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(a) Geological sketch map of the Campanian Plain (modified from: Bigi et al., 1990; Cassano & La Torre, 1987; Finetti & Morelli, 1974; La Torre et al., 1983). (b) DTM model of the Somma-Vesuvius volcano with the delimitation of the mapped area (white line).
Volcanology of the Southwestern sector of Vesuvius volcano, Italy
Summary of the models used in the exercise
Results of the eruptive column model inter-comparison study
A. Aerial view showing Shinmoe-dake volcano peak erupting between Miyazaki and Kagoshima prefectures on January 27, 2011 (REUTERS/Kyodo) B. The June 12, 1991 eruption column from Mount Pinatubo taken from the east side of Clark Air Base. U.S. Geological Survey Photograph taken by Richard P. Hoblitt.
Uncertainty quantification and sensitivity analysis of volcanic columns models: Results from the integral model PLUME-MoM
Time domain distribution of Reworked Coccoliths
Reworked Coccoliths as runoff proxy for the last 400 years: The case of Gaeta Gulf (central Tyrrhenian Sea, Central Italy)
Nature, Queisser et al. 2016 - fig. 01
A new frontier in CO2 flux measurements using a highly portable DIAL laser system
Il contributo dei ricercatori della Sezione INGV di Pisa nella gestione dell’emergenza sismica di Amatrice
Fig. 7 - a Modeled Deposited masses (DMi ) expressed as percentages of the emitted mass (EMi ) for each simulated grain-size.
Reconstructing eruptive source parameters from tephra deposit: a numerical study of medium-sized explosive eruptions at Etna volcano
Fig. 5 - Sensitivity analysis results
Insights into the formation and dynamics of coignimbrite plumes from one-dimensional models
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