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),…
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MISARA: Matlab Interface for Seismo-Acoustic aRray Analysis
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,…
Ostracod and Foraminifer Responses to Late Pleistocene-Holocene Volcanic Activity in Northern Victoria Land as Recorded in Ross Sea (Antarctica) Marine Sediments
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.
Public earthquake communication in Italy through a multi-source social media platform: the INGVterremoti experience (2010-2022)
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…
Age of the Valle del Bove formation and chronology of the post-collapse flank eruptions, Etna volcano (Italy)
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,…
Dynamics of Magma Chamber Replenishment Under Buoyancy and Pressure Forces
Computed evolution of composition for the buoyant simulation cases. The figures show a zoom view of the shallow chamber and upper portion of the feeding dyke. Longo A., D. Garg, P. Papale, C. P. Montagna (2023).Journal of Geophysical Research – Solid Earth, 128/1.https://doi.org/10.1029/2022JB025316 Active magma chambers…
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