Evolution of an Alpine fluvioglacial system at the LGM decay: The Cormor megafan (NE Italy)

Autor: Ivonne Burla, Enrico Zavagno, Franco Cucchi, Alessandro Fontana, Stefano Devoto, Giovanni Monegato

Publikováno v: Geomorphology (Amst.) 204 (2014): 136–153. doi:10.1016/j.geomorph.2013.07.034
info:cnr-pdr/source/autori:Fontana A.[1], Monegato G. [2], Zavagno E.[3], Devoto S. [3], Burla I. [3], Cucchi F.[3]/titolo:Evolution of an Alpine fluvioglacial system at the LGM decay: The Cormor megafan (NE Italy)/doi:10.1016%2Fj.geomorph.2013.07.034/rivista:Geomorphology (Amst.)/anno:2014/pagina_da:136/pagina_a:153/intervallo_pagine:136–153/volume:204

The dramatic climatic and environmental changes that occurred at the end of the last glaciation led to the formation of landforms (e.g., moraines, fluvial ridges, and alluvial terraces) that strongly characterize the landscape in the alluvial plains

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https://publications.cnr.it/doc/269849