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  • 1
    Publication Date: 2022-03-25
    Description: The magnitude and intensity of the 60 CE Cretaio Tephra, the largest historical explosive eruption at Ischia caldera (Italy), was studied integrating field data and numerical modelling in order to reconstruct the dispersal of the fall out related to the climax phase of the eruption and characterize its physical parameters. A field survey of the main fall unit (EUC) of Cretaio Tephra and its sampling was performed on the island, which is the proximal area of dispersal, and for the first time outcrops of this tephra were found southward on the Capri Island. The dataset is completed by a distal tephra sampled in the offshore and described in the literature, allowing the analysis of samples of intermediate and distal deposits. Grain size analysis of the samples collected on the island show bimodal distributions due to the presence of a ballistic component, especially in the most proximal sampling sites around the inferred and buried vent. Tails of fine ash in the distributions can be associ ated with settling enhanced by ash aggregation processes in the moisture-rich plume. Tephra dispersal was re constructed using the HAZMAP tephra dispersal model by minimizing the difference between the simulations obtained exploring plausible ranges of eruption source parameters and the available thickness and grain-size measurements. Results show that the dispersal axis of EUC is to the south-southeast, the best guess for the total erupted volume of tephra is 0.075 km3 , the plume height ranges between 5 and 13 km, for an average mass eruption rate (MER) of 105 kg/s, hence a duration of the eruption of a few days. Considering an eruptive sce nario given by the eruption parameters and diffusion coefficient of the Cretaio Tephra, together with a statistical set of wind profiles, HAZMAP modelling allowed us to generate tephra loading probability maps, needed to assess the impact of such an eruption at Ischia Island and the Neapolitan metropolitan area, pivotal for civil protection purposes. Another important outcome of the study is that, for volcanic islands, the reconstruction of eruption parameters may benefit much more from the search of even few medial and distal offshore outcrops than from implementing the on-island proximal dataset only.
    Description: Published
    Description: 107248
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Keywords: fallout features ; Cretaio Tephra (Ischia Island, Italy) ; data analysis ; numerical modelling: ; hazard assessment
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2021-11-29
    Description: L’eruzione pliniana delle Pomici di Avellino rappresenta uno dei principali eventi esplosivi nell’area Mediterranea dell’Olocene. Le eruzioni pliniane costituiscono uno fra gli eventi naturali potenzialmente più dannosi per le vite umane e l’ambiente. Esse sono generalmente caratterizzate da fasi esplosive sostenute molto energetiche, che possono durare diverse ore, con Intensità non inferiori a 107 -108 kg s-1 . Queste caratteristiche portano alla formazione di colonne convettive stratosferiche, la cui instabilità e collasso possono generare correnti piroclastiche di densità (PDC)1 , che si formano quando miscele di gas e particelle solide, emesse durante le eruzioni, collassano e scorrono al suolo sotto l’effetto della gravità2 . Le PDC possono devastare completamente le zone circostanti il vulcano fino a decine di chilometri di distanza. Distanze di centinaia di chilometri dal centro eruttivo, nella direzione del vento dominante caratterizzano, invece, i depositi da caduta associati alle fasi di colonna sostenuta. Nell’insieme, si tratta di eventi molto rari alla scala della vita umana, per cui la loro dinamica eruttiva viene ricostruita principalmente sulla base dello studio dei depositi delle eruzioni passate. Tali studi sono particolarmente importanti nel caso di vulcani quiescenti, la cui riattivazione e comportamento eruttivo sono difficili da definire in assenza di attività frequente3 .
