Articles | Volume 15, issue 6
https://doi.org/10.5194/tc-15-2889-2021
https://doi.org/10.5194/tc-15-2889-2021
Research article
 | 
28 Jun 2021
Research article |  | 28 Jun 2021

Formation of ribbed bedforms below shear margins and lobes of palaeo-ice streams

Jean Vérité, Édouard Ravier, Olivier Bourgeois, Stéphane Pochat, Thomas Lelandais, Régis Mourgues, Christopher D. Clark, Paul Bessin, David Peigné, and Nigel Atkinson

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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
ED: Publish subject to revisions (further review by editor and referees) (31 Mar 2021) by Delphine Lannuzel
AR by Jean Vérité on behalf of the Authors (31 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to revisions (further review by editor and referees) (06 May 2021) by Delphine Lannuzel
AR by Jean Vérité on behalf of the Authors (06 May 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (09 May 2021) by Delphine Lannuzel
RR by Richard C.A. Hindmarsh (25 May 2021)
RR by Martin Ross (27 May 2021)
ED: Publish subject to minor revisions (review by editor) (28 May 2021) by Delphine Lannuzel
AR by Jean Vérité on behalf of the Authors (28 May 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (03 Jun 2021) by Delphine Lannuzel
AR by Jean Vérité on behalf of the Authors (03 Jun 2021)  Author's response   Manuscript 
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Short summary
Subglacial bedforms are commonly used to reconstruct past glacial dynamics and investigate processes occuring at the ice–bed interface. Using analogue modelling and geomorphological mapping, we demonstrate that ridges with undulating crests, known as subglacial ribbed bedforms, are ubiquitous features along ice stream corridors. These bedforms provide a tantalizing glimpse into (1) the former positions of ice stream margins, (2) the ice lobe dynamics and (3) the meltwater drainage efficiency.