Articles | Volume 6, issue 3
Earth Surf. Dynam., 6, 809–828, 2018
https://doi.org/10.5194/esurf-6-809-2018
Earth Surf. Dynam., 6, 809–828, 2018
https://doi.org/10.5194/esurf-6-809-2018

Research article 26 Sep 2018

Research article | 26 Sep 2018

Glacial dynamics in pre-Alpine narrow valleys during the Last Glacial Maximum inferred by lowland fluvial records (northeast Italy)

Sandro Rossato et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sandro Rossato on behalf of the Authors (24 Jul 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (29 Jul 2018) by David Lundbek Egholm
RR by Stefan Winkler (11 Aug 2018)
RR by Laura Stutenbecker (24 Aug 2018)
ED: Publish subject to technical corrections (28 Aug 2018) by David Lundbek Egholm
ED: Publish subject to technical corrections (03 Sep 2018) by Andreas Lang(Editor)
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Short summary
Glaciations may induce significant changes in the catchments of major sedimentary systems over time, even during a single phase. The rugged morphology of Alpine valleys may slow, block or divert glacial tongues. This conclusion arises from reconstructions made regarding the dynamics of the Brenta glacial system (northeast Italy). These reconstructions included sediment analysis techniques on the related alluvial stratigraphic record and mapping of in-valley glacial/glaciofluvial remnants.