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

Rossato, Sandro; Carraro, Anna; Monegato, Giovanni; Mozzi, Paolo; Tateo, Fabio

doi:https://doi.org/10.5194/esurf-6-809-2018

Articles | Volume 6, issue 3

https://doi.org/10.5194/esurf-6-809-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/esurf-6-809-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 6, issue 3

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, Anna Carraro, Giovanni Monegato, Paolo Mozzi, and Fabio Tateo

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Final revised paper (published on 26 Sep 2018)
Supplement to the final revised paper
Preprint (discussion started on 14 May 2018)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Manuscript esurf-2018-22 Lowlands fluvial sedimentation enlightens glacial dynamics in narrow valleys during the Last Glacial Maximum (Venetian Forealps, Italy) by Rossato et al.', Stefan Winkler, 19 May 2018
RC2: 'Review of ESurf-2018-22 by Rossato et al.', Laura Stutenbecker, 23 May 2018
AC1: 'Reply to reviewers', Sandro Rossato, 24 Jul 2018

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)

AR by Sandro Rossato on behalf of the Authors (04 Sep 2018) Manuscript

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.