Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9024
Authors: Bonaccorso, A.* 
Currenti, G.* 
Linde, A.* 
Sacks, S.* 
Title: New data from borehole strainmeters to infer lava fountain sources (Etna 2011-2012)
Issue Date: 2013
Series/Report no.: /40 (2013)
DOI: 10.1002/grl.50692
URI: http://hdl.handle.net/2122/9024
Keywords: Etna volcano
lava fountain eruptions
shallow plumbing system
borehole strainmeters
Subject Classification05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions 
Abstract: In January 2011 eruptive activity resumed at Etna producing a new phase with frequent lava fountain episodes until April 2012. In November 2011, the first two borehole strainmeters were installed, which detected negative strain changes (~ 0.15 - 0.8 strain) during the paroxysmal events. A Finite Element Model was set up to estimate accurately the tilt and volumetric strain, taking into account the real profile of the volcano and the elastic medium heterogeneity. The numerical computations indicated an elongated depressurizing source located at 0 km b.s.l., which underwent a volume change of ~2 x 106 m3 which is the most of the magma volume erupted while a smaller remaining part is accommodated by the magma compressibility. This shallow source cannot accumulate large magma volumes and, thus, favours short term periodic eruptive events with a fairly constant balance between the refilling and the erupted magma.
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