Massimo Pompilio

Massimo Pompilio

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Massimo Pompilio

Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Pisa, 56125, Italy

Research Focus & Metrics

Academic Career Length

43Years (1984-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 March 2009 in Nature
Verified
Journal Article
Closed access
PDF file
TNT. Naish
T. Naish
RPR. Powell
R. Powell
RLR. Levy
R. Levy
Gary WilsonGary Wilson
Gary Wilson
RSR. Scherer
R. Scherer
TWT. Williams
T. Williams

7 July 2004 in Bulletin of Volcanology
Verified
Journal Article
Closed access
PDF file
DADaniele Andronico
Daniele Andronico
SBStefano Branca
Stefano Branca
Sonia CalvariSonia Calvari
Sonia Calvari
MBMike Burton
Mike Burton
TCTommaso Caltabiano
Tommaso Caltabiano
FMFilippo Murè
Filippo Murè

1 August 2011 in Earth and Planetary Science Letters
Verified
Journal Article
Closed access
MKMaren Kahl
Maren Kahl
SCSumit Chakraborty
Sumit Chakraborty
FCFidel Costa
Fidel Costa
MPMassimo Pompilio
Massimo Pompilio


1 January 2013 in Geological Society, London, Memoirs
Verified
Journal Article
Closed access
MRM. Rosi
M. Rosi
MPMarco Pistolesi
Marco Pistolesi
ABA. Bertagnini
A. Bertagnini
PLP. Landi
P. Landi
MPM. Pompilio
M. Pompilio
PRP. L. Rossi
P. L. Rossi
Stromboli, the northernmost island of the Aeolian archipelago, is known for its persistent volcanic activity over the last several centuries and for its cone which, on clear days, is surmounted by a gas plume rising from its summit. The island hosts two settled areas: the village of Stromboli ( c. 500 inhabitants) to the NE and that of Ginostra ( c. 40 inhabitants) to the SW, both situated along the coast. In summer the number of residents grows considerably, reaching c. 5000 people. This paper provides a description of the present activity and reassesses volcanic hazards on the basis of data from a new monitoring system and from studies on the 2002–2003 and 2007 crises. The normal activity, that of mild Strombolian explosions, is occasionally interrupted by violent eruptions of variable scale (paroxysmal events) and lava flows. Volcanic hazards directly generated by eruptive activity consist of ballistic and tephra fallout, pyroclastic flows, lava flows, wildfires and minor lahars, presenting serious problems to the settled areas only occasionally. In addition to hazards directly related to eruptive phenomena, the Sciara del Fuoco depression has been the site of landslides at various scales, sometimes accompanied by the formation of tsunamis.

1 February 1994 in Contributions to Mineralogy and Petrology
Verified
Journal Article
Closed access
PDF file
PAP. Armienti
P. Armienti
MPM. T. Pareschi
M. T. Pareschi
FIF. Innocenti
F. Innocenti
MPM. Pompilio
M. Pompilio