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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…

Fig. 2. Satellite view of the studied area highlighted the main geographic features described in the text. Orange dots represent stratigraphic sections identified, measured and described around the cone of Montaña Grande (MG); yellow dots are site where samples for paleomagnetic datings have been recovered. The white dashed line indicates…

Read more… La collaborazione avrà durata quinquennale È stato firmato l’8 aprile scorso l’accordo quadro di collaborazione di ricerca tra il Joint Research Centre (JRC, il servizio scientifico interno della Commissione Europea) e l’ecosistema di ricerca pisano, rappresentato dall’Università di Pisa, la Scuola Normale Superiore, la Scuola Superiore Sant’Anna,…