Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9635
AuthorsLa Rocca, M.* 
Galluzzo, D.* 
TitleSeismic Monitoring of Mt. Vesuvius by Array Methods
Issue DateJul-2014
Series/Report no.4/85 (2014)
DOI10.1785/0220130216
URIhttp://hdl.handle.net/2122/9635
Keywordsseismic array
volcanic seismicity
array methods
Subject Classification04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
AbstractMt. Vesuvius is a worldwide known active volcano located in Southern Italy, east of the city of Napoli. Its last eruption occurred in 1944, ending a continuous open-conduit activity that lasted for more than three centuries. After then the volcano entered into a quiescent phase. Nonetheless, the explosive style of its past activity and its proximity to densely populated areas make Mt. Vesuvius one of the most dangerous volcanoes in the world. For this reason, a comprehensive monitoring program was established, with the goal of early detection of any possible signals of unrest.
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