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Davide Tantardini

Biographic Data

ID8538675
NAMEDavide Tantardini
GIVEN NAMESDavide
FAMILY NAMETantardini
SIGNATURETANTARDINI D
AFFILIATIONSUniversity of Milan
ORCID0000-0003-3797-7619
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS0
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2022
LATEST PUBLICATION YEAR2026
H-INDEX0
  • Periglacial landforms and deposits from the Last Glacial Maximum to the Holocene in the Visogno and Spluga valleys (Central Italian Alps)

    Open Access•Sofia Pietrogrande, Davide Tantardini et al.•ARTICLE•Journal of Maps•2026

    We present the geomorphological mapping of the Visogno and Spluga valleys in the Central Italian Alps, including the morphometric and activity analysis of local rock glaciers, aimed at understanding the response to ongoing climate change. The onset of geomorphic processes controlling the evolution of local landscape dates to the Last Glacial Maximum, under glacial conditions, and continued under warmer conditions in the Holocene. The latter phase…

  • Geology of the area of the Piuro 1618 event (Val Bregaglia, Italian Central Alps)

    Open Access•Enrico Pigazzi, Riccardo Bersezio et al.•ARTICLE•Journal of Maps•2022

    The Piuro 1618 landslide is renowned as one of the most catastrophic historical events of the Central Alps. The landscape of the Bregaglia Valley has been successively modified to such an extent to make it difficult to ascertain the source of the landslide, the extent of its deposits and the setting of the ancient village. This study focuses on the identification of the source area of the landslide, its dynamics, the extent of its deposits and th…

No prominent works on this page.

  • Geology of the area of the Piuro 1618 event (Val Bregaglia, Italian Central Alps)

    Open Access•Enrico Pigazzi, Riccardo Bersezio et al.•ARTICLE•Journal of Maps•2022

    The Piuro 1618 landslide is renowned as one of the most catastrophic historical events of the Central Alps. The landscape of the Bregaglia Valley has been successively modified to such an extent to make it difficult to ascertain the source of the landslide, the extent of its deposits and the setting of the ancient village. This study focuses on the identification of the source area of the landslide, its dynamics, the extent of its deposits and th…

  • Periglacial landforms and deposits from the Last Glacial Maximum to the Holocene in the Visogno and Spluga valleys (Central Italian Alps)

    Open Access•Sofia Pietrogrande, Davide Tantardini et al.•ARTICLE•Journal of Maps•2026

    We present the geomorphological mapping of the Visogno and Spluga valleys in the Central Italian Alps, including the morphometric and activity analysis of local rock glaciers, aimed at understanding the response to ongoing climate change. The onset of geomorphic processes controlling the evolution of local landscape dates to the Last Glacial Maximum, under glacial conditions, and continued under warmer conditions in the Holocene. The latter phase…

Cryospheric studies and observations (2 works) · Geology and Paleoclimatology Research (2 works) · Archaeology (1 work) · Climate change (1 work) · Climate change and permafrost (1 work) · Debris (1 work) · Debris flow (1 work) · Erosion (1 work) · Geography (1 work) · Geology (1 work)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae