Search results for "Mt. Etna"

showing 10 items of 26 documents

Active tectonics along the south east offshore margin of Mt. Etna: New insights from high-resolution seismic profiles

2018

The offshore margin of Mt. Etna has been shaped by Middle Pleistocene to Holocene shortening and extension and, more recently, by gravity-related sliding of the volcanic edifice. These processes have acted contemporaneously although the gravitational component largely prevails over the tectonic one. In order to investigate this issue, we focused on the main role of active tectonics along the south-eastern offshore of Mt. Etna by means of marine high-resolution seismic data. Seismic profiles revealed post-220 ka sedimentary deposits unconformably overlaying the Lower-Middle Pleistocene Etnean clayey substratum and volcanics of the Basal Tholeiitic phase and the Timpe phase. Offshore Aci Trez…

010504 meteorology & atmospheric sciencesPleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturaleactive tectonics010502 geochemistry & geophysics01 natural sciencesSicilian thrust-beltPaleontologyActive tectonicActive tectonics; Ionian Sea; Mt. Etna; Seismic investigation; Sicilian thrust-belt; Earth and Planetary Sciences (all)Seismic investigationHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryContinental shelfMt. Etnalcsh:QE1-996.5Fold (geology)Ionian SeaMt. Etna; seismic investigation; active tectonics; Sicilian thrust-belt; Ionian SeaSeafloor spreadingVolcanic rocklcsh:GeologyTectonicsGeneral Earth and Planetary SciencesSedimentary rockEarth and Planetary Sciences (all)Geology
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The value of by-catch data: how species-specific surveys can serve non-target species

2019

Camera trapping has a wide range of research application, but, while research designs are often focused on the study of a single focal species, cameras can also record other non-target species. Occupancy modeling using by-catch data can be a valuable resource to gain information on these species maximizing the scientific effort and efficiency of wildlife surveys. In this study, we used by-catch data from a European wildcat (Felis silvestris silvestris) survey in Southern Italy to assess the habitat covariates determinant for the occupancy of the crested porcupine (Hystrix cristata). We recorded 33 detections at 17 out of 51 cameras (naive occupancy = 0.33). The best models fitted the data w…

0106 biological sciencesCamera trappingOccupancyRange (biology)biology.animal_breedSettore BIO/05 - ZoologiaWildlifeManagement Monitoring Policy and Law010603 evolutionary biology01 natural sciences010605 ornithologyHystrix cristataCrested porcupineEcology Evolution Behavior and SystematicsNature and Landscape ConservationbiologyMt. EtnaOccupancybiology.organism_classificationBycatchGeographyHabitat useHabitatEuropean wildcatCamera trapCartographyEuropean Journal of Wildlife Research
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A TWO-COMPONENT MANTLE EXTENDING FROM MT. ETNA TO HYBLEAN PLATEAU (EASTERN SICILY) AS INFERRED BY AN INTEGRATED APPROACH WITH NOBLE GASES, TRACE ELEM…

2012

A TWO-COMPONENT MANTLE EXTENDING FROM MT. ETNA TO HYBLEAN PLATEAUSettore GEO/07 - Petrologia E PetrografiaINTEGRATED APPROACH WITH NOBLE GASES TRACE ELEMENTS AND ISOTOPIC GEOCHEMISTRY.
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The contingent equilibrium during imbalanced volcano tourism demand through fee estimation: An empirical analysis of tourism in Mt. Etna

2022

Volcanic sites can be considered strategic areas for conservation and protection policies, but such policies may involve considerable costs However, not only are volcanic sites often integral to the tourism industry and, hence, of potential significant benefit to local economies in general; entrance fee income from tourists can also contribute to management and conservation costs in particular. Nevertheless, seasonal variations in tourism demand, resulting in over-and under-tourism situations, may impact on both the level of income generated as well as on the sustainability of sites Therefore, based on a case study of Mt Etna in Italy, this study considers establishing appropriate entry fee…

Environmental EngineeringItalyVolcanic sites contingent valuation volcano tourism Over-tourism Economic equilibrium Mt. EtnaN832Costs and Cost AnalysisIncomeN831General MedicineManagement Monitoring Policy and LawSettore SECS-P/06 - Economia ApplicataWaste Management and DisposalTourism
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Insights into magma and fluid transfer at Mount Etna by a multiparametric approach: A model of the events leading to the 2011 eruptive cycle

