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Probabilistic hazard map of PDC showing the inundation probability conditioned on the occurrence of a small-scale PDC at the SSVC. Inundation probabilities are expressed in percent. Aravena A., A. Bevilacqua, A. Neri, P. Gabellini, D. Ferrés, D. Escobar, A. Aiuppa, R. Cioni (2023).Journal of Volcanology and Geothermal Research, 438,…

Figure 1. Maps of the study area. a) Map of Antarctica showing the locations of the studied sediment core, ice core tephra archives, and blue ice field. b) Detail of the Edisto Inlet area and location of core TR17-08. Bathymetry and land morphology are from map SS 58–60/2 (Cape Hallett),…

Figure 1. Overview of Matlab Interface for Seismo-Acoustic aRray Analysis (MISARA). (a) Data preparation window for data preparation and formatting. (b) Home window, the main panel for management of all functionalities of MISARA. (c) Data pre-processing modules for data quality control. (d) Signal features modules provide access to data processing,…

Study area with the location of core ANTA02-NW2 collected in 2002 during the XVII PNRA cruise. The detailed map of the study area is shown in the red inset. Map created using [54] with modified bathymetry. Isobaths every 25 m. Salvi G., R. Melis, P. Del Carlo and A.

Pignone M., A. Amato, C. Nostro, E. Casarotti, C. Meletti, M. Quintiliani, V. Lauciani (2022). Frontiers in Earth Science, 10.https://www.frontiersin.org/articles/10.3389/feart.2022.1003867/full Abstract Communicating scientific information about earthquakes is an important and delicate issue in countries like Italy,where seismic risk is high. Furthermore, continuous and scientifically sound communication…

Figure 4. Thin section images at simple Plane Polarized Light (PPL) or Crossed Nicols (NX) of five different sites sampled at Caselle (a, b, c, d, e) and Fornazzo (f) quarries (Fig. 2, Fig. 3). a) ETN35 (NX); b) ETN36 (NX); c and d) ETN37 (NX and PPL,…