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D.M. Doronzo, Di Vito M.A., Arienzo I., Bini M., Calusi B., Cerminara M., Corradini S., de Vita S., Giaccio B., Gurioli L., Mannella G., Ricciardi G.P., Rucco I., Sparice D., Todesco M., Trasatti E., Zanchetta G., (2022).Earth-Science Reviews, https://doi.org/10.1016/j.earscirev.2022.104072. Abstract Abstract: A full review of the…

Si rende noto che l’INGV ha pubblicato il seguente bando di concorso per la sede di Pisa: Bando di concorso pubblico, per titoli ed esami, per l’assunzione a tempo determinato (12 mesi) di n. 1 unità di personale nel profilo professionale di Collaboratore di Amministrazione – VII livello retributivo presso l’Istituto…

Figure 1:[A] La Réunion island; [B] enlargement of [A]with the indication of key elements for the target ques-tions described in Section3.1.2. Grey lines are mainroads, the blue line is the line of steepest descent, theorange dashed line is the limit of the Enclos Fouquécaldera. CoordinatesareexpressedintheUTM-WGS8440S system. Service Layer Credits, source:…

Brogi F., S. Colucci, J. Matrone, C.P. Montagna, M. de’ Michieli Vitturi, P. Papale (2022).Geoscientific Model Development, 15, 3773–3796, https://doi.org/10.5194/gmd-15-3773-2022, 2022 Abstract Numerical simulations of volcanic processes play a fundamental role in understanding the dynamics of magma storage, ascent, and eruption. The recent extraordinary progress in…

Paolo Papale, Roberto Moretti, Antonio Paonita (2022).Reviews in Mineralogy and Geochemistry, 87, 431-556, https://doi.org/10.2138/rmg.2022.87.10. Abstract Volatiles are the fuel and fundamental control for major processes involving magmas and volcanoes. Magmatic volatiles are not just transported by magmas. They do cause, to a large extent, magma transfer from deep…

Schematic illustration of the phenomenological model for paroxysm initiation. (a) Paroxysm initiation starts with the ascent of a LP magma batch from its storage region. LP magma ascent results in bubble (grey rounded symbols) nucleation, vesiculation and closed-system degassing. Arrival of the LP magma at shallow levels is preceded or…