    Description: Published
    Description: 41-55
    Description: 5V. Processi eruttivi e post-eruttivi
    Keywords: L’eruzione pliniana ; Nola - Croce del Papa
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 3
    Publication Date: 2022-02-17
    Description: Il sito delle “Ciampate del diavolo”, sul fianco nord­orientale del vulcano Roccamonfina, è un sito unico al Mondo grazie alle sue peculiarità geologiche ed antropologiche. Il ritrovamento di impronte di hominini al di sopra di un deposito ignimbritico, impresse in nel periodo di maggiore attività del vulcano, dà spazio a numerose questioni circa le condizioni paleoambientali esistenti sul vulcano ed i complessi processi che hanno permesso la formazione e la conservazione delle impronte. La nota dedica particolare attenzione al contesto dell’attività del vulcano ed alle caratteristiche della serie dei Tufi Leucitici Bruni, in quanto le impronte note come “Ciampate del diavolo” sono presenti sulla superficie di una delle unità più alte della sequenza di questi tufi. The “Ciampate del diavolo” geosite is unique in the World due to its geological and anthropological peculiarities. Finding hominin footprints on the ignimbrite deposits of 350,000 years ago, imprinted in the period of greatest activity of the volcano, opens up numerous questions about the palaeoenvironmental conditions of the volcano and the complex processes that allowed the generation and conservation of the footprints. The note pays particular attention to the framing of the volcano's activity and to the features of deposits of the Brown Leucitic Tuff series, as the human fossil footprints known as "Ciampate del Diavolo" are preserved on the surface of one of the highest units in the sequence.
    Description: Published
    Description: 49-55
    Description: 1V. Storia eruttiva
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 1TR. Georisorse
    Description: 6SR VULCANI – Servizi e ricerca per la società
    Description: N/A or not JCR
    Keywords: Stratigrafia ; Ignimbrite ; Eruzioni esplosive ; Volcano di Roccamonfina ; Tufo Leucitico Bruno
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2021-12-07
    Description: INGV, IMO, UI and CPD-NCIP.
    Description: Published
    Description: 1V. Storia eruttiva
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: 4V. Processi pre-eruttivi
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Keywords: Somma - Vesuvius ; active volcanoes ; Campania
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: web product
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  • 5
    Publication Date: 2021-12-07
    Description: INGV, IMO, UI and CPD-NCIP
    Description: Published
    Description: 1V. Storia eruttiva
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: 4V. Processi pre-eruttivi
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Keywords: Campi Flegrei caldera ; seismicity ; fumarolic activity ; ground deformation
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: web product
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  • 6
    Publication Date: 2021-12-15
    Description: 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 and human history of Campi Flegrei and discuss the interactions between humans and the environment within the “burning felds” from around 10,000 years until the 1538 CE Monte Nuovo eruption and more recent times. The region’s incredibly rich written history documents how the landscape changed both naturally and anthropogenically, with the volcanic system fuelling these considerable natural changes. Humans have exploited the beautiful landscape, accessible resources (e.g. volcanic ash for pulvis puteolana mortar) and natural thermal springs associated with the volcano for millennia, but they have also endured the downsides of living in a volcanically active region—earthquakes, signifcant ground deformation and landscape altering eruptions. The pre-historic record is detailed, and various archaeological sites indicate that the region was certainly occupied in the last 10,000 years. This history has been reconstructed by identifying archaeological fnds in sequences that often contain ash (tephra) layers from some of the numerous volcanic eruptions from Campi Flegrei and the other volcanoes in the region that were active at the time (Vesuvius and Ischia). These tephra layers provide both a relative and absolute chronology and allow the archaeology to be placed on a relatively precise timescale. The records testify that people have inhabited the area even when Campi Flegrei was particularly active.The archaeological sequences and outcrops of pyroclastic material preserve details about the eruption dynamics, buildings from Roman times, impressive craters that now host volcanic lakes and nature reserves, all of which make this region particularly mystic and fascinating, especially when we observe how society continues to live within the active caldera system. The volcanic activity and long record of occupation and use of volcanic resources in the region make it unique and here we outline key aspects of its geoheritage.
