Waveform Variation of the Explosion-Quakes as a Function of the Eruptive Activity at Stromboli Volcano

Author(s):  
Antonietta M. Esposito ◽  
Luca D’Auria ◽  
Flora Giudicepietro ◽  
Marcello Martini
1996 ◽  
Vol 39 (2) ◽  
Author(s):  
J. Neuberg ◽  
R. Luckett

A detailed analysis of broadband seismic recordings leads to models of eruption mechanisms for Strombolian activity. The data used comprise signals from arrays of nine three-component seismometers and video recordings of visual eruptive activity with precise time reference. As a major tool particle motion analysis is used to locate the seismo-volcanic sources. Here, a surface correction is employed to account for the effects of the steep slopes of the volcanic edifice. After careful filtering of the data single seismic phases can be separated and linked to corresponding eruptive features.


2010 ◽  
Vol 73 (1) ◽  
pp. 101-112 ◽  
Author(s):  
Sonia Calvari ◽  
Stefano Branca ◽  
Rosa Anna Corsaro ◽  
Emanuela De Beni ◽  
Lucia Miraglia ◽  
...  

2019 ◽  
Vol 11 (15) ◽  
pp. 1813 ◽  
Author(s):  
Flora Giudicepietro ◽  
Sonia Calvari ◽  
Salvatore Alparone ◽  
Francesca Bianco ◽  
Alessandro Bonaccorso ◽  
...  

After a period of mild eruptive activity, Stromboli showed between 2017 and 2018 a reawakening phase, with an increase in the eruptive activity starting in May 2017. The alert level of the volcano was raised from “green” (base) to “yellow” (attention) on 7 December 2017, and a small lava overflowed the crater rim on 15 December 2017. Between July 2017 and August 2018 the monitoring networks recorded nine major explosions, which are a serious hazard for Stromboli because they affect the summit area, crowded by tourists. We studied the 2017–2018 eruptive phase through the analysis of multidisciplinary data comprising thermal video-camera images, seismic, geodetic and geochemical data. We focused on the major explosion mechanism analyzing the well-recorded 1 December 2017 major explosion as a case study. We found that the 2017–2018 eruptive phase is consistent with a greater gas-rich magma supply in the shallow system. Furthermore, through the analysis of the case study major explosion, we identified precursory phases in the strainmeter and seismic data occurring 77 and 38 s before the explosive jet reached the eruptive vent, respectively. On the basis of these short-term precursors, we propose an automatic timely alarm system for major explosions at Stromboli volcano.


2013 ◽  
Vol 37 (1) ◽  
pp. 473-490 ◽  
Author(s):  
M. Rosi ◽  
M. Pistolesi ◽  
A. Bertagnini ◽  
P. Landi ◽  
M. Pompilio ◽  
...  

Geomorphology ◽  
2021 ◽  
pp. 108093
Author(s):  
Federico Di Traglia ◽  
Alessandro Fornaciai ◽  
Daniele Casalbore ◽  
Massimiliano Favalli ◽  
Irene Manzella ◽  
...  

2021 ◽  
Vol 559 ◽  
pp. 116761
Author(s):  
A. Caracciolo ◽  
L. Gurioli ◽  
P. Marianelli ◽  
J. Bernard ◽  
A. Harris

2021 ◽  
Vol 260 ◽  
pp. 112441
Author(s):  
Federico Di Traglia ◽  
Claudio De Luca ◽  
Mariarosaria Manzo ◽  
Teresa Nolesini ◽  
Nicola Casagli ◽  
...  

2011 ◽  
Vol 3 (1) ◽  
pp. 411-430 ◽  
Author(s):  
A. Aiuppa ◽  
M. Burton ◽  
P. Allard ◽  
T. Caltabiano ◽  
G. Giudice ◽  
...  

Abstract. We report on the first detection of CO2 flux precursors of the till now unforecastable larger than normal ("major") explosions that intermittently occur at Stromboli volcano (Italy). Automated survey of the crater plume emissions in the period 2006–2010, during which 12 such explosions happened, demonstrate that these events are systematically preceded by a brief phase of increasing CO2/SO2 weight ratio (up to >40) and CO2 flux (>1300 t/d) with respect to the time-averaged values of 3.7 and ~500 t/d typical for standard Stromboli's activity. These signals are best explained by the accumulation of CO2-rich gas at a discontinuity of the plumbing system (decreasing CO2 emission at the surface), followed by increasing gas leakage prior to the explosion. Our observations thus support the recent model of Allard (2010) for a CO2-rich gas trigger of recurrent major explosions at Stromboli, and demonstrate the possibility to forecast these events in advance from geochemical precursors. These observations and conclusions have clear implications for monitoring strategies at other open-vent basaltic volcanoes worldwide.


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