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Tra nuovi percorsi e vecchie storie. Prime note sulla memoria storico-letteraria legata all’eruzione vesuviana del 1631
In: UniSa. Sistema Bibliotecario di Ateneo (2018)
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Conduit- to Localized-scale Degassing during Plinian Eruptions: Insights from Major Element and Volatile (Cl and H2O) Analyses within Vesuvius ad 79 Pumice
In: ISSN: 0022-3530 ; EISSN: 1460-2415 ; Journal of Petrology ; https://hal.archives-ouvertes.fr/hal-01134311 ; Journal of Petrology, Oxford University Press (OUP), 2014, 55 (2), pp.315-344. ⟨10.1093/petrology/egt069⟩ (2014)
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3
Late Pleistocene to Holocene tephrostratigraphic record from the Northern Ionian Sea
In: ISSN: 0025-3227 ; Marine Geology ; https://hal.archives-ouvertes.fr/hal-03634466 ; Marine Geology, Elsevier, 2012, 311-314, pp.41 - 51. ⟨10.1016/j.margeo.2012.04.001⟩ (2012)
Abstract: International audience ; A detailed tephrostratigraphic study supported by stable isotope (δ 18 O) analyses and AMS 14 C dating was carried out on a high sedimentation rate deep-sea core recovered in the northern Ionian Sea. Eight tephra layers were recognised, all originated from explosive eruptions of southern Italian volcanoes. These tephra layers are correlated with terrestrial proximal counterparts and with both marine and lacustrine tephra already known in the central Mediterranean area. The oldest tephra (dated at ca. 19.4 ka cal BP) is tentatively correlated to the Monte Guardia eruption from Lipari Island. Two other rhyolitic tephra layers were correlated with the explosive volcanic activity of Lipari Island: Gabellotto-Fiumebianco/E-1 (8.3 ka cal BP) located close to the interruption of Sapropel S1 deposit, and Monte Pilato (ca. AD 1335) in the uppermost part of the core. The Na-phonolitic composition of the other five recognised tephra layers indicates the Somma-Vesuvius as the source. The composition is quite homogeneous among the five tephra layers, and fits that of the Mercato proximal deposits. Beyond the striking chemical similarity with the Mercato eruption, these tephra layers span over ca. 2000 years, preventing correlation with the single well known Plinian eruption of the Somma-Vesuvius. Therefore, at least two of these tephra layers were assigned to an interplinian activity of the Somma-Vesuvius between the eruptions of Mercato and Avellino, even though these eruptions remains poorly constrained in the proximal area. By contrast, the most prominent tephra layer (2 mm white tephra visible at naked eyes) was found within the S1a Sapropel interval. Despite the possible complication for the presence of similar eruption with different ages we argue that Mercato is probably a very good marker for the onset of sapropelic condition in the Ionian Sea and can be used for land-sea correlations for this important climatic event. More in general, these data allow a significant update of the knowledge of the volcanic ash dispersal from Lipari and Somma-Vesuvius volcanoes.
Keyword: [SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy; [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology; Gabellotto-Fiumebianco/E-1; Ionian Sea; Italy; Lipari; Mercato; Monte Guardia; Monte Pilato; Somma-Vesuvius; tephrochronology; volcano
URL: https://doi.org/10.1016/j.margeo.2012.04.001
https://hal.archives-ouvertes.fr/hal-03634466/file/caron-et-al-2012.pdf
https://hal.archives-ouvertes.fr/hal-03634466/document
https://hal.archives-ouvertes.fr/hal-03634466
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4
Composition and origin of nodules from the ≈20 ka Pomici di Base (PB)-Sarno eruption of Mt. Somma – Vesuvius, Italy ; Open Geosciences
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5
Naturae perdiscere mores : Naturrecht und Naturgesetz in Martin Opitz' wissenschaftlichem Gedicht "Vesuvius"
In: Zeitschrift für Germanistik. - Bern : Lang 19 (2009) 1, 41-50
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Interpretation of pre-AD 472 Roman soils from physicochemical and mineralogical properties of buried tephric paleosols at Somma Vesuviana ruin, southwest Italy
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7
Stratovolcanoes
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8
Viscous lava flows
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9
Laboratory measurements of electrical conductivities of hydrous and dry Mt. Vesuvius melts under pressure
In: ISSN: 0148-0227 ; EISSN: 2156-2202 ; Journal of Geophysical Research ; https://hal-insu.archives-ouvertes.fr/insu-00211165 ; Journal of Geophysical Research, American Geophysical Union, 2008, 113 (B05205), 41 p. ⟨10.1029/2007JB005269⟩ (2008)
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10
Non-volatile vs volatile behaviours of halogens during the AD 79 plinian eruption of Mt. Vesuvius, Italy
In: ISSN: 0012-821X ; Earth and Planetary Science Letters ; https://hal.archives-ouvertes.fr/hal-00365260 ; Earth and Planetary Science Letters, Elsevier, 2008, 269 (1-2), pp.66-79. ⟨10.1016/j.epsl.2008.02.003⟩ (2008)
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