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

Bibliographic Data

ID21785847
AuthorsSofia Pietrogrande (0009-0001-7878-5587, University of Milan, corresponding author), Davide Tantardini (0000-0003-3797-7619, University of Milan), Andrea Pezzotta (0000-0002-1093-1576, University of Milan), Paola Tartarotti (0000-0002-2236-2702, University of Milan), Andrea Zerboni (0000-0002-6844-8528, University of Milan), Roberto Sergio Azzoni (0000-0002-5931-486X, University of Milan)
Year2026
Volume22
Issue1
Publication date2026-12-31
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueJournal of Maps (JOURNAL)
Journal identifiersISSN: 1744-5647 • E-ISSN: 1744-5647
PublisherInforma UK Limited (PUBLISHER • GB)
DOI10.1080/17445647.2026.2663631
OpenAlexW7159972437
LanguageEN
References cited31

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 promoted glacial retreat and favoured the onset of periglacial and paraglacial processes. Our survey identifies 19 rock glaciers, predominantly SE-facing aspects, 11 relict and 8 transitional occurring above the 2200 m threshold suggested in regional inventories as the altitude limit for permafrost. These results highlight the importance of transitional rock glaciers as potential freshwater reservoirs under ongoing climate warming, emphasising the need for their monitoring as these features are out of equilibrium in the extant climate and likely to undergo rapid changes soon

Climate change · Glacial landform · Glacial period · Glacier · Holocene · Landform · Last Glacial Maximum · Rock glacier · Climate change and permafrost · Cryospheric studies and observations · Geology and Paleoclimatology Research

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Citation velocityhistorical
Highly citedNo

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