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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, 125-143, 2017
http://www.earth-surf-dynam.net/5/125/2017/
doi:10.5194/esurf-5-125-2017
© Author(s) 2017. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
21 Feb 2017
Autogenic versus allogenic controls on the evolution of a coupled fluvial megafan–mountainous catchment system: numerical modelling and comparison with the Lannemezan megafan system (northern Pyrenees, France)
Margaux Mouchené et al.
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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: 'Referee report', Anonymous Referee #1, 09 Sep 2016 Printer-friendly Version 
AC1: 'Answer to RC1: 'Referee report', Anonymous Referee #1, 09 Sep 2016', Margaux Mouchene, 23 Sep 2016 Printer-friendly Version 
 
RC2: 'Review of Mouchené et al., on the Lannemezan Fan', Hugh Sinclair, 17 Nov 2016 Printer-friendly Version 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Margaux Mouchene on behalf of the Authors (09 Jan 2017)  Author's response  Manuscript
ED: Publish as is (24 Jan 2017) by Pr. Sebastien Castelltort
ED: Publish as is (30 Jan 2017) by Prof. Niels Hovius (Editor)  
Publications Copernicus
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Short summary
The Lannemezan megafan (northern Pyrenean foreland) was abandoned during the Quaternary and subsequently incised. We use numerical models to explore possible scenarios for the evolution of this megafan. We show that autogenic processes are sufficient to explain its evolution. Climate may have played a second-order role; in contrast base-level change, tectonic activity and flexural isostatic rebound do not appear to have influenced its evolution.
The Lannemezan megafan (northern Pyrenean foreland) was abandoned during the Quaternary and...
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