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showing 10 items of 6771 documents

Major-ion bulk deposition around an active volcano (Mt. Etna, Italy)

2005

Bulk atmospheric deposition of major cations (Na, K, Ca, Mg) and anions (Cl, F, SO4) were measured at 15 sites around an active volcano, Mount Etna, from 2001 to 2003. Their composition indicates several natural sources, among which deposition of plume-derived volcanogenic gas compounds is prevalent for F, Cl and S. Plume-derived acidic compounds are also responsible for the prevailing acidic composition of the samples collected on the summit of the volcano (pH in the 2.45–5.57 range). Cation species have complex origin, including deposition of plume volcanogenic ash and aerosols and soil-dust wind re-suspension of either volcanic or carbonate sedimentary rocks. Variation of the deposition …

geographygeography.geographical_feature_categoryLateral eruptionMineralogyPlumechemistry.chemical_compoundDeposition (aerosol physics)VolcanochemistryImpact craterGeochemistry and PetrologyPanacheCarbonateEtnaSedimentary rockGeology
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Reconstruction of the Holocene palaeoenvironmental conditions accordingly to the multiproxy sedimentary records from Lake Pilvelis, Latvia

2015

Abstract Reconstruction of the Holocene palaeoenvironment conditions in Southeastern Latvia is based on multiproxy records from Lake Pilvelis: pollen, plant macrofossil and microfossil analysis; loss-on-ignition (LOI) measurements; 14 C dating; humic substances content; humification index; and elemental composition of gyttja organic mass. The data complex obtained in the result of multiproxy studies of sediments in Lake Pilvelis indicates significant changes in the depositional environment during the lake development. Data from Lake Pilvelis show that the start of organic-rich sediments formation before approximately 9750 cal BP, when birch–pine forest dominated in the surrounding landscape…

geographygeography.geographical_feature_categoryMacrofossilmedicine.disease_causeWater levelSedimentary depositional environmentPaleontologyPollenmedicineSedimentary rockPhysical geographyBogHoloceneGeologyEarth-Surface ProcessesGyttjaQuaternary International
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Chemical and isotopic characterization of the gases of Mount Etna (Italy)

1997

Abstract In the period 1990–1995, 43 samples of dissolved gases in groundwaters (wells, springs and drainage galleries) and 64 samples of free gases (fumaroles, bubbling and soil gases) from the Mount Etna area were collected and analysed. Isotopic analyses were also carried out of both the carbon of the CO 2 in free gases and dissolved inorganic carbon (DIC) in the waters. The chemical composition of the gases depends on the relative abundances of three interacting components. These are gases of (1) atmospheric origin enriched in O 2 and N 2 , present almost exclusively in dissolved gases, (2) deep origin enriched in CO 2 , prevalent in the majority of cases, and (3) more superficial origi…

geographygeography.geographical_feature_categoryMineralogychemistry.chemical_elementNitrogenFumarolechemistry.chemical_compoundGeophysicsVolcanochemistryGeochemistry and PetrologyEnvironmental chemistryIsotope geochemistryDissolved organic carbonCarbon dioxideChemical compositionGroundwaterGeologyJournal of Volcanology and Geothermal Research
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Rapid oxidation of mercury (Hg) at volcanic vents: Insights from high temperature thermodynamic models of Mt Etna's emissions

2011

A major uncertainty regarding the environmental impacts of volcanic Hg is the extent to which Hg is deposited locally or transported globally. An important control on dispersion and deposition is the oxidation state of Hg compounds: Hg(0) is an inert, insoluble gas, while Hg(II) occurs as reactive gases or in particles, which deposit rapidly and proximally, near the volcanic vent. Using a new high temperature thermodynamic model, we show that although Hg in Etna's magmatic gases is almost entirely Hg(0) (i.e., gaseous elemental mercury), significant quantities of Hg(II) are likely formed at Etna's vents as gaseous HgCl2, when magmatic gases are cooled and oxidised by atmospheric gases. Thes…

geographygeography.geographical_feature_categoryModel studyGeochemistrychemistry.chemical_elementGeologyElemental mercurySettore GEO/08 - Geochimica E VulcanologiaMercury (element)Thermodynamic modelEtna Mercury Hg Volcano DepositionAtmosphere of EarthVolcanochemistryImpact craterGeochemistry and PetrologyOxidation stateEnvironmental chemistryGeologyChemical Geology
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Innovación y TIC en el paisaje sonoro de la música festera a través de la creación de musicomovigramas

2019

Este artículo es parte de un proyecto de investigación sobre el paisaje sonoro, la escucha y la creación y recreación de espacios de educación ambiental y musical. Consiste en una propuesta de creación y utilización de un recurso auditivo-didáctico e interactivo, el musicomovigrama o musicograma en movimiento, para trabajar la escucha y el desarrollo emocional mediante la Fiesta y la música de Moros y Cristianos de Alcoy y su paisaje sonoro. La gran potencialidad de este recurso deriva de su capacidad para ofrecer al alumnado un soporte visual atractivo sincronizado con la progresión de la música que escucha, de tal manera que ambos códigos avancen simultáneamente. El objetivo principal es …

geographygeography.geographical_feature_categoryMovement (music)media_common.quotation_subjectBandes (Música)General MedicineViolin musical stylesExpression (architecture)AestheticsPerceptionNatural (music)Active listeningSociologyComposition (language)Sound (geography)media_commonMúsica Ensenyament
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Volcanic SiO2-cristobalite: A natural product of chemical vapor deposition

