Search Results - "Di Vito, M A"
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Magma Degassing as a Source of Long‐Term Seismicity at Volcanoes: The Ischia Island (Italy) Case
Published in Geophysical research letters (28-12-2019)“…Transient seismicity at active volcanoes poses a significant risk in addition to eruptive activity. This risk is powered by the common belief that volcanic…”
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The Pomici di Avellino eruption of Somma–Vesuvius (3.9 ka BP). Part II: sedimentology and physical volcanology of pyroclastic density current deposits
Published in Bulletin of volcanology (01-07-2010)“…Pyroclastic density currents (PDCs) generated during the Plinian eruption of the Pomici di Avellino (PdA) of Somma–Vesuvius were investigated through field and…”
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Stress inversions to forecast magma pathways and eruptive vent location
Published in Science advances (01-07-2019)“…When a batch of magma reaches Earth's surface, it forms a vent from which volcanic products are erupted. At many volcanoes, successive batches may open vents…”
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Tephra fallout hazard assessment at the Campi Flegrei caldera (Italy)
Published in Bulletin of volcanology (01-04-2009)“…Tephra fallout associated with renewal of volcanism at the Campi Flegrei caldera is a serious threat to the Neapolitan area. In order to assess the hazards…”
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The Pomici di Avellino eruption of Somma-Vesuvius (3.9 ka bp). Part I: stratigraphy, compositional variability and eruptive dynamics
Published in Bulletin of volcanology (01-07-2010)“…The stratigraphic succession of the Pomici di Avellino Plinian eruption from Somma-Vesuvius has been studied through field and laboratory data in order to…”
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The long and intertwined record of humans and the Campi Flegrei volcano (Italy)
Published in Bulletin of volcanology (2022)“…The Campi Flegrei volcano (or Phlegraean Fields), Campania, Italy, generated the largest eruption in Europe in at least 200 ka. Here we summarise the volcanic…”
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Reactivation of Stromboli's summit craters at the end of the 2007 effusive eruption detected by thermal surveys and seismicity
Published in Journal of geophysical research. Solid earth (01-11-2015)“…This work arises from the field observations made during the civil protection emergency period connected to the 2007 Stromboli eruption. We observed changes in…”
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The volcanic and geothermally active Campi Flegrei caldera: an integrated multidisciplinary image of its buried structure
Published in International journal of earth sciences : Geologische Rundschau (01-03-2014)“…The Campi Flegrei caldera in southern Italy is one of the greatest geohazard areas on Earth. Evidence of an active magmatic and geothermal system is provided…”
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The “Pomici di mercato” Plinian eruption of Somma-Vesuvius: magma chamber processes and eruption dynamics
Published in Bulletin of volcanology (01-05-2008)“…The Pomici di Mercato (PdM, 8,010 ± 40 a), also known in the literature as Pomici Gemelle or Pomici di Ottaviano, is one of the oldest Plinian eruptions of…”
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The magmatic feeding system of the Campi Flegrei caldera: Architecture and temporal evolution
Published in Chemical geology (24-02-2011)“…To develop a model of both the structure and evolution of the Campi Flegrei caldera (CFc) magmatic feeding system, geochronological, geochemical and Sr, Nd, Pb…”
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Magmatic History of Somma-Vesuvius on the Basis of New Geochemical and Isotopic Data from a Deep Borehole (Camaldoli della Torre)
Published in Journal of petrology (01-04-2007)“…A continuous-coring borehole recently drilled at Camaldoli della Torre on the southern slopes of Somma-Vesuvius provides constraints on the volcanic and…”
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Slope processes in weathered volcaniclastic deposits within the city of Naples: The Camaldoli Hill case
Published in Geomorphology (Amsterdam) (15-06-2007)“…We describe the slope processes acting on Camaldoli Hill, the main volcanic feature of the Neapolitan area whose geological evolution and setting have been…”
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Journal Article Conference Proceeding -
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Distal Effects of Volcanic Eruptions on Pre-industrial societies
Published in Quaternary international (10-01-2019)Get full text
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Intersection of exogenous, endogenous and anthropogenic factors in the Holocene landscape: A study of the Naples coastline during the last 6000 years
Published in Quaternary international (25-07-2013)“…New data on the ancient landscape of Naples (southern Italy) during the middle and late Holocene from geo-archaeological excavations associated with public…”
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The late Pleistocene pyroclastic deposits of the Campanian Plain: New insights into the explosive activity of Neapolitan volcanoes
Published in Journal of volcanology and geothermal research (20-10-2008)“…The lithological and compositional characteristics of eighteen different pyroclastic deposits of Campanian origin, dated between 125 cal ky BP and 22 cal ky…”
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Journal Article Conference Proceeding -
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Volcanism and deformation since 12,000 years at the Campi Flegrei caldera (Italy)
Published in Journal of volcanology and geothermal research (01-08-1999)“…The Campi Flegrei caldera is a restless, nested structure resulting from two major collapses related to the Campanian Ignimbrite (37,000 years BP) and the…”
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The role of volcanic activity and climate in alluvial fan growth at volcanic areas: an example from southern Campania (Italy)
Published in Sedimentary geology (15-06-2004)“…Volcaniclastic-rich alluvial fans developed in the southern Campanian Plain (Italy) during the late Pleistocene and Holocene in an area eastward of the…”
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The Agnano–Monte Spina eruption (4100 years BP) in the restless Campi Flegrei caldera (Italy)
Published in Journal of volcanology and geothermal research (01-08-1999)“…The Agnano–Monte Spina tephra (AMST), dated at 4100 years BP by 40 Ar/ 39 Ar and 14 C AMS techniques, is the product of the highest-magnitude eruption in the…”
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The present state of the magmatic system of the Campi Flegrei caldera based on a reconstruction of its behavior in the past 12 ka
Published in Journal of volcanology and geothermal research (01-08-1999)“…New geochemical and Sr-isotope data have been acquired on samples representative of volcanic units erupted inside the resurgent Campi Flegrei caldera (CFc)…”
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