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http://hdl.handle.net/2122/2262
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| Authors: | Bonaccorso, A.* Bonforte, A.* Guglielmino, F.* Palano, M.* Puglisi, G.* |
| Title: | Composite ground deformation pattern forerunning the 2004–2005 Mount Etna eruption |
| Title of journal: | Journal Geophysical Research |
| Series/Report no.: | /111 (2006) |
| Publisher: | AGU |
| Issue Date: | 2006 |
| DOI: | 10.1029/2005JB004206 |
| Keywords: | NONE |
| Abstract: | After the end of the 2002–2003 eruption, Mount Etna activity was characterized only
by gentle degassing at the summit craters and some earthquake swarms. Suddenly, an
eruption started on 7 September 2004 in complete absence of summit crater volcanic
activity, seismicity or seismic tremor, and ground deformation. This is the first time that
magma poured out passively without preeruptive and coeruptive volcanic and/or
geophysical phenomena. The primary key to understanding this event is represented by the
ground deformation pattern recorded through GPS measurements during the year
before the eruption. The ground deformation shows inflation superimposed by a
predominant eastward movement of the eastern sector at a rate never observed before
in a noneruptive period. The images from satellite radar interferometry confirmed this
pattern. The deformation field clearly shows that the maximum tension in the eastern
sector of the volcano caused the opening of the eruptive fracture which favored the
silent pouring out of already resident magma. |
| Appears in Collections: | Papers Published / Papers in press 04.03.07. Satellite geodesy 04.08.07. Instruments and techniques 04.08.06. Volcano monitoring
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