Search results for "Vesuvius"

showing 7 items of 7 documents

Crustal dynamics of Mount Vesuvius from 1998 to 2005: Effects on seismicity and fluid circulation

2008

[1] This paper presents the results of hydrogeochemical and seismological studies carried out at Mount Vesuvius during the period June 1998 to December 2005. Hydrogeochemical data show the occurrence of slowly varying long-term variations in the total dissolved salts and bicarbonate contents of the groundwaters, accompanied by a general decline in water temperatures. The temporal distributions of air temperature and rainfall in the Vesuvius area suggest that these variations do not depend on changes in the hydrological regime. The changes in the geochemical parameters are accompanied by slight variations in both the seismicity rate and energy release. A further relationship between seismic …

Atmospheric ScienceSoil Sciencehydrogeochemistry vesuviusAquiferAquatic ScienceInduced seismicityOceanographyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryAtmospheric temperatureStress fieldGeophysicsVolcanoShear (geology)Space and Planetary ScienceSedimentary rockGroundwaterGeologySeismologyJournal of Geophysical Research
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Geochemical monitoring of groundwaters (1998-2001) at Vesuvius volcano (Italy)

2004

This work presents the results of hydrogeochemical studies carried out at Vesuvius during the period May 1998-December 2001, mostly focusing on compositional time variations observed during this time. Based on their chemistry, groundwater samples are distinguished into two groups, 1 and 2, representative of water circulation in the southern and northern sectors of the volcano, respectively. Waters from group 1 are typically more acidic, warmer, and more saline than those of group 2. They also have higher CO2 and CH4 contents, attributed to enhanced input of deep-rising volatiles and prolonged water-rock interactions. Time-series highlight the fairly constant chemical composition of the enti…

Hydrologygeographygeography.geographical_feature_categoryVesuvius volcanic surveillance groundwater hydro-geochemistry oxygen-18biologyStable isotope ratioGeochemistryAquiferbiology.organism_classificationGeophysicsVolcanoGeochemistry and PetrologyMagmaSpring (hydrology)OlivellaVolatilesGroundwaterGeology
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"Nel più fulgido scenario di colori” Goethe e la scoperta del paradiso a Napoli

2017

Dopo avere visitato Roma, nel febbraio del 1787, J.W. Goethe giungeva a Napoli dove: «l’atmosfera si faceva sempre più pura, ormai ci trovavamo in un’altra terra». Nella seconda metà del Settecento, in Europa il poeta di Francoforte rappresentava certamente il massimo fra i divulgatori del mito del paradiso a Napoli e in Campania, ma anche in Sicilia, e dunque nel Meridione d’Italia, sia per la loro rigogliosa e sempre verde natura sia per l’abbondanza delle loro antichità classiche. A Roma Goethe aveva pregustato i frutti di questo paradiso, ma è solo visitando Napoli e il suo territorio che realizza di essere in un altro mondo, totalmente diverso dai paesi del Nord. Il presente saggio ha …

J.W. Goethe Napoli e Vesuvio Antichità classiche resti archeologici conservazione.Settore ICAR/19 - RestauroJ. W. Goethe Naples and Vesuvius classical Antiquity the archaeological remains conservation.
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Diffuse degassing of carbon dioxide at Somma-Vesuvius volcanic complex (Southern Italy) and its relation with regional tectonics

2004

Abstract A systematic survey of soil CO 2 concentrations was carried out on the flanks of Somma–Vesuvius volcano in order to constrain possible pathways responsible of carbon dioxide diffuse degassing taking place during the present state of quiescence. Measurements were performed at 1162 sites in late winter–spring 2000, highlighting that soil CO 2 concentrations range from 50 to 10500 ppmV. A statistical analysis was developed in order to define the threshold value of anomaly and separate the biogenic CO 2 component, produced by soil respiration, from the inorganic component of deep provenance. A computer routine was also elaborated to interpret the grid of CO 2 anomalous concentration va…

Provenancegeographygeography.geographical_feature_categoryLineamentSomma–Vesuvius CO2 degassing TectonicsGeochemistryMineralogyBasementTectonicschemistry.chemical_compoundGeophysicsVolcanochemistryGeochemistry and PetrologyCarbonate rockCarbonateSedimentary rockGeology
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The use and beauty of ultra-high-resolution seismic reflection imaging in Late Quaternary marine volcaniclastic settings, Napoli Bay, Italy

2019

A Nápolyi-öbölben felvett ultra nagy felbontású egycsatornás (IKB-Seistec™) reflexiós szeizmikus szelvények korábbi geológiai és geofizikai vizsgálatok eredményeivel együtt kivételes, eddig soha nem látott felbontású szeizmikus leképezését nyújtják a Flegrei-mezők és a Somma-Vezúv felszín alá süllyedt késő-pleisztocén–holocén rétegtani felépí - tésének. A szeizmikus szelvényeken látott geometria és gravitációs magvevővel nyert üledékek adatainak összevetéséből Campania partközeli kontinentális talapzatán számos olyan üledékes és vulkáni szerkezet, valamint hidrotermális jelenség került leképezésre, melyek a legutolsó glaciális maximum (kb. 18 000 év) óta keletkeztek. A Pozzuoli-öbölben mért…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleStratigraphyVolcaniclastic settingsPyroclastic rockFault (geology)PaleontologyGeochemistry and PetrologyPumiceCampania VolcanismStratovolcanoSomma-Vesuviushigh-resolution single channel reflection seismics Campania Volcanism Volcaniclastic settings Campi Flegrei Caldera ring fault Somma-Vesuvius Late Quaternary Bay of Naplesgeographygeography.geographical_feature_categoryContinental shelfResurgent domePaleontologyCaldera ring faultGeologyLate QuaternarySeafloor spreadingVolcanoHigh-resolution single channel reflection seismicsBay of NaplesCampi FlegreiGeologyFöldtani Közlöny
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Trace metal modelling of groundwater–gas–rock interactions in a volcanic aquifer: Mount Vesuvius

2005

Vesuvius
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The holocene marine record of unrest, volcanism, and hydrothermal activity of campi flegrei and somma-vesuvius

2020

Abstract This chapter illustrates the marine record of a spectrum of volcanic, hydrothermal, and sedimentary features that characterize the Latest Pleistocene–Holocene evolution of the Naples Bay offshore Campi Flegrei and Somma–Vesuvius. The work is based on review of previous literature integrated with interpretation of new high-resolution marine Digital Terrain Models (DTMs) derived from swath bathymetry surveys and high-resolution reflection seismic profiles calibrated with marine gravity core data. Seismic profiles from Pozzuoli Bay provide detailed images of the ring fault system and resurgent dome associated with the evolution of the Neapolitan Yellow Tuff (NYT) collapse caldera and …

geographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCampania volcanismResurgent domeSettore GEO/03 - Geologia StrutturaleGeochemistrySommavesuviusPyroclastic rockEastern tyrrhenian marginVolcanismFault (geology)Naples baySeafloor spreadingVolcanoPumiceCampi flegreiHolocene marine recordCalderaGeology
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