Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6286
AuthorsAiuppa, A.*
Cannata, A.* 
Cannavò, F.* 
Di Grazia, G.* 
Ferrari, F.* 
Giudice, G.* 
Gurrieri, S.* 
Liuzzo, M.* 
Mattia, M.* 
Montalto, P.* 
Patanè, D.* 
Puglisi, G.* 
TitlePatterns in the recent 2007–2008 activity of Mount Etna volcano investigated by integrated geophysical and geochemical observations
Issue Date2010
Series/Report no./11 (2010)
DOI10.1029/2010GC003168
URIhttp://hdl.handle.net/2122/6286
Keywordsvolcano monitoring
Mt. Etna volcano
geochemistry and geophysics
volcanic tremor
Subject Classification04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
04. Solid Earth::04.08. Volcanology::04.08.01. Gases 
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring 
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques 
AbstractSeismic, deformation, and volcanic gas observations offer independent and complementary information on the activity state and dynamics of quiescent and eruptive volcanoes and thus all contribute to volcanic risk assessment. In spite of their wide use, there have been only a few efforts to systematically integrate and compare the results of these different monitoring techniques. Here we combine seismic (volcanic tremor and long‐period seismicity), deformation (GPS), and geochemical (volcanic gas plume CO2/SO2 ratios) measurements in an attempt to interpret trends in the recent (2007–2008) activity of Etna volcano. We show that each eruptive episode occurring at the Southeast Crater (SEC) was preceded by a cyclic phase of increase‐decrease of plume CO2/SO2 ratios and by inflation of the volcano’s summit captured by the GPS network. These observations are interpreted as reflecting the persistent supply of CO2‐rich gas bubbles (and eventually more primitive magmas) to a shallow (depth of 1–2.8 km asl) magma storage zone below the volcano’s central craters (CCs). Overpressuring of the resident magma stored in the upper CCs’ conduit triggers further magma ascent and finally eruption at SEC, a process which we capture as an abrupt increase in tremor amplitude, an upward (>2800 m asl) and eastward migration of the source location of seismic tremor, and a rapid contraction of the volcano’s summit. Resumption of volcanic activity at SEC was also systematically anticipated by declining plume CO2/SO2 ratios, consistent with magma degassing being diverted from the central conduit area (toward SEC).
DescriptionAn edited version of this paper was published by AGU. Copyright (2010) American Geophysical Union
Appears in Collections:Papers Published / Papers in press

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