from the Civil Protection Department, the Campania Region, the Prefecture of Naples, the Municipalities of the red zone, the Regions and twinned autonomous Provinces.

\n","value":"

For the red zone, the only preventive measure is to remove the population before the eruption begins. People can decide whether to find accommodation outside the risk zones or to benefit from accommodation offered by the State in the Autonomous Region or Province twinned with their Municipality.

\r\n\r\n

For the yellow zone, the removal of the population will be assessed on the basis of the current event, the direction of the winds and the extent of the eruption. The Plan for volcanic risk at the Phlegraean Fields is set at national level, therefore it must be drawn up by the entire National Service of Civil Protection starting from the Civil Protection Department, the Campania Region, the Prefecture of Naples, the Municipalities of the red zone, the Regions and twinned autonomous Provinces.

\r\n"},"relationships":{"field_immagine":null,"field_video":null,"field_link_interni":[{"__typename":"node__approfondimento","title":"The National Emergency Planning for volcanic risk in the Phlegraean Fields ","field_titolo_esteso":"The National Emergency Planning for volcanic risk in the Phlegraean Fields ","body":{"processed":"

Over the past few years, the National Planning for volcanic risk in the Phlegraean Fields has been updated. In particular, by means of the Decree of the President of the Council of Ministers of June 24, 2016, the eruptive scenario, the red zone (exposed to the invasion of pyroclastic flows) and the yellow zone (affected by ash fallout) have been redefined based on studies by the scientific community. This redefinition preceded a phase of mutual sharing and consultation between the Civil Protection Department, the Campania Region, and the affected municipalities.

\n

Planning activities were carried out based on the guidelines issued by the Head of the Civil Protection Department on February 2, 2015, \"Indications to the components and operational structures of the National Service for the updating of emergency plans for the precautionary removal of the population of the red zone of the Vesuvian area,\" which also apply to the Phlegraean Fields area.

\n

In 2019, the national exercise \"Exe Flegrei 2019\" was organized, in which procedures and operational strategy assumed in the national planning were tested. The exercise was also valuable for reshaping some operational decisions related to evacuating the population from the red zone.

\n

(Last update: 3 January 2024)

\n","value":"

Over the past few years, the National Planning for volcanic risk in the Phlegraean Fields has been updated. In particular, by means of the Decree of the President of the Council of Ministers of June 24, 2016, the eruptive scenario, the red zone (exposed to the invasion of pyroclastic flows) and the yellow zone (affected by ash fallout) have been redefined based on studies by the scientific community. This redefinition preceded a phase of mutual sharing and consultation between the Civil Protection Department, the Campania Region, and the affected municipalities.

\r\n\r\n

Planning activities were carried out based on the guidelines issued by the Head of the Civil Protection Department on February 2, 2015, \"Indications to the components and operational structures of the National Service for the updating of emergency plans for the precautionary removal of the population of the red zone of the Vesuvian area,\" which also apply to the Phlegraean Fields area.

\r\n\r\n

In 2019, the national exercise \"Exe Flegrei 2019\" was organized, in which procedures and operational strategy assumed in the national planning were tested. The exercise was also valuable for reshaping some operational decisions related to evacuating the population from the red zone.

\r\n\r\n

(Last update: 3 January 2024)

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The red zone encompasses the area exposed to pyroclastic flows which, due to their high temperatures and speed, represent the most dangerous phenomenon for people.

\n

The red zone includes the municipalities of Pozzuoli, Bacoli, Monte di Procida and Quarto; part of the municipalities of Giugliano in Campania and Marano in Naples; some districts of Naples: Soccavo, Pianura, Bagnoli, Fuorigrotta and part of the districts of San Ferdinando, Posillipo, Chiaia, Arenella, Vomero, Chiaiano and Montecalvario.

\n

The yellow area includes the area exposed to the danger of lapilli and volcanic ash fallout.

\n

The yellow zone includes the municipalities of Villaricca, Calvizzano, Marano di Napoli, Mugnano di Napoli, Melito di Napoli, Casavatore and 24 districts of the Municipality of Naples: Arenella, Avvocata, Barra, Chiaia, Chiaiano, Mercato, Miano, Montecalvario, Pendino, Piscinola, Poggioreale, Porto, San Carlo all’Arena, San Ferdinando, San Giovanni a Teduccio, San Giuseppe, San Lorenzo, San Pietro a Patierno, Scampia, Secondigliano, Stella, Vicaria, Vomero and Zona Industriale.

\n","value":"

The red zone encompasses the area exposed to pyroclastic flows which, due to their high temperatures and speed, represent the most dangerous phenomenon for people.

\r\n\r\n

The red zone includes the municipalities of Pozzuoli, Bacoli, Monte di Procida and Quarto; part of the municipalities of Giugliano in Campania and Marano in Naples; some districts of Naples: Soccavo, Pianura, Bagnoli, Fuorigrotta and part of the districts of San Ferdinando, Posillipo, Chiaia, Arenella, Vomero, Chiaiano and Montecalvario.

\r\n\r\n

The yellow area includes the area exposed to the danger of lapilli and volcanic ash fallout.

\r\n\r\n

The yellow zone includes the municipalities of Villaricca, Calvizzano, Marano di Napoli, Mugnano di Napoli, Melito di Napoli, Casavatore and 24 districts of the Municipality of Naples: Arenella, Avvocata, Barra, Chiaia, Chiaiano, Mercato, Miano, Montecalvario, Pendino, Piscinola, Poggioreale, Porto, San Carlo all’Arena, San Ferdinando, San Giovanni a Teduccio, San Giuseppe, San Lorenzo, San Pietro a Patierno, Scampia, Secondigliano, Stella, Vicaria, Vomero and Zona Industriale.

