INVESTIGATING EVIDENCES OF QUATERNARY GLACIATIONS IN THE PREALPINE ENVIRONMENT OF THE ASTICO VALLEY

Article Sidebar

PDF
Published: 2011-01-15
DOI: https://doi.org/10.26382/
Keywords:
Quaternary glaciations, Astico valley, sand petrography

Main Article Content

Sandro Rossato
University of Padua, Department of Geography, Padova (Italy)
Giovanni Monegato
University of Padua, Department of Geoscience, Padova (Italy)
Paolo Mozzi
University of Padua, Department of Geography, Padova (Italy)

Abstract

ABSTRACT: Rossato S., Monegato G. & Mozzi P., Investigating evidences of Quaternary glaciations in the Prealpine environment of the Astico valley. (IT ISSN 0394-3356, 2011) In the Astico valley (Venetian Prealps) some glacial, fluvioglacial and glaciolacustrine deposits were found. They are attributed to a pre-LGM glacial advance which reached further out in the valley. Geomorphological and stratigraphic data support this hypothesis. It is also pointed out the presence of a tectonic guidance in the developing of the Astico fluvial network.

Article Details

Issue

Vol. 24 No. Extended Abstract (2011): IL QUATERNARIO

Section

Articles
Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

The Author grants usage rights to others using an open license (Creative Commons or equivalent) allowing for immediate free access to the work and permitting any user to read, download, copy, distribute, print, search, or link to the full texts of articles, crawl them for indexing, pass them as data to software, or use them for any other lawful purpose.

How to Cite

Rossato, S., Monegato, G., & Mozzi, P. (2011). INVESTIGATING EVIDENCES OF QUATERNARY GLACIATIONS IN THE PREALPINE ENVIRONMENT OF THE ASTICO VALLEY. Alpine and Mediterranean Quaternary, 24(Extended Abstract), 126-128. https://doi.org/10.26382/