The I don't take risks campaign currently is based on the Sicilian volcanoes Stromboli and Vulcano, in the Aeolian Islands, and the Vesuvius and the Phlegraean Fields, in the Campania Region.
\r\n","processed":"The I don't take risks campaign currently is based on the Sicilian volcanoes Stromboli and Vulcano, in the Aeolian Islands, and the Vesuvius and the Phlegraean Fields, in the Campania Region.
\n"},"relationships":{"field_sottodominio":{"name":"Io Non Rischio"},"field_immagine_dettaglio":{"field_alt":"Rischio vulcanico","field_didascalia":"Rischio vulcanico","field_titolo_esteso":"Vulcanico_generico_evidenza","relationships":{"image":{"localFile":{"publicURL":"/static/a5a70176a5f1308793ca82998a1ed147/ok-rischio-vulcanico-generico.jpg","childImageSharp":{"fluid":{"aspectRatio":1.5027322404371584,"src":"/static/a5a70176a5f1308793ca82998a1ed147/14b42/ok-rischio-vulcanico-generico.jpg","srcSet":"/static/a5a70176a5f1308793ca82998a1ed147/cf463/ok-rischio-vulcanico-generico.jpg 275w,\n/static/a5a70176a5f1308793ca82998a1ed147/dee3b/ok-rischio-vulcanico-generico.jpg 550w,\n/static/a5a70176a5f1308793ca82998a1ed147/14b42/ok-rischio-vulcanico-generico.jpg 800w","sizes":"(max-width: 800px) 100vw, 800px"}}}}}},"field_immagine_anteprima":null,"field_riferimento_traduzione":{"fields":{"slug":"/preparati/vulcani/"}},"field_accordion":[],"field_box_1_riga_1":[{"__typename":"node__sezione_con_anticipazioni","field_categoria_primaria":"sezione","field_titolo_esteso":"Phlegraean Fields","field_abstract":{"processed":"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.
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 island of Stromboli is part of the Aeolian archipelago. It is a volcano in constant volcanic activity, populated and visited for centuries. Its main morphological feature is the Sciara del Fuoco: a steep slope that descends from the craters down to below sea level, where most of the volcanic erupted material pours out.
\nOrdinary volcanic activity is characterised by explosions every 10-20 minutes, known as 'Strombolian', although more intense and dangerous 'major' and 'paroxysmal' explosions may occur, as well as effusive eruptions. Volcano activity can cause further dangerous phenomena such as landslides, tsunamis, fires and earthquakes.
The island of Stromboli is part of the Aeolian archipelago. It is a volcano in constant volcanic activity, populated and visited for centuries. Its main morphological feature is the Sciara del Fuoco: a steep slope that descends from the craters down to below sea level, where most of the volcanic erupted material pours out.
\r\nOrdinary volcanic activity is characterised by explosions every 10-20 minutes, known as 'Strombolian', although more intense and dangerous 'major' and 'paroxysmal' explosions may occur, as well as effusive eruptions. Volcano activity can cause further dangerous phenomena such as landslides, tsunamis, fires and earthquakes.
Vesuvius lies east of Naples in a densely populated area; for this reason, it is considered one of the highest-risk volcanoes in the world.
\nThe last eruption, on the other hand, was in 1944 and was marked by low-energy effusive and explosive activity. Since then, the volcano has been quiescent, meaning in a rest period, and is characterized by fumarolic activity inside the crater and low seismicity.
Vesuvius lies east of Naples in a densely populated area; for this reason, it is considered one of the highest-risk volcanoes in the world.
\r\nThe last eruption, on the other hand, was in 1944 and was marked by low-energy effusive and explosive activity. Since then, the volcano has been quiescent, meaning in a rest period, and is characterized by fumarolic activity inside the crater and low seismicity.
The island of Vulcano is part of the Aeolian archipelago and represents the emerged part of an active volcano. The last eruption occurred from 1888 to 1890. So far, the volcano has recorded intense gas emission activity, even at high temperatures, from the crater of La Fossa and near Porto di Levante.
\nThe emission of volcanic gases from underground and from fumaroles is the most frequent phenomenon, but phreatic explosions, earthquakes, landslides and tsunamis can also occur.
The island of Vulcano is part of the Aeolian archipelago and represents the emerged part of an active volcano. The last eruption occurred from 1888 to 1890. So far, the volcano has recorded intense gas emission activity, even at high temperatures, from the crater of La Fossa and near Porto di Levante.
\r\nThe emission of volcanic gases from underground and from fumaroles is the most frequent phenomenon, but phreatic explosions, earthquakes, landslides and tsunamis can also occur.