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L’Istituto Nazionale di Ottica (INO) del Consiglio Nazionale delle Ricerche, capofila del progetto ORMA “Alta fORMAzione e ricerca-azione presso enti di ricerca toscani”, ha indetto una selezione per il conferimento di 11 borse di studio di Alta Formazione da fruirsi presso: Consiglio Nazionale delle Ricerche (Area di Firenze e Area…

Trellis plot of the median values of the GMMs pre-selected for ASCRs Lanzano G., L. Luzi, V. D’Amico, F. Pacor, C. Meletti, W. Marzocchi, R. Rotondi, E. Varini (2020).Bulletin of Earthquake Engineering, doi: 10.1007/s10518-020-00850-y. Abstract The aim of this paper is to identify the ground motion models (GMMs),…

Figure 2. Volcán de Colima—comparison between max flow height maps of simulated flow, assuming MC (a,d), PF (b,e), and VS (c,f) models. Extreme cases—(a–c) max. volume–min. resistance and (d–f) min. volume–max. resistance. Patra A.K., A. Bevilacqua, A. Akhavan-Safaei, E.B. Pitman, M.I. Bursik, and D. Hyman (2020).Frontiers in Earth Science, doi:…

Aravena A., R. Cioni, A. Bevilacqua, M. de’ Michieli Vitturi, T. Esposti Ongaro and A. Neri (2020).Journal of Geophysical Research: Solid Earth, doi: 10.1029/2019JB019271. Abstract Kinetic energy models, also called kinetic models, are simple tools able to provide a fast estimate of the inundation area of…

Del Carlo P., A. Smedile, M. Petrelli, A. Di Roberto (2020).Journal of Volcanology and Geothermal Research, https://doi.org/10.1016/j.jvolgeores.2020.106992. Abstract We report on the geochemical and chronological characterization of a tephra layer, here called RdV-T1, recovered within a continental sequence at Riparo di Venere site in the Fucino…

Fig. 1. Simplified map of Tenerife (from a DEM-shaded relief image courtesy of Instituto Geográfico Nacional – IGN) showing the studied lava flows and the sites of palaeomagnetic sampling. Reported flow ages are according to Carracedo et al. (2007). For each site is implied TEN. Black circles reproduce palaeomagnetic…