Computed evolution of composition for the buoyant simulation cases. The figures show a zoom view of the shallow chamber and upper portion of the feeding dyke. Longo A., D. Garg, P. Papale, C. P. Montagna (2023).Journal of Geophysical Research – Solid Earth, 128/1.https://doi.org/10.1029/2022JB025316 Active magma chambers…
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Real-time probabilistic assessment of volcanic hazard for tephra dispersal and fallout at Mt. Etna: the 2021 lava fountain episodes
Ground hazard maps produced for the 28 February 2021 lava fountain episode. The left plots of panel (a) and (b) show the probability to exceed a ground load of 0.5 kg m2, while the right plots present the probability to exceed 5 kg m2. Contour lines highlight the places of…
Data analysis of the unsteadily accelerating GPS and seismic records at Campi Flegrei caldera from 2000 to 2020
Bevilacqua A., P. De Martino, F. Giudicepietro, P. Ricciolino, A. Patra, E.B. Pitman, M. Bursik, B. Voight, F. Flandoli, G. Macedonio, A. Neri (2022).Nature – Scientific reports, 12, https://doi.org/10.1038/s41598-022-23628-5 Abstract Ongoing resurgence affects Campi Flegrei caldera (Italy) via bradyseism, i.e. a series of ground deformation episodes accompanied…
Shallow portion of an active geothermal system revealed by multidisciplinary studies: the case of Le Biancane (Larderello, Italy)
Figure 1.a) Geologic sketch map of the Larderello-Travale Geothermal Field (modified after Liotta and Brogi, 2020). The red dot in the inset is the location of the LTGF; b) Geological sketch section (A-A’ in Fig. 1a; modified after Arias et al., 2010 and Liotta and Brogi, 2020). c) Sketch showing the surface manifestation and the general movement…
Volcanic Tremor Tracks Changes in Multi-Vent Activity at Mt. Etna, Italy: Evidence From Analyses of Seismic Array Data
(a) 10-min RMS of seismic volcanic tremor between 16 July 2021 and 24 August 2021 at station ACPN1 (HHZ, vertical component; see Figure 1b for details on station location); (b) spectrogram between 16 July 2021 and 24 August 2021 at station ACPN1 (HHZ, vertical component) and dominant frequency (white line);…
Come cambia la probabilità di terremoti dopo le eruzioni laterali dell’Etna?
di Andrea Bevilacqua, Raffaele Azzaro, Stefano Branca, Salvatore D’Amico, Franco Flandoli, Augusto Neri. Storicamente le eruzioni laterali dell’Etna, quelle che producono colate di lava da fessure situate lungo i fianchi del vulcano, sono spesso accompagnate da eventi sismici distruttivi nell’area Etnea. L’impatto concomitante dei due fenomeni sul territorio può essere…
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