Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2864
AuthorsCubellis, E.* 
Luongo, G.* 
Marturano, A.* 
TitleSeismic hazard assessment at Mt. Vesuvius: Maximum expected magnitude
Issue Date2007
Series/Report no./ 162 (2007)
DOI10.1016/j.jvolgeores.2007.03.003
URIhttp://hdl.handle.net/2122/2864
KeywordsMt. Vesuvius
seismic hazard
historical seismicity
Subject Classification04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology 
04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk 
AbstractThis paper deals with the problem of seismicity at Mt. Vesuvius with a view to providing an estimation of the maximum expected earthquake. Integrated analysis of both historical and current seismicity as well as the geological conditions of Vesuvius and the surrounding areas show that seismogenetic structures may fall within the crater axis and at the boundaries of the volcanic complex. While activation of the whole seismogenetic volume detected by seismicity in the past 30 years would indicate a total seismic moment of Mo = 7.1E+ 15 Nm for a magnitude M = 4.5, knowledge of the area's geological structure suggests faulting surfaces of about 32 km2 with an associated magnitude of M = 5.4. The areas of maximum expected damage differ according to the orientation of the hypothesized structure. Analysis of geological and geophysical data and the damage associated to the AD 62 earthquake shows that the prevailing directions in the faulting planes are NE–SW in the eastern sector of the volcanic complex, and roughly WNW–ESE in the southern part of the volcano along the coast. Comparison of instrumental seismicity and historical data reveals two significantly different energy levels: a lower earthquake level with Mmax = 4.5, corresponding to current seismicity and that which accompanied volcanic activity in the eruptive period from 1631–1944; an upper level with Mmax = 5.4, represented by the AD 62 earthquake. The two levels correspond to two stress states and different seismogenetic structures.
Appears in Collections:Papers Published / Papers in press

Files in This Item:
File Description SizeFormat 
CubLuonMar_2007.pdf385.26 kBAdobe PDFView/Open    Request a copy
Show full item record

Page view(s)

134
checked on Apr 24, 2017

Download(s)

35
checked on Apr 24, 2017

Google ScholarTM

Check

Altmetric