    Description: Published
    Description: 5
    Description: 1V. Storia eruttiva
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: 6SR VULCANI – Servizi e ricerca per la società
    Description: JCR Journal
    Keywords: Archaeology ; Campania ; Campi Flegrei volcano ; History ; Human
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
    Publication Date: 2021-12-15
    Description: Archaeological and volcanological studies have revealed that eruptions of Neapolitan volcanoes have conditioned human settlement patterns since prehistoric times. The occurrence of high intensity explosive eruptions, interspersed with long periods of quiescence, has characterized the last 10 ka of activity of these volcanoes. Geoarchaeological studies, carried out in advance of investigations for the construction of the Rome-Naples and the new Naples-Bari railway lines, have made possible a detailed reconstruction of human presence in the central part of the Campania Plain up to the coastal strip, between the late Neolithic and the late Bronze Age. The examined chronological interval includes sequences of pyroclastic deposits erupted by both Campi Flegrei and Somma-Vesuvius, and paleosols with evidence of anthropic frequentation. Altogether, the geoarchaeological data have provided a detailed picture of human settlement and activities through time with a particular focus on a long period of quiescence of the two volcanoes and also during their intense activity.
    Description: Published
    Description: VO546
    Description: 1V. Storia eruttiva
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: JCR Journal
    Keywords: Campania Plain ; Neapolitan Volcanoes ; Archaeology ; Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2021-12-15
    Description: The paper aims at merging the first results from the analyses of the georesources exploited in the site of Piano dei Cardoni (Ustica island, Italy) during the Neolithic phases of its occupation (MiddleLate Neolithic, 4.7-4.2 ka cal BC). Grinding tools consist of a very varied typology of local volcanic rocks, easy to collect and available very close to the investigated site. A selection of shapes and lithology is applied to reach the best performance of the tools. The elevated number of grinders, pestles, mortars testify to an intense activity of food/plant processing in the site. The absence of chert or obsidian resources on the island pushed the human communities to import such raw materials from the Aeolian islands and probably from the north-western area of Palermo. Pumice is collected on the same island, probably due to the local availability and its good quality. Similarly, local clay resources are used for the manufacture of ceramics, mostly burnished and incised wares. Ustica was therefore almost autonomous for the exploitation of resources, with volcanic rocks readily available in abundance and with the most significant exception being chert and obsidian. This last one probably imported and worked on the island and then moved towards North-Western Sicily.
    Description: Published
    Description: VO552
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: Neolithic ; Chert ; Obsidian ; Ceramics ; Volcanic tools
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2021-12-15
    Description: This special issue of Annals of Geophysics entitled: “When Volcanologists Meet Archaeologists and Other Disciplines: Relationships Between Eruptions and Human Communities” originates from a session (S13) of the Rittmann International Conference which took place in Catania on February 13th 2020, having as its main theme the history of volcanology and the impact of volcanic activity on humans. The twelve articles collected in this special issue reflect the aims and contents of the reports presented by some participants at this session of the Rittmann conference
    Description: Published
    Description: 6SR VULCANI – Servizi e ricerca per la società
    Description: JCR Journal
    Keywords: volcanologists ; archaeologists ; Eruptions ; Human Communities
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2021-11-29
    Description: L’eruzione pliniana delle Pomici di Avellino rappresenta uno dei principali eventi esplosivi nell'area Mediterranea dell’Olocene. Le eruzioni pliniane costituiscono uno fra gli eventi naturali potenzialmente più dannosi per le vite umane e l’ambiente. Esse sono generalmente caratterizzate da fasi esplosive sostenute molto energetiche, che possono durare diverse ore, con Intensità non inferiori a 107 -108 kg s-1. Queste caratteristiche portano alla formazione di colonne convettive stratosferiche, la cui instabilità e collasso possono generare correnti piroclastiche di densità (PDC)1 , che si formano quando miscele di gas e particelle solide, emesse durante le eruzioni, collassano e scorrono al suolo sotto l’effetto della gravità2 . Le PDC possono devastare completamente le zone circostanti il vulcano fino a decine di chilometri di distanza. Distanze di centinaia di chilometri dal centro eruttivo, nella direzione del vento dominante caratterizzano,invece,i depositi da caduta associati alle fasi di colonna sostenuta. Nell’insieme, si tratta di eventi molto rari...
    Description: Published
    Description: 41-56
    Description: 1V. Storia eruttiva
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Keywords: eruzione Pomici di Avellino ; Nola - Croce del Papa
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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