Back to Search Start Over

Volcanic spreading of Vesuvius, a new paradigm for interpreting its volcanic activity.

Authors :
Borgia, A
Tizzani, P
Solaro, G
Manzo, M
Casu, F
Luongo, G
Pepe, A
Berardino, P
Fornaro, G
Sansosti, E
Ricciardi, G
Fusi, N
Di Donna, G
Lanari, R
Borgia, A.
Tizzani,P
Solaro,G
Manzo, M.
Casu, F.
Luongo, G.
Pepe, A.
Berardino, P.
Fornaro, G.
Sansosti, E.
Ricciardi, G. P.
FUSI, NICOLETTA CHIARA
Di Donna, G.
Lanari R.
Borgia, A
Tizzani, P
Solaro, G
Manzo, M
Casu, F
Luongo, G
Pepe, A
Berardino, P
Fornaro, G
Sansosti, E
Ricciardi, G
Fusi, N
Di Donna, G
Lanari, R
Borgia, A.
Tizzani,P
Solaro,G
Manzo, M.
Casu, F.
Luongo, G.
Pepe, A.
Berardino, P.
Fornaro, G.
Sansosti, E.
Ricciardi, G. P.
FUSI, NICOLETTA CHIARA
Di Donna, G.
Lanari R.
Publication Year :
2005

Abstract

We integrate geologic, structural, leveling and Differential SAR Interferometry data to show that Vesuvius began to spread onto its sedimentary substratum about 3,600 years ago. Moreover, we model the detected deformation with a solution of the lubrication approximation of the Navier-Stokes equations to show that spreading may continue for about 7,200 years more. Correlation of volcanic spreading with phases of the eruptive activity suggests that Plinian eruptions, which are thought to pose the major hazard, are less likely to occur in the near future.

Details

Database :
OAIster
Notes :
English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1308891537
Document Type :
Electronic Resource