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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union

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Earth Surf. Dynam., 5, 161-186, 2017
https://doi.org/10.5194/esurf-5-161-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
28 Feb 2017
River profile response to normal fault growth and linkage: an example from the Hellenic forearc of south-central Crete, Greece
Sean F. Gallen and Karl W. Wegmann
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Review comments', Sarah Boulton, 21 Dec 2016 Printer-friendly Version 
AC1: 'Response to review by Dr. Sarah Boulton', Sean Gallen, 31 Dec 2016 Printer-friendly Version Supplement 
 
RC2: 'Comment', Mary Ford, 12 Jan 2017 Printer-friendly Version 
AC2: 'Response to review by Dr. Mary Ford', Sean Gallen, 13 Jan 2017 Printer-friendly Version Supplement 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sean Gallen on behalf of the Authors (13 Jan 2017)  Author's response  Manuscript
ED: Publish as is (30 Jan 2017) by Francois METIVIER  
ED: Publish as is (31 Jan 2017) by Niels Hovius (Editor)  
CC BY 4.0
Publications Copernicus
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Short summary
We present results from a natural experiment where bedrock rivers are adjusting to a step change in rock uplift rate and where constraints on the recent pattern of rock uplift exist. We show that while rivers record the relative rock uplift history, quantitative information on timing is masked by complexities in incision processes, changes in river network configuration, and possibly other factors. Our results emphasize caution when interpreting tectonic signals from some bedrock river systems.
We present results from a natural experiment where bedrock rivers are adjusting to a step change...
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