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In the pre-alarm phase, people wishing to leave the red zone can do it independently, moving to an alternative accommodation (second home, to relatives or friends, rented house) and receiving a financial contribution from the State.

\n

In the alarm phase, the population can decide whether to move by their means, notifying their municipality, following the routes provided by the plan and according to the timetable established, or by means made available by the State. It is possible to decide whether to move to an alternative accommodation chosen independently and receive a financial contribution from the State or benefit from the accommodation offered in the twinned Region or Autonomous Province. Those who decide to leave with the means made available by the State must go to the waiting area identified by the Municipal Civil Protection Plan, either independently or with the shuttles organized by their municipality. From here, the transfer to the meeting area outside the red zone will take place with the buses of the Campania Region, while the transfer to the twinned Region or Autonomous Province will be provided by the means of transport identified by the planning (train, bus, ship). Details regarding the transfer and reception of the population will be defined in the Plans of the individual Regions and Autonomous Provinces.

\n","value":"

In the pre-alarm phase, people wishing to leave the red zone can do it independently, moving to an alternative accommodation (second home, to relatives or friends, rented house) and receiving a financial contribution from the State.

\r\n\r\n

In the alarm phase, the population can decide whether to move by their means, notifying their municipality, following the routes provided by the plan and according to the timetable established, or by means made available by the State. It is possible to decide whether to move to an alternative accommodation chosen independently and receive a financial contribution from the State or benefit from the accommodation offered in the twinned Region or Autonomous Province. Those who decide to leave with the means made available by the State must go to the waiting area identified by the Municipal Civil Protection Plan, either independently or with the shuttles organized by their municipality. From here, the transfer to the meeting area outside the red zone will take place with the buses of the Campania Region, while the transfer to the twinned Region or Autonomous Province will be provided by the means of transport identified by the planning (train, bus, ship). Details regarding the transfer and reception of the population will be defined in the Plans of the individual Regions and Autonomous Provinces.

\r\n"},"relationships":{"field_immagine":{"field_alt":"Piano nazionale di emergenza rischio vulcanico Campi Flegrei - Schema gemellaggi","field_didascalia":" Lo schema dei gemellaggi previsti dal Piano nazionale di emergenza per il rischio vulcanico per i Campi Flegrei","relationships":{"image":{"localFile":{"childImageSharp":{"fluid":{"aspectRatio":1.5027322404371584,"src":"/static/954a0f3c63d76e3ec9b1b63ca5890cff/ee604/piano-nazionale-di-emergenza-rischio-vulcanico-campi-flegrei-gemellaggi.png","srcSet":"/static/954a0f3c63d76e3ec9b1b63ca5890cff/90683/piano-nazionale-di-emergenza-rischio-vulcanico-campi-flegrei-gemellaggi.png 275w,\n/static/954a0f3c63d76e3ec9b1b63ca5890cff/1c1a5/piano-nazionale-di-emergenza-rischio-vulcanico-campi-flegrei-gemellaggi.png 550w,\n/static/954a0f3c63d76e3ec9b1b63ca5890cff/ee604/piano-nazionale-di-emergenza-rischio-vulcanico-campi-flegrei-gemellaggi.png 800w","sizes":"(max-width: 800px) 100vw, 800px"}}}}}},"field_video":null,"field_link_interni":[]},"drupal_internal__id":19620},{"field_titolo":"When will the IT-alert message be sent?","field_tabella":null,"field_testo":{"processed":"

The IT-alert public warning system for the risk of eruption in the is used to give early warning of a potential upcoming eruption in the Phlegraean Fields with the resulting need to take civil protection actions, including the evacuation of the population living in the red zone, provided for in the plans. When the operational phase of \"alarm\" is activated, an IT-alert message is sent to the cell phones of those in the Campania region to inform them of the potential danger. It is, therefore, essential to know what to do right away.

\n","value":"

The IT-alert public warning system for the risk of eruption in the is used to give early warning of a potential upcoming eruption in the Phlegraean Fields with the resulting need to take civil protection actions, including the evacuation of the population living in the red zone, provided for in the plans. When the operational phase of \"alarm\" is activated, an IT-alert message is sent to the cell phones of those in the Campania region to inform them of the potential danger. It is, therefore, essential to know what to do right away.

\r\n"},"relationships":{"field_immagine":null,"field_video":null,"field_link_interni":[]},"drupal_internal__id":19621}],"field_tab":[{"field_titolo":"What to know right away","field_tabella":null,"field_testo":{"processed":"","value":"\r\n"},"relationships":{"field_immagine":null,"field_video":null,"field_link_interni":[]},"drupal_internal__id":21300}],"field_immagine_anteprima":{"field_alt":"Campi Flegrei","field_didascalia":"Campi Flegrei","relationships":{"image":{"localFile":{"childImageSharp":{"fluid":{"aspectRatio":1.7857142857142858,"src":"/static/a13410d7897abb7370c0287c4c6ea2be/42364/primo-piano-campi-freglei.jpg","srcSet":"/static/a13410d7897abb7370c0287c4c6ea2be/cf463/primo-piano-campi-freglei.jpg 275w,\n/static/a13410d7897abb7370c0287c4c6ea2be/dee3b/primo-piano-campi-freglei.jpg 550w,\n/static/a13410d7897abb7370c0287c4c6ea2be/42364/primo-piano-campi-freglei.jpg 1100w,\n/static/a13410d7897abb7370c0287c4c6ea2be/eeda9/primo-piano-campi-freglei.jpg 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