@prefix prodottidellaricerca: . @prefix istituto: . @prefix prodotto: . istituto:CDS066 prodottidellaricerca:prodotto prodotto:ID41517 . @prefix pubblicazioni: . @prefix unitaDiPersonaleInterno: . unitaDiPersonaleInterno:MATRICOLA16574 pubblicazioni:autoreCNRDi prodotto:ID41517 . @prefix rdf: . @prefix retescientifica: . prodotto:ID41517 rdf:type retescientifica:ProdottoDellaRicerca , prodotto:TIPO1101 . @prefix rdfs: . prodotto:ID41517 rdfs:label "Landslides and climate change in the Italian Dolomites since the Lateglacial. (Articolo in rivista)"@en . @prefix xsd: . prodotto:ID41517 pubblicazioni:anno "2004-01-01T00:00:00+01:00"^^xsd:gYear . @prefix skos: . prodotto:ID41517 skos:altLabel "
Soldati M.; Corsini A.; Pasuto A. (2004)
Landslides and climate change in the Italian Dolomites since the Lateglacial.
in Catena (Cremling.)
"^^rdf:HTML ; pubblicazioni:autori "Soldati M.; Corsini A.; Pasuto A."^^xsd:string ; pubblicazioni:paginaInizio "141"^^xsd:string ; pubblicazioni:paginaFine "161"^^xsd:string ; pubblicazioni:numeroVolume "55/2"^^xsd:string . @prefix ns10: . prodotto:ID41517 pubblicazioni:rivista ns10:ID347507 ; pubblicazioni:note "pp. 141-161."^^xsd:string ; skos:note "ISI Web of Science (WOS)"^^xsd:string , "Scopus"^^xsd:string ; pubblicazioni:affiliazioni "Soldati M., Dipartimento di Scienze della Terra, Universita` degli Studi di Modena e Reggio Emilia, Largo S. Eufemia 19, 41100 Modena, Italy\nCorsini A., Dipartimento di Scienze della Terra, Universita` degli Studi di Modena e Reggio Emilia, Largo S. Eufemia 19, 41100 Modena, Italy"^^xsd:string ; pubblicazioni:titolo "Landslides and climate change in the Italian Dolomites since the Lateglacial."^^xsd:string ; prodottidellaricerca:abstract "The paper deals with the relationship between the temporal occurrence of landslides and climatic\nchanges in the Italian Dolomites since the Late glacial. After an introduction on the state of the art,\nwith particular reference to the Alpine region, the results of recent investigations in the two study\nsites are illustrated. At Cortina d'Ampezzo, several landslides were dated mainly by the radiocarbon\nmethod. The most ancient landslide event there involved large rock slides, which affected the\ndolomitic slopes following the withdrawal of glaciers after the Last Glacial Maximum (LGM), and\nalso slides and flows mainly occurring in pelitic materials of the valley floors (from 13,000 to\n10,000 cal BP). A later series of flows occurred between 5500 and 2500 cal BP. In the Upper Badia\nValley (Alta Badia), the most ancient events go back to 10,000 and 9000 cal BP, and correspond\nwith earth flows that followed vast rotational slides affecting the bedrock up to a depth of about 50\nm. More recent earth flows, involving more modest amounts of material, took place between 6500\nand 2300 cal BP.\nBy analysing the dates from the two study areas, it was possible to correlate the recorded\nincrease of landslide activity with the climatic changes occurring at the boundary between the Late\nglacial and the Holocene and between the Atlantic and the Subboreal, and to compare the results\nwith those derived from other European regions. The types and causes of landslides taking place in\nthese two periods were substantially different, reflecting the different morphoclimatic conditions\nthat existed in the two areas when these mass movements were triggered. Finally, notwithstanding\nthe importance of non-climatic causes, such as geological-structural factors and possible human\ninfluences, it is concluded that many of the dated landslides can be considered as indicators of\nclimatic change."@en ; prodottidellaricerca:prodottoDi istituto:CDS066 ; pubblicazioni:autoreCNR unitaDiPersonaleInterno:MATRICOLA16574 . @prefix parolechiave: . prodotto:ID41517 parolechiave:insiemeDiParoleChiave . ns10:ID347507 pubblicazioni:rivistaDi prodotto:ID41517 . parolechiave:insiemeDiParoleChiaveDi prodotto:ID41517 .