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Andrea Caburlotto

Biographic Data

ID6372440
NAMEAndrea Caburlotto
GIVEN NAMESAndrea
FAMILY NAMECaburlotto
SIGNATURECABURLOTTO A
AFFILIATIONSNational Institute of Oceanography and Applied Geophysics
ORCID0000-0001-7259-6884
VERIFIEDYes
TOTAL WORKS3
TOTAL CITATIONS0
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2021
LATEST PUBLICATION YEAR2024
H-INDEX0
  • Geohazard Features of the Ionian Calabrian Margin

    Open Access•Silvia Ceramicola, Andrea Cova et al.•ARTICLE•Journal of Maps•2024

    Here we present a detailed description of different geomorphic features to complement the Maps of Geohazard Features of the Ionian Calabrian Margin produced by the Magic project (Marine Geohazard along Italian Coasts). Some of the most striking features we imaged are sources of widespread and recurrent geohazards. These include multiple coastal landslides, failure scars along open slopes, shelf-indenting retrogressive canyon headwalls and active …

  • Late Quaternary transgressions and regressions in the Trieste Gulf (north-eastern Adriatic Sea)

    Open Access•Massimo Zecchin, Mauro Caffau et al.•ARTICLE•Quaternary International•2024

    The integration of high-resolution seismic profiles, core data and radiocarbon plus U-Th datings, allows to document the late Quaternary succession of the Trieste Gulf, which represents the easternmost part of the northern Adriatic Sea. This succession consists of an alternation of shallow-marine and continental deposits organized to compose four transgressive-regressive sequences down to ca. 90 m below present sea level. The sequences terminate …

  • Stratigraphic signature of the Perito Moreno ice-dammings during the Little Ice Age (southern Patagonia, Argentina)

    Open Access•Mauro Caffau, Emanuele Lodolo et al.•ARTICLE•The Holocene•2021•References: 7

    The spectacular water outburst occurring semi-periodically when the ice-dam formed by the external front of the Perito Moreno glacier collapses, is one of the most attracting events in the UNESCO ‘Parque Nacional Los Glaciares’ of southern Patagonia. These occurrences have been documented since 1936. Instead, evidence of previous events has been only indirectly provided by dendrochronology analysis. Here we show for the first time radiocarbon-dat…

No prominent works on this page.

  • Stratigraphic signature of the Perito Moreno ice-dammings during the Little Ice Age (southern Patagonia, Argentina)

    Open Access•Mauro Caffau, Emanuele Lodolo et al.•ARTICLE•The Holocene•2021•References: 7

    The spectacular water outburst occurring semi-periodically when the ice-dam formed by the external front of the Perito Moreno glacier collapses, is one of the most attracting events in the UNESCO ‘Parque Nacional Los Glaciares’ of southern Patagonia. These occurrences have been documented since 1936. Instead, evidence of previous events has been only indirectly provided by dendrochronology analysis. Here we show for the first time radiocarbon-dat…

  • Geohazard Features of the Ionian Calabrian Margin

    Open Access•Silvia Ceramicola, Andrea Cova et al.•ARTICLE•Journal of Maps•2024

    Here we present a detailed description of different geomorphic features to complement the Maps of Geohazard Features of the Ionian Calabrian Margin produced by the Magic project (Marine Geohazard along Italian Coasts). Some of the most striking features we imaged are sources of widespread and recurrent geohazards. These include multiple coastal landslides, failure scars along open slopes, shelf-indenting retrogressive canyon headwalls and active …

  • Late Quaternary transgressions and regressions in the Trieste Gulf (north-eastern Adriatic Sea)

    Open Access•Massimo Zecchin, Mauro Caffau et al.•ARTICLE•Quaternary International•2024

    The integration of high-resolution seismic profiles, core data and radiocarbon plus U-Th datings, allows to document the late Quaternary succession of the Trieste Gulf, which represents the easternmost part of the northern Adriatic Sea. This succession consists of an alternation of shallow-marine and continental deposits organized to compose four transgressive-regressive sequences down to ca. 90 m below present sea level. The sequences terminate …

Geology (3 works) · Geography (2 works) · Geology and Paleoclimatology Research (2 works) · Geomorphology (2 works) · Glacial period (2 works) · Maritime and Coastal Archaeology (2 works) · Oceanography (2 works) · Paleontology (2 works) · Radiocarbon dating (2 works) · Stadial (2 works)

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