Lipari, la più estesa delle Isole Eolie con poco meno di 38 km2 di superficie, occupa una posizione centrale nell’arcipelago delle Eolie. La forma irregolare allungata in direzione Nord-Sud, è legata ai numerosi centri eruttivi che la costituiscono. I punti più alti sono il Monte Chirica (602 m) e il Monte S.Angelo (594 m) rispettivamente nella parte settentrionale e centrale dell’isola.
\nLe vicende preistoriche dell’isola sono strettamente legate alla sua natura vulcanica. Nel neolitico raggiunse infatti grande importanza e ricchezza grazie all’ossidiana, un vetro vulcanico che si forma per il rapido raffreddamento di rocce effusive di tipo acido, che rappresentava il materiale più tagliente allora conosciuto e che veniva utilizzato per costruire armi e strumenti di uso domestico quotidiano.
\nLipari è un sistema vulcanico attivo e quiescente, come dimostra una debole attività idrotermale nella parte occidentale dell'isola nonché l’occorrenza di eruzioni esplosive/effusive in epoca tardo romana e medievale.
\n"},"fields":{"slug":"/pagina-base/lipari-0/"},"field_link_esterni":[{"title":"Comune di Lipari","uri":"http://www.comunelipari.it/hh/index.php"}],"field_tabella":null,"relationships":{"field_sottodominio":{"name":"Rischi"},"field_riferimento_traduzione":{"fields":{"slug":"/vulcanico/vulcani-italia/lipari/"}},"field_immagine_singola":null,"field_mappa":null,"field_box_social":null,"field_accordion":[{"field_titolo":"Storia eruttiva","field_tabella":null,"field_testo":{"processed":"La morfologia dell’Isola di Lipari è il risultato di una serie di eruzioni effusive ed esplosive che hanno contribuito alla costruzione degli edifici vulcanici, e di processi di erosione che ne hanno rimodellato i rilievi e la linea di costa. Lipari è la parte emersa di una struttura vulcanica che si estende per circa 1000 metri sotto il livello del mare.
\nGli studi geologici di superficie indicano che l’attività vulcanica può essere suddivisa in tre diversi cicli eruttivi, intervallati da periodi di stasi.
\nAll’attività del primo periodo, intorno a 200.000 anni fa, appartengono prodotti sottomarini affioranti prevalentemente lungo la costa occidentale dell'isola.
\nDopo un periodo di inattività, iniziò il secondo ciclo eruttivo tra 130.000 e 125.000 anni fa, caratterizzato dall’attività prevalentemente esplosiva di Monte S.Angelo, con l'emissione di lave e piroclastiti dal vulcano di Monte Chirica (Costa d'Agosto). La fine di tale periodo viene contraddistinta da uno sprofondamento vulcano-tettonico che diede origine ad una caldera situata tra la parte meridionale di Lipari e quella settentrionale di Vulcano.
\nDopo un ulteriore periodo di stasi dell'attività vulcanica, ebbe inizio intorno a 40.000 anni fa il terzo ciclo eruttivo, caratterizzato da forte attività esplosiva seguita dall’emissione di lava degassata, a cui si deve la formazione dei duomi lavici di Monte Guardia e Monte Giardina, nella parte meridionale dell'isola. A seguito di ulteriori alternanze tra periodi di stasi e attività eruttiva, l'intensa attività esplosiva tra 11.000 e 8.000 anni fa, portò alla formazione nell’estremità nord-orientale dell'isola di grandi depositi di pomice, tra loro separati da una colata di ossidiana affiorante lungo il versante di Monte Pilato.
L'attività vulcanica di Lipari si è conclusa, in epoca storica, tra il 500 e il 1230 d.C., con l'emissione delle colate di ossidiana delle Rocche Rosse e della Forgia Vecchia tracimate dal cono di pomici del Monte Pilato.
\n","value":"La morfologia dell’Isola di Lipari è il risultato di una serie di eruzioni effusive ed esplosive che hanno contribuito alla costruzione degli edifici vulcanici, e di processi di erosione che ne hanno rimodellato i rilievi e la linea di costa. Lipari è la parte emersa di una struttura vulcanica che si estende per circa 1000 metri sotto il livello del mare.
\r\n\r\nGli studi geologici di superficie indicano che l’attività vulcanica può essere suddivisa in tre diversi cicli eruttivi, intervallati da periodi di stasi.
\r\nAll’attività del primo periodo, intorno a 200.000 anni fa, appartengono prodotti sottomarini affioranti prevalentemente lungo la costa occidentale dell'isola.
\r\nDopo un periodo di inattività, iniziò il secondo ciclo eruttivo tra 130.000 e 125.000 anni fa, caratterizzato dall’attività prevalentemente esplosiva di Monte S.Angelo, con l'emissione di lave e piroclastiti dal vulcano di Monte Chirica (Costa d'Agosto). La fine di tale periodo viene contraddistinta da uno sprofondamento vulcano-tettonico che diede origine ad una caldera situata tra la parte meridionale di Lipari e quella settentrionale di Vulcano.
