Scaling of peak ground motions from digital recordings of small earthquakes at Campi Flegrei, southern Italy

1988 ◽  
Vol 126 (1) ◽  
pp. 37-53 ◽  
Author(s):  
Giuseppe De Natale ◽  
Ezio Faccioli ◽  
Aldo Zollo
Keyword(s):  
Southern Italy ◽  
Ground Motions ◽  
Campi Flegrei ◽  
Digital Recordings

scholarly journals A three-dimensional QP imaging of the shallowest subsurface of Campi Flegrei offshore caldera, southern Italy

2016 ◽  
Vol 43 (21) ◽  
pp. 11,209-11,218 ◽  
Author(s):  
Vincenzo Serlenga ◽  
Salvatore de Lorenzo ◽  
Guido Russo ◽  
Ortensia Amoroso ◽  
Stephane Garambois ◽  
...  
Keyword(s):  
Southern Italy ◽  
Three Dimensional ◽  
Campi Flegrei

Q c of three component seismograms of volcanic microearthquakes at Campi Flegrei volcanic area — Southern Italy

1985 ◽  
Vol 123 (5) ◽  
pp. 683-696 ◽  
Author(s):  
E. Del Pezzo ◽  
G. De Natale ◽  
G. Scarcella ◽  
A. Zollo
Keyword(s):  
Southern Italy ◽  
Campi Flegrei ◽  
Volcanic Area

scholarly journals Review article: Brief history of volcanic risk in the Neapolitan area (Campania, southern Italy): a critical review

2021 ◽  
Vol 21 (10) ◽  
pp. 3097-3112
Author(s):  
Stefano Carlino
Keyword(s):  
Southern Italy ◽  
Maximum Growth ◽  
Maximum Growth Rate ◽  
Campi Flegrei ◽  
Volcanic Risk ◽  
Campania Region ◽  
Greco Roman ◽  
Systematic Strategy ◽  
History Of ◽  
Very High

Abstract. The presence of three active volcanoes (Vesuvius, Campi Flegrei and Ischia island) along the coast of Naples did not contain the huge expansion of the urbanized zones around them. In contrast, since the Greco-Roman era, volcanoes have featured among the favourite sites for people colonizing the Campania region. The stable settlements around Vesuvius, Campi Flegrei caldera and Ischia were progressively enlarged, attaining a maximum growth rate between 1950 and 1980. Between 1982 and 1984, Neapolitans faced the last and most dramatic volcanic crises, which occurred at Campi Flegrei (Pozzuoli) without an eruption. Since that time, volcanologists have focused their attention on the problem of risks associated with eruptions in the Neapolitan area, but a systematic strategy to reduce the very high volcanic risk of this zone is still lacking. A brief history of volcanic risk in the Neapolitan district is narrated here in an effort to provide new food for thought for the scientific community that works for the mitigation of volcanic risk in this area.

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