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Figure 2 Workflow summarizing the main steps for mapping the burnt areas through satellite data and validating such areas through drone imageryacquired a few days after the 3rd of July 2019 paroxysm Iacono F., · M. Bisson, · C. Spinetti, · T. Kwasnitschka, (2025).Remote Sensing in Earth Systems Sciences. https://doi.org/10.1007/s41976-025-00215-6…

Figure 2. Images of sampling sites. (a): PAL03 site, overview of the contact (the dashed white line) between the Malforada–Nambroque lava flow and the younger AD 1949 flow. (b): PAL08 site, view of Montaña Quemada lava flow with its massive core. (c): PAL10 site, photograph of a Martín flow outcrop.

Fig. 2. Lithostratigraphic logs of volcaniclastic sequences presented in this work including that of Passo delle Croci (Pizzo Sopra La Fossa Fm., modified from Francalanci et al., 2014) and of Trench 1 (Lower Sequence, modified from Rosi et al., 2000); depth is reported in cm. Colours for labelling…

Sarti C., A. Cascella, C. Conti, S. Cresta, G. Agostinelli (2025).Journal of Iberian Geology, https://doi.org/10.1007/s41513-025-00287-9 Abstract The Upper Jurassic aspidoceratoid genus Hybopeltoceras Olóriz is very scarcely recorded, and distributed only in the Cordillera Betica (Spain), Southern Alps (Italy) and in the Central Apennines (Italy). From rocks of the Lower Tithonian, with particular…

Giudicepietro F., R. Avino, E. Bellucci Sessa, A. Bevilacqua, et al., (2025). Nature Communications, 16, 1548. https://doi.org/10.1038/s41467-025-56723-y Abstract Since early 2021, peculiar Volcano-Tectonic (VT) seismic sequences with very short inter-event times have become increasingly frequent and evident in the Campi Flegrei caldera (Italy), which has been…

Figure 12 a) Infrasound array locations and b) spectrogram of the infrasound record at the Monte Conca site; c) location of the CONC array with respect to the summit of Mt. Etna and directions (red dotted lines) to the different summit craters. Zuccarello L., S. De Angelis M. Sciotto, S.