2013

Geophysicsground deformationGeochemistry and PetrologySpace and Planetary ScienceMt. Etnavolcano plumbing systemEarth and Planetary Sciences (miscellaneous)CO2SO2CO2; ground deformation; Mt. Etna; SO2; volcanic tremor; volcano plumbing system; Geophysics; Geochemistry and Petrology; Earth and Planetary Sciences (miscellaneous); Space and Planetary Sciencevolcanic tremorCO2; ground deformation; Mt. Etna; SO2; volcanic tremor; volcano plumbing system; Geochemistry and Petrology; Geophysics; Earth and Planetary Sciences (miscellaneous); Space and Planetary Science
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Degassing vs. eruptive styles at Mt. Etna volcano (Sicily, Italy). Part I: Volatile stocking, gas fluxing, and the shift from low-energy to highly ex…

2018

International audience; Basaltic magmas can transport and release large amounts of volatiles into the atmosphere, especially in subduction zones, where slab-derived fluids enrich the mantle wedge. Depending on magma volatile content, basaltic volcanoes thus display a wide spectrum of eruptive styles, from common Strombolian-type activity to Plinian events. Mt. Etna, in Sicily, is a typical basaltic volcano where the volatile control on such a variable activity can be investigated. Based on a melt inclusion study in products from Strombolian or lava-fountain activity to Plinian eruptions, here we show that for the same initial volatile content, different eruptive styles reflect variable dega…

Melt inclusion010504 meteorology & atmospheric sciencesExplosive materialMantle wedgeGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMicroliteGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyBasaltic explosive volcanism0105 earth and related environmental sciencesMelt inclusionsBasaltgeographygeography.geographical_feature_categorySubductionMt. EtnaTotal volatilesChemical thermodynamicsGeologyTotal volatileStrombolian eruptionChemical thermodynamicVolcano13. Climate actionengineeringMelt inclusionsGeology
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UV camera-based monitoring SO2 flux on Mt. Etna

Mt. Etna eruptionsSO2 fluxUV camera monitoringVolcano degassingSettore GEO/08 - Geochimica E Vulcanologia
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EVIDENCES OF ENRICHED MANTLE (EM-2) SOURCE CONTRIBUTION TO ETNEAN MAGMAS: A COMPREHENSIVE STUDY ON FLUID AND MELT INCLUSIONS OF 2001-2006 ERUPTIONS

2009

Mt. Etna Fluid inclusions noble gases melt inclusions mantle sources
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Etna International Training School of Geochemistry. Science meets Practice

2019

Also this year, the “Etna International Training School of Geochemistry. Science meets practice” took place at Mt. Etna, now in its fourth edition. The school was hosted in the historical Volcanological Observatory “Pizzi Deneri”, one of the most important sites of the INGV - Osservatorio Etneo for geochemical and geophysical monitoring. Mount Etna, located in eastern Sicily, is the largest active volcano in Europe and one of the most intensely degassing volcanoes of the world [Allard et al., 1991; Gerlach, 1991]. Mt Etna emits about 1.6 % of global H2O fluxes from arc volcanism [Aiuppa et al., 2008] and 10 % of global average volcanic emission of CO2 and SO2 [D’Alessandro et al., 1997; Cal…

Mt. Etna Geochemistry Volcanology Remote SensingSettore GEO/08 - Geochimica E Vulcanologia
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Environmental impact of magmatic fluorine emission in the Mt. Etna area

2007

The sustained and uninterrupted plume degassing at Mount Etna volcano, Southern Italy, represents the troposphere's most prominent natural source of fluorine. Of the ∼ 200 Mg of fluorine (as HFg) emitted daily by the volcano, 1.6 ± 2.7 Mg are deposited by wet and dry deposition. Fluorine-deposition via volcanic ash, here characterised for the first time, can be quite significant during volcanic eruptions (i.e. 60 Mg of fluorine were deposited during the 2001 eruption through volcanic ash, corresponding to ∼ 85% of the total fluorine deposition). Despite the fact that these depositions are huge, the fate of the deposited fluorine and its impact on the environment are poorly understood. We he…

Mt. Etna fluorine emission
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