Articles | Volume 13, issue 4
https://doi.org/10.5194/esurf-13-629-2025
https://doi.org/10.5194/esurf-13-629-2025
Research article
 | 
28 Jul 2025
Research article |  | 28 Jul 2025

Late Pleistocene–Holocene denudation, uplift, and morphology evolution of the Armorican Massif (western Europe)

Oswald Malcles, Stéphane Mazzotti, Philippe Vernant, and Vincent Godard

Data sets

Isopaques de bancs sableux en Mer du Nord, Manche et Atlantique Claude Augris et al. https://doi.org/10.12770/75AD486F-9D03-4FEB-B742-BE6C6F791345

Isopaques de couverture indiff\'{e}renci\'{e}e en Mer du Nord, Manche et Atlantique Claude Augris et al. https://doi.org/10.12770/C841CA37-B414-4C51-AD6A-16BC34E8CF6F

Isopaques de nappes alluviales en Mer du Nord, Manche et Atlantique Claude Augris et al. https://doi.org/10.12770/6C4CCD44-71B1-411D-91D1-ECCD1B2A46F1

Model code and software

Open-source modular solutions for flexural isostasy: gFlex v1.0 (https://github.com/awickert/gFlex) A. D. Wickert https://doi.org/10.5194/gmd-9-997-2016

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Short summary
The Armorican region (NW France) is marked by several old coastal and marine markers that are today located several tens of meters above sea level. This fact is commonly explained by sea-level variations and complex tectonic processes (e.g., mantle dynamics). In this study, we test the role of the erosion and the associated flexural (lithospheric bending) response. We show that this simple model of flexural adjustment is to be taken into account to explain the regional evolution.
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