LANDSLIDES OF THE WESTERN DOLOMITES: CASE STUDIES FROM THE ADIGE AND SARCA VALLEYS(NE ITALY)

Autor: Martin S.[1], Ivy-Ochs S.[2, Viganò A.[4], Campedel P.[4], Rigo M.[1, Vockenhuber C.[3], Gabrieli F.[6], Mair V.[7], Rossato S.[5]

Publikováno v: Alpine and Mediterranean Quaternary
33 (2020): 191–207. doi:10.26382/AMQ.2020.15
info:cnr-pdr/source/autori:Martin S.[1], Ivy-Ochs S.[2,3], Viganò A.[4], Campedel P.[4], Rigo M.[1,5], Vockenhuber C.[3], Gabrieli F.[6], Mair V.[7], Rossato S.[5]/titolo:LANDSLIDES OF THE WESTERN DOLOMITES: CASE STUDIES FROM THE ADIGE AND SARCA VALLEYS(NE ITALY)./doi:10.26382%2FAMQ.2020.15/rivista:Alpine and Mediterranean Quaternary (Print)/anno:2020/pagina_da:191/pagina_a:207/intervallo_pagine:191–207/volume:33

The Lavini di Marco, Marocche di Dro and Molveno rock avalanches in Trentino, and the Termeno landslide in South Tyrol are here presented as case studies for the western Dolomites(Adige and Sarca Valleys, NE Italy). Their structural predisposition, r

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