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  • 1
    Publication Date: 2023-01-30
    Description: Mt. Stromboli is an iconic active volcano, located in the Aeolian Islands archipelago, off the north coast of Sicily (Italy), in the Mediterranean Sea. Its volcanic activity is characterized by mild and frequent explosions, sometimes interrupted by occasional episodes of more vigorous activity, which can be accompanied by lava flows and more energetic eruptions, known as "major" or "paroxysmal" eruptions, according to the energy dissipated during the event. Stromboli produced vulcanian eruptions in 2003, 2007 and July-August 2019, which were well recorded by the INGV monitoring network. In particular the last three events were accompanied by a wide range of phenomena (pyroclastic flows which produced tsunami waves, lava flows, eruptive column several kilometers high) and have been studied through records from borehole strainmeters, which allow us to infer many details of source dynamics. These events are clearly preceded by an inflation phase of the volcanic building characterized by a slow strain buildup, starting several minutes before the paroxysms. These observations could be used in future for civil protection purposes. The recorded eruptions consist of two or more pulses, with oscillations ranging from several seconds, as in 2007, to some minutes, such as in 2019 and lasting from several minutes to one hour after the explosions. Mechanisms involved in the triggering process of the vulcanian explosions include an increase of magma flux ascending from sources located from 2 to 5-7 km depths and morphological complexity in the upper feeding system. A preliminary early-warning algorithm, based on an evaluation of strain rate change, has been defined: it has shown itself capable of ascertain the occurring eruptions minutes before their summit onset.
    Keywords: early-warning algorithm; early-warning system; paroxysmal eruption; Sacks-Evertson_borehole; STRAIN; Strainmeter; Stromboli, Italy; volcanic eruption
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-12-04
    Description: In 2004, the DINEV project started in the Campi Flegrei - Vesuvius volcanic areas (Scarpa et al., 2007). This research program belongs to the Centro Regionale di Competenza AMRA, supported by PON funds, Regione Campania. The project was designed to complement the seismic and geodetic monitoring system of the Osservatorio Vesuviano through the installation of a small network of seven borehole stations, each installed at a depth up to 200m and instrumented with a Sacks-Evertson volumetric strainmeter. Each borehole station is separated by several kilometres from other stations, and the network covers many strategical distances from Campi Flegrei and Vesuvius volcanoes. The network of four borehole strainmeters in the Pozzuoli region permits us to examine subsurface magma movements and pressures associated with magma ascent, storage, and the recharge of shallow magma reservoirs, and with the response of surface faults to these changes. Strainmeters are recognized as the potential best short-and middle-term instruments for eruption forecasting. Their maximum utility is recognized in the measurement of deformation 170 signals with durations of hours to weeks, providing quantitative constraints on the depth of the pressure source in case of inflation or deflation, and the possible detection of ground deformation accompanying small pressure variations due to increased bubble formation, hydrothermal fluid motions, and/or magmatic ascent in prior to inflation episodes. A recent uplift episode was initiated in Campi Flegrei in November 2004, shortly after the installation of the borehole strainmeters. Relevant strainmeter data have been collected and analysed from the instruments installed near Campi Flegrei caldera during the recent unrest episodes. In the period 2004-2005 strain, tilt and GPS data from Campi Flegrei indicate the onset of surface deformation that accompanied a low rate of vertical displacement that continued to 2006, corresponding to an 15 increase of CO2 emission. This strain episode preceded caldera microseismic activity by a few months, as was observed also during a significant inflation episode in 1982. Other transient strain episodes occurred in October 2006, which were accompanied by a swarm of VT (Volcano-Tectonic) and LP (Long Period) events, in 2009, at the time of renewed gas emission activity at Solfatara, and again in March 2010, several minutes before a seismic swarm. The time scale of these transient strain events ranges from some hours to several days, putting tight constraints on the origin of ground uplifts at Campi Flegrei.
