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  • elsevier  (2)
  • Aracne Editore, Napoli  (1)
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  • 1
    Publication Date: 2017-04-04
    Description: We describe the slope processes acting on Camaldoli Hill, the main volcanic feature of the Neapolitan area whose geological evolution and setting have been reconstructed. The backbone of the hill includes the remnants of two partially superposed tuff cones, lying between the Campanian Ignimbrite (CI) and the Neapolitan Yellow Tuff (NYT). This sequence is mantled by pyroclastic, anthropogenic and epiclastic deposits, with abrupt thickness and facies variations. The structural setting of the hill mainly results from several phases of reactivation of the CI caldera faults which were active until about 9.5 ka. Deformation younger than 15 ka is evidenced by landslide deposits, caused by slope instability from volcano-tectonism, and by a high-angle erosional unconformity, formed in response to a base-level lowering. A stratigraphic analysis of the reworked deposits at the foot of the slopes allowed us to define both depositional mechanisms and sedimentation rates. The results of combined volcanological, geomorphological and engineering-geological studies permitted us to constrain and quantify past geological processes and hypothesis about the future evolution of the hill. Present-day slope processes on Camaldoli Hill are largely controlled by the presence of weathered and reworked deposits, whose nature and thickness have been analysed and mapped in detail. Four main kinds of slope processes have been recognized: falls and toppling failures from NYT; small-scale slides in the weathered and pedogenized loose cover; mixed events, represented by slides evolving to hyperconcentrated flows, mud flows and debris flows; and areal and linear erosion. Consequently, a high number of mass movements not previously documented have been mapped. At the same time, an insight into the sedimentation rate due to the overall slope processes, covering a time-span of about 5 ka, was given. Some final considerations regarding landslide hazard are presented in the context of the most suitable remedial works.
    Description: Published
    Description: 132–157
    Description: 3.5. Geologia e storia dei sistemi vulcanici
    Description: 4.4. Scenari e mitigazione del rischio ambientale
    Description: JCR Journal
    Description: reserved
    Keywords: Slope processes ; Weathering ; Volcaniclastic rocks ; Hazard ; Risk ; 04. Solid Earth::04.04. Geology::04.04.03. Geomorphology ; 04. Solid Earth::04.04. Geology::04.04.07. Rock geochemistry ; 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport ; 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2017-04-04
    Description: Studi archeologici e vulcanologici condotti nell’area napoletana, hanno evidenziato che le eruzioni del Somma-Vesuvio e della caldera dei Campi Flegrei hanno fortemente condizionato lo sviluppo e il declino degli insediamenti umani in quest’area sin dalla Preistoria. Il verificarsi di eruzioni fortemente esplosive, intercalate con eruzioni effusive ed esplosive di bassa intensità, ha caratterizzato gli ultimi 10.000 anni di attività di questi vulcani. La lunga storia dell’interazione tra uomo e vulcano è dettagliatamente registrata nella stratigrafia della Piana Campana e gli studi archeologici e vulcanologici condotti in concomitanza con l’esecuzione di indagini sistematiche o preventive ad opere pubbliche, hanno contribuito a definire il quadro degli insediamenti e delle attività umane tra il Tardo Neolitico e l’epoca storica attorno ai vulcani napoletani. Durante questo periodo di tempo la Piana Campana è stata intensamente frequentata, attraversata da vie di comunicazione di lunga persistenza temporale e soggetta a consistente sfruttamento agricolo. Le eruzioni vulcaniche del Vesuvio e dei Campi Flegrei hanno spesso determinato lunghi intervalli nella frequentazione di queste aree, ma hanno altresì contribuito alla straordinaria fertilità dei suoli favorendone lo sfruttamento agricolo. In particolare, come verrà illustrato nel paragrafo seguente, l’attività vulcanica del Vesuvio ha fortemente condizionato l’evoluzione delle piane circostanti in un periodo di tempo tanto interessante quanto poco conosciuto, compreso tra le eruzioni pliniane delle Pomici di Avellino e del 472 d.C.
    Description: Published
    Description: 62-67
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: 3.10. Storia ed archeologia applicate alle Scienze della Terra
    Description: reserved
    Keywords: Vesuvio ; Piana Campana ; impatto delle eruzioni esplosive su insediamenti antropici ; uso e abbandono del territorio ; 05. General::05.01. Computational geophysics::05.01.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 3
    Publication Date: 2021-12-16
    Description: Ash samples from tephra layers correlated with the Pomici di Avellino (Avellino Pumice) eruption of Somma-Vesuvius were collected in distal archives and their composition and particle morphology investigated in order to infer their behaviour of transportation and deposition. Differences in composition and particle morphologies were recognised for ash particles belonging to the magmatic Plinian and final phreatomagmatic phases of the eruption. The ash particles were dispersed in opposite directions during the two different phases of the eruption, and these directions are also different from that of coarse-grained fallout deposits. In particular, ash generated during magmatic phase and injected in the atmosphere to form a sustained column shows a prevailing SE dispersion, while ash particles generated during the final phreatomagmatic phase and carried by pyroclastic density currents show a general NW dispersion. These opposite dispersions indicate an ash dispersal influenced by both high and low atmosphere dynamics. In particular, the magmatic ash dispersal was first driven by stratospheric wind towards NE and then the falling particles encountered a variable wind field during their settling, which produced the observed preferential SE dispersal. The wind field encountered by the rising ash clouds that accompanied the pyroclastic density currents of the final phreatomagmatic phase was different with respect to that encountered by the magmatic ash, and produced a NW dispersal. These data demonstrate how ash transportation and deposition are greatly influenced by both high and low atmosphere dynamics. In particular, fine-grained particles transported in ash clouds of small-scale pyroclastic density currents may be dispersed over distances and cover areas comparable with those injected into the stratosphere by Plinian, sustained columns. This is a point not completely addressed by present day mitigation plans in case of renewal of activity at Somma-Vesuvius, and can yield important information also for other volcanoes potentially characterised by explosive activity.
    Description: Published
    Description: On line First
    Description: 2.3. TTC - Laboratori di chimica e fisica delle rocce
    Description: 3.5. Geologia e storia dei sistemi vulcanici
    Description: 3.6. Fisica del vulcanismo
    Description: JCR Journal
    Description: open
    Keywords: Pomici di Avellino eruption ; ash dispersal ; atmosphere dynamics ; volcanic hazard ; 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology ; 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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