Articles | Volume 14, issue 2
https://doi.org/10.5194/esurf-14-191-2026
https://doi.org/10.5194/esurf-14-191-2026
Research article
 | 
16 Mar 2026
Research article |  | 16 Mar 2026

New experiments to probe the role of fractures in bedrock on river erosion rate and processes

Marion Fournereau, Laure Guerit, Philippe Steer, Jean-Jacques Kermarrec, Paul Leroy, Christophe Lanos, Hélène Hivert, Claire Astrié, and Dimitri Lague

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-1541', Alexander Neely, 01 May 2025
  • RC2: 'Comment on egusphere-2025-1541', Anonymous Referee #2, 10 Jun 2025
  • AC1: 'Comment on egusphere-2025-1541', Marion Fournereau, 18 Jul 2025

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Marion Fournereau on behalf of the Authors (21 Jul 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (31 Jul 2025) by Anastasia Piliouras
RR by Alexander Neely (18 Aug 2025)
RR by Anonymous Referee #3 (16 Sep 2025)
ED: Reconsider after major revisions (23 Sep 2025) by Anastasia Piliouras
AR by Marion Fournereau on behalf of the Authors (14 Nov 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (24 Nov 2025) by Anastasia Piliouras
RR by Alexander Neely (05 Dec 2025)
RR by Anonymous Referee #3 (22 Dec 2025)
ED: Reconsider after major revisions (08 Jan 2026) by Anastasia Piliouras
AR by Marion Fournereau on behalf of the Authors (04 Feb 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (21 Feb 2026) by Anastasia Piliouras
ED: Publish subject to technical corrections (26 Feb 2026) by Andreas Lang (Editor)
AR by Marion Fournereau on behalf of the Authors (05 Mar 2026)  Author's response   Manuscript 
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Short summary
River bedrock erosion can occur by abrasion and by the removal of entire blocks. We observe that when there is no or few fractures most erosion occurs by abrasion, whereas with more fractures, blocks can be removed at once leading to different patterns of erosion and riverbed morphology. Fractures affect barely mean erosion rate but change the location and occurrence of block removal. Our results highlight how river bedrock properties influence erosion processes and thus landscape evolution.
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