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  • 1
    Publication Date: 2017-04-04
    Description: Published
    Description: 5.3. TTC - Banche dati vulcanologiche
    Description: open
    Keywords: Data base ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: web product
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  • 2
    Publication Date: 2017-04-04
    Description: Gaetano Ponte (1876-1955), docente di vulcanologia presso lʼUniversità di Catania dal 1919 al 1951, rappresenta una figura di notevole spessore nel panorama mondiale degli studi sulle scienze della Terra. Le idee e i risultati delle ricerche da lui condotte sono ben noti attraverso la sua vasta produzione scientifica. È invece meno noto il suo patrimonio fotografico,costituito da oltre 2500 immagini realizzate dalla fine del 1800 fino al 1950. Questa pregevole raccolta di fotografie, che rappresenta un patrimonio unico di documentazione storica dell'attività dei vulcani siciliani,è stata recuperata e valorizzata attraverso una collaborazione fra l'Archivio Fotografico Toscano di Prato e l'Istituto Nazionale di Geofisica e Vulcanologia, che hanno realizzato un catalogo informatico disponibile su internet. In questo libro sono selezionate e presentate le più significative immagini di carattere vulcanologico, geologico e paesaggistico dei vulcani siciliani. Le fotografie di questo libro ricostruiscono un affascinante viaggio attraverso la storia eruttiva dellʼEtna e di Stromboli durante la prima metà del XX secolo e, insieme ai cambiamenti e alle modifiche del paesaggio etneo e siciliano, raccontano il lungo percorso culturale e scientifico della vita di Gaetano Ponte dove arte e scienza si fondono nella fotografia.
    Description: Published
    Description: 5.8. TTC - Biblioteche ed editoria
    Description: open
    Keywords: Gaetano Ponte ; Fotografia storica ; Etna ; Stromboli ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book
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  • 3
    Publication Date: 2017-04-04
    Description: A multidisciplinary approach integrating a wide data set ranging from bulk rock compositions of the erupted products to volcanic tremor, long‐period events, and tilt and gravity signals is used to investigate the source depth and magma dynamics of the 10 May 2008 lava fountain at Southeast crater (SEC) of Mount Etna. The investigation was undertaken in the framework of the previous 2007 explosive activity as well as the subsequent effusive eruption beginning 13 May 2008 and lasting up to July 2009. All the data concur in indicating that the 10 May lava fountain was generated by the fragmentation of a foam layer trapped at the top of a shallow reservoir, about 1500–1700 m below the summit of SEC. The shift from the episodic strombolian/lava fountain activity occurring in 2007 at SEC to the more powerful 10 May 2008 lava fountain is explained by the intrusion of a new more primitive magma into the shallow reservoir. Data also indicate that an attempted magma intrusion east of the summit area occurred during the 10 May fire fountain. This event caused the fracturing and weakening of the surrounding rocks and created a preferential pathway for the penetration of the magma that, only 3 days later, started to feed the 2008–2009 effusive eruption.
    Description: Published
    Description: Q07009
    Description: 2.6. TTC - Laboratorio di gravimetria, magnetismo ed elettromagnetismo in aree attive
    Description: JCR Journal
    Description: reserved
    Keywords: Etna volcano ; lava fountain mechanism ; multidisciplinary monitoring ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2017-04-04
    Description: Elasto-plastic models for pressure sources in heterogeneous domain were constructed to describe, assess, and interpret observed deformation in volcanic regions. We used the Finite Element Method (FEM) to simulate the deformation in a 3D domain partitioned to account for the volcano topography and the heterogeneous material properties distribution. Firstly, we evaluated the extent of a heated zone surrounding the magmatic source calculating the temperature distribution by a thermo-mechanical numerical model. Secondly, we included around the pressurized magma source an elasto-plastic zone, whose dimension is related to the temperature distribution. This elasto-plastic model gave rise to deformation comparable with that obtained from elastic and viscoelastic models, but requiring a geologically satisfactory pressure. We successfully applied the method to review the ground deformation accompanying the 1993–1997 inflation period on Mt Etna. The model considerably reduces the pressure of a magma chamber to a few tens of MPa to produce the observed surface deformation. Results suggest that the approach presented here can lead to more accurate interpretations and inferences in future modeling-based assessments of volcano deformation.
    Description: Published
    Description: 311-318
    Description: 3.6. Fisica del vulcanismo
    Description: JCR Journal
    Description: reserved
    Keywords: ground deformation elasto-plastic rheology finite element method Etna volcano ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 5
    Publication Date: 2017-04-04
    Description: A procedure, based on the Finite Element Method (FEM) for high-resolution geodetic data inversion, was developed to estimate non-uniform slip distribution during the 2002 September 22 M3.7 earthquake rupture occurring only one month before the 2002–2003 eruption of Etna volcano. FEM-generated synthetic Green’s functions are combined with an inverse algorithm to simulate deformation of the earthquake for a 3-D problem domain that takes into account heterogeneity of material properties in the volcanic edifice. The inversion of DInSAR data shows complex kinematics of the northeastern flank of theEtna volcano involving the Pernicana fault system. We detailed the coseismic shear-rupture mechanism and highlighted a tensile mechanism, never observed before, related to a first attempt of magma intrusion, which preceded the following October 26 eruption.
    Description: Published
    Description: 765-773
    Description: 3.6. Fisica del vulcanismo
    Description: JCR Journal
    Description: reserved
    Keywords: Numerical solutions; Radar interferometry; Volcanic hazards and risks. ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2017-04-04
    Description: Accepted for publication in Journal of Geophysical Research. Copyright (2010) American Geophysical Union
    Description: Between 2007 and early 2008, the INGV monitoring networks on Etna volcano recorded a recharging phase that climaxed with a new effusive eruption on 13 May 2008, and lasted about 14 months. A dike-forming intrusion was accompanied by a violent seismic swarm, with more than 230 events recorded in the first six hours, the largest being ML = 3.9. In the meanwhile, marked ground deformation was recorded by the permanent tilt and GPS networks, and sudden changes in the summit area were detected by five continuously recording magnetic stations. Poor weather conditions did not allow direct observation of the eruptive events, but important information was provided by infrared satellite images that detected the start of lava fountains from the eruptive fissure, feeding a lava flow. This flow spread within the Valle del Bove depression, covering 6.4 km on the south-eastern flank of the volcano in a few hours. The seismicity and deformation pattern indicated that the dike-forming intrusion was propagating northwards. It produced a dry fracture field, which generated concern for the possibility that the eruptive fissures could expand downslope towards populated areas. Monitoring and modeling of the multi-disciplinary data, together with the simulations of ash dispersal and lava flows, allowed us both to infer the eruptive mechanisms and provide a correct interpretation of the ongoing phenomena, furnishing useful information for civil defense purposes. We describe how this approach of feedback between monitoring and research provides critical support to risk evaluation.
    Description: In press
    Description: 3.6. Fisica del vulcanismo
    Description: JCR Journal
    Description: open
    Keywords: multi-disciplinary hazard assessment, Etna 2008 eruption ; 04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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