\r\nDopo un ulteriore periodo di stasi dell'attività vulcanica, ebbe inizio intorno a 40.000 anni fa il terzo ciclo eruttivo, caratterizzato da forte attività esplosiva seguita dall’emissione di lava degassata, a cui si deve la formazione dei duomi lavici di Monte Guardia e Monte Giardina, nella parte meridionale dell'isola. A seguito di ulteriori alternanze tra periodi di stasi e attività eruttiva, l'intensa attività esplosiva tra 11.000 e 8.000 anni fa, portò alla formazione nell’estremità nord-orientale dell'isola di grandi depositi di pomice, tra loro separati da una colata di ossidiana affiorante lungo il versante di Monte Pilato.
\r\n
\r\nL'attività vulcanica di Lipari si è conclusa, in epoca storica, tra il 500 e il 1230 d.C., con l'emissione delle colate di ossidiana delle Rocche Rosse e della Forgia Vecchia tracimate dal cono di pomici del Monte Pilato.
Da un periodo incerto compreso tra il VII e il XIII secolo d.C. Lipari si trova in una condizione di quiescenza con manifestazioni vulcaniche unicamente rappresentate da fumarole e sorgenti termali che raggiungono temperature superiori ai 50°.
\nUna tipologia di rischio indirettamente connesso all’attività vulcanica è rappresentato dai movimenti franosi. Alcuni versanti, infatti, anche in condizioni ordinarie, risultano instabili a causa dell’elevata pendenza dei versanti.
\nOltre al pericolo indotto dall’improvviso scivolamento di masse rocciose, un pericolo aggiuntivo può essere la formazione di onde di maremoto dovute all’ingresso in mare di frane di grandi dimensioni.
\n","value":"Da un periodo incerto compreso tra il VII e il XIII secolo d.C. Lipari si trova in una condizione di quiescenza con manifestazioni vulcaniche unicamente rappresentate da fumarole e sorgenti termali che raggiungono temperature superiori ai 50°.
\r\n
\r\nUna tipologia di rischio indirettamente connesso all’attività vulcanica è rappresentato dai movimenti franosi. Alcuni versanti, infatti, anche in condizioni ordinarie, risultano instabili a causa dell’elevata pendenza dei versanti.
\r\n
\r\nOltre al pericolo indotto dall’improvviso scivolamento di masse rocciose, un pericolo aggiuntivo può essere la formazione di onde di maremoto dovute all’ingresso in mare di frane di grandi dimensioni.
Le strutture preposte al monitoraggio dell’attività vulcanica sull’isola di Lipari sono la Sezione di Catania e quella di Palermo dell'Istituto Nazionale di Geofisica e Vulcanologia (Ingv).
\nLa rete si compone di sistemi di monitoraggio della sismicità e delle deformazioni del suolo. Vengono inoltre effettuate misure e campionamenti periodici di acque e gas.
Le strutture preposte al monitoraggio dell’attività vulcanica sull’isola di Lipari sono la Sezione di Catania e quella di Palermo dell'Istituto Nazionale di Geofisica e Vulcanologia (Ingv).
\r\nLa rete si compone di sistemi di monitoraggio della sismicità e delle deformazioni del suolo. Vengono inoltre effettuate misure e campionamenti periodici di acque e gas.
Nelle prime ore del mattino del 3 novembre 2002, di fronte alla costa orientale dell’isola, i pescatori locali avvertirono un forte odore di zolfo e avvistarono il mare in ribollimento, con pesci morti in superficie e cambiamento di colore dell'acqua.
\nIl fenomeno avveniva in tre punti di fronte all'isola.
\nUna zona era a Ovest di Lisca Bianca in direzione di Dattilo, dove il gas arrivava in superficie sotto forma di bolle di qualche metro di diametro.
\nIn una seconda area, a Ovest di Bottaro, l'emissione di gas era ancora più intensa e avveniva da una profondità intorno ai 20 m.
La terza zona occupava una superficie più piccola, tra Bottaro e Lisca Nera. Intorno alle fumarole, l'acqua aveva una temperatura intorno ai 22-23°C, non diversa da quella misurata presso il molo dell'isola, mentre l’acidità era maggiore rispetto a quella comunemente osservata nelle acque marine.
\nL'emissione di gas fu così intensa che l'odore di acido solfidrico era percepibile a grandi distanze. Tuttavia, nel corso di pochi giorni l'attività si ridusse notevolmente, continuando con intensità minore fino al gennaio del 2003.
:
\n","value":"Nelle prime ore del mattino del 3 novembre 2002, di fronte alla costa orientale dell’isola, i pescatori locali avvertirono un forte odore di zolfo e avvistarono il mare in ribollimento, con pesci morti in superficie e cambiamento di colore dell'acqua.
\r\nIl fenomeno avveniva in tre punti di fronte all'isola.
\r\nUna zona era a Ovest di Lisca Bianca in direzione di Dattilo, dove il gas arrivava in superficie sotto forma di bolle di qualche metro di diametro.
\r\nIn una seconda area, a Ovest di Bottaro, l'emissione di gas era ancora più intensa e avveniva da una profondità intorno ai 20 m.
La terza zona occupava una superficie più piccola, tra Bottaro e Lisca Nera. Intorno alle fumarole, l'acqua aveva una temperatura intorno ai 22-23°C, non diversa da quella misurata presso il molo dell'isola, mentre l’acidità era maggiore rispetto a quella comunemente osservata nelle acque marine.
\r\nL'emissione di gas fu così intensa che l'odore di acido solfidrico era percepibile a grandi distanze. Tuttavia, nel corso di pochi giorni l'attività si ridusse notevolmente, continuando con intensità minore fino al gennaio del 2003.
:
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