    Keywords: strain; Volcano deformation
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-12-04
    Keywords: DATE/TIME; Day of the year; DEPTH, sediment/rock; DINEV_MRUS; Mount Vesuvius, Gulf of Naples, Italy; Sacks-Evertsen dilatometer; SEDIL; strain; Strain, mechanics, counts; Volcano deformation
    Type: Dataset
    Format: text/tab-separated-values, 173092 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-12-04
    Keywords: DATE/TIME; Day of the year; DEPTH, sediment/rock; DINEV_MRUS; Mount Vesuvius, Gulf of Naples, Italy; Sacks-Evertsen dilatometer; SEDIL; strain; Strain, mechanics, counts; Volcano deformation
    Type: Dataset
    Format: text/tab-separated-values, 100794 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-12-04
    Keywords: DATE/TIME; Day of the year; DEPTH, sediment/rock; DINEV_ARCO; Mount Vesuvius, Gulf of Naples, Italy; Sacks-Evertsen dilatometer; SEDIL; strain; Strain, mechanics, counts; Volcano deformation
    Type: Dataset
    Format: text/tab-separated-values, 173170 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2023-12-04
    Keywords: DATE/TIME; Day of the year; DEPTH, sediment/rock; DINEV_ARCO; Mount Vesuvius, Gulf of Naples, Italy; Sacks-Evertsen dilatometer; SEDIL; strain; Strain, mechanics, counts; Volcano deformation
    Type: Dataset
    Format: text/tab-separated-values, 100796 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2023-12-04
    Keywords: DATE/TIME; Day of the year; DEPTH, sediment/rock; DINEV_QUAR; Mount Vesuvius, Gulf of Naples, Italy; Sacks-Evertsen dilatometer; SEDIL; strain; Strain, mechanics, counts; Volcano deformation
    Type: Dataset
    Format: text/tab-separated-values, 172842 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2023-12-04
    Keywords: DATE/TIME; Day of the year; DEPTH, sediment/rock; DINEV_QUAR; Mount Vesuvius, Gulf of Naples, Italy; Sacks-Evertsen dilatometer; SEDIL; strain; Strain, mechanics, counts; Volcano deformation
    Type: Dataset
    Format: text/tab-separated-values, 100798 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2023-12-04
    Keywords: DATE/TIME; Day of the year; DEPTH, sediment/rock; DINEV_QUAR; Mount Vesuvius, Gulf of Naples, Italy; Sacks-Evertsen dilatometer; SEDIL; strain; Strain, mechanics, counts; Volcano deformation
    Type: Dataset
    Format: text/tab-separated-values, 100808 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2023-09-11
    Description: Lava overflows are highly hazardous phenomena that can occur at Stromboli. They can destabilize the crater area and the "Sciara del Fuoco" unstable slope, formed by several sector collapses, which can generate potentially tsunamigenic landslides. In this study, we have identified precursors of the October-November 2022 effusive crisis through seismic and thermal camera measurements. We analyzed the lava overflow on October 9, which was preceded by a crater-rim collapse, and the overflow on November 16. In both cases, seismic precursors anticipating the overflow onset have been observed. The analysis of the seismic and thermal data led to the conclusion that the seismic precursors were caused by an escalating degassing process from the eruptive vent, which climaxed with the overflows. Volcano deformation derived from ground-based InSAR and strainmeter data showed that inflation of the crater area accompanied the escalating degassing process up to the beginning of the lava overflows. The inflation of the crater area was especially evident in the October 9 episode, which also showed a longer seismic precursor compared to the November 16 event (58 and 40 min respectively). These results are important for understanding Stromboli's eruptive mechanisms and open a perspective for early warning of potentially dangerous phenomena.
    Description: This work has been supported by the INGV project Pianeta Dinamico 2023-2025 - ObseRvation, Measurement and modelling of Eruptive processes (ORME), and partially supported by the Progetto Strategico Dipartimentale INGV 2019 “Forecasting eruptive activity at Stromboli volcano: timing, eruptive style, size, intensity and duration” (FIRST, Delibera n. 144/2020; Scientific Responsibility: S.C.). Furthermore, this research has benefited from the support of Convenzione B2 DPC-INGV 2022-2024, Stromboli, Task 1.3 “Development of a unique activity index and estimation of the probability of the transition between ‘ordinary’ and ‘extraordinary’ eruptive activity”, and of the INGV project Reti Multiparametriche, Task A2 “Development of methods for the identification of precursors of Stromboli’s paroxysms and major explosions based on multiparametric data analysis and study of possible early warning techniques”. The data used in this study were provided by the Istituto Nazionale di Geofisica e Vulcanologia (Osservatorio Vesuviano, Osservatorio Etneo) and by the Centro per la Protezione Civile, Università degli Studi di Firenze (GBInSAR data). We would also like to acknowledge the support of the Italian Dipartimento della Protezione Civile (DPC). It should be noted that this paper does not necessarily reflect the official opinion and policies of DPC.
    Description: Published
    Description: 11115
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Stromboli ; Crater collapses ; overflows ; Volcano instability ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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