2020

Abstract Cristobalite is a low-pressure, high-temperature SiO2 polymorph that occurs as a metastable phase in many geologic settings, including as crystals deposited from vapor within the pores of volcanic rocks. Such vapor-phase cristobalite (VPC) has been inferred to result from silica redistribution by acidic volcanic gases but a precise mechanism for its formation has not been established. We address this by investigating the composition and structure of VPC deposited on plagioclase substrates within a rhyolite lava flow, at the micrometer to nanometer scale. The VPC contains impurities of the form [AlO4/Na+]0—coupled substitution of Al3+ charge-balanced by interstitial Na+—which are ty…

geographygeography.geographical_feature_categoryNatural productMaterials scienceChemical substance010504 meteorology & atmospheric sciencesChemical vapor deposition010502 geochemistry & geophysics01 natural sciencesCristobalitechemistry.chemical_compoundGeophysicsVolcanoChemical engineeringchemistryGeochemistry and PetrologyRhyoliteGlass corrosion0105 earth and related environmental sciencesAmerican Mineralogist
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Minor and trace elements in olivines as probes into early igneous and mantle melting processes

2013

Abstract The trace element composition of olivine is a rapidly growing research area that has several applications of great potential. Mantle olivines can be distinguished from volcanic olivines by lower concentrations of Ca (

geographygeography.geographical_feature_categoryOlivine010504 meteorology & atmospheric sciencesContinental crustMantle metasomatismGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Igneous rockGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyOceanic crustEarth and Planetary Sciences (miscellaneous)Trace element compositionengineeringGeology0105 earth and related environmental sciences
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Vertical movements in NE Sicily and its offshore: Outcome of tectonic uplift during the last 125 ky

2013

New data in the coastal area between Acquedolci and Patti (northeastern Sicily, Italy) have been collected to calculate vertical tectonic rates in a key sector between the Kabilian-Calabrian and the Sicilian-Maghrebian chain. The comparison among marine geology data (multibeam and seismic reflection profiles) on the continental shelf-slope system and the radiocarbon ages on geomorphological markers collected during a coastal survey, provided new stratigraphic, geomorphological and biological data, contributing to the knowledge of the geological evolution of this sector for the last 125 ky.This coastal area is framed between two main structural features active during the Pleistocene in north…

geographygeography.geographical_feature_categoryPleistoceneHoloceneLast Glacial MaximumSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E GeomorfologiaMarine geologyLast Glacial MaximumFault (geology)Last Interglaciallaw.inventionTectonicsTectonic upliftlawRelative Sea level changeUplift rateLate Quaternary depositional sequenceRadiocarbon datingGeomorphologyGeologyHoloceneEarth-Surface Processes
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Ash resuspension related to the 2011–2012 Cordón Caulle eruption, Chile, in a rural community of Patagonia, Argentina

2017

Abstract The 2011–2012 Cordon Caulle eruption emitted about 1 km3 of rhyodacitic tephra. Dominant westerly winds in the region caused most of the primary tephra to deposit in neighboring Argentina. In addition to the impact of widespread dispersal and fallout of primary tephra during the eruption, Argentina was also significantly affected by remobilization of the primary ash even several years after the climactic phase of the eruption. In this mixed methods study, we combine aspects of natural and social sciences to characterize the ash resuspension events associated with the 2011–2012 Cordon Caulle deposits and assess the impacts on the Argentinian farming community of Ingeniero Jacobacci …

geographygeography.geographical_feature_categorySeasonal distribution010504 meteorology & atmospheric sciencesRural communitySteppeWesterlies010502 geochemistry & geophysics01 natural sciencesDeposition (geology)GeophysicsVolcano13. Climate actionGeochemistry and Petrologyddc:550Biological dispersalPhysical geographyTephraGeomorphologyGeology0105 earth and related environmental sciences
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The “Camporeale wedge-top Basin” (NW Sicily; Italy) in the frame of the Late Miocene Sicilian Foreland Basin System; Inferences from the Upper Torton…

2011

Abstract Since the latest Oligocene–earliest Miocene the building of the Sicilian fold and thrust belt has been accompanied by development of a “peripheral” foreland basin system which migrated toward the foreland. In north-western Sicily, the sedimentary record of the foreland basin system migration is represented by a stratigraphic succession made up of several lithostratigraphic units, bounded by regional unconformity surfaces, deposited recording at least four main sedimentary phases, each characterized by the development of different types of syntectonic basins. In particular, during the Late Miocene (Late Tortonian to Early Messinian) a wide wedge-top depozone developed in the innermo…

geographygeography.geographical_feature_categorySedimentary basinStructural basinLate MioceneUnconformitySedimentary depositional environmentPaleontologyGeophysicsFold and thrust beltSedimentary rockForeland basinGeologyEarth-Surface ProcessesJournal of Geodynamics
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