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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
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Volume 5, issue 3
Earth Surf. Dynam., 5, 331-345, 2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Earth Surf. Dynam., 5, 331-345, 2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 04 Jul 2017

Research article | 04 Jul 2017

Bayesian inversion of a CRN depth profile to infer Quaternary erosion of the northwestern Campine Plateau (NE Belgium)

Eric Laloy et al.
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Cited articles  
Beerten, K.: Toelichting bij de Quartairgeologische kaart, kaartblad (10-18) Beverbeek-Maaseik, Vlaamse Overheid, Departement Leefmilieu, Natuur en Energie, Brussel, 2005.
Beerten, K., Wemaere, I., Gedeon, M., Labat, S., Rogiers, B., Mallants, D., Salah, S., and Leterme, B.: Geological, hydrogeological and hydrological data for the Dessel disposal site. Project near surface disposal of category A waste at Dessel, NIROND–TR 2009–05 E V1, ONDRAF/NIRAS, Brussels, 2010.
Beerten, K., Dreesen, R., Janssen, J., and Van Uytven, D.: The Campine Plateau, in: Geomorphology of Belgium and Luxembourg, edited by: Demoulin, A., Springer Verlag, Berlin, in press, 2017.
Bogaart, P. W. and van Balen, R. T.: Numerical modeling of the response of alluvial rivers to Quaternary climate change, Glob. Planet. Change, 27, 147–163, 2000.
Braucher, R., Del Castillo, P., Siame, L., Hidy, A. J., and Bourlés, D. L.: Determination of both exposure time and denudation rate from an in situ-produced 10Be depth profile: A mathematical proof of uniqueness. Model sensitivity and applications to natural cases, Quat. Geochronol., 4, 56–67, 2009.
Publications Copernicus
Short summary
Over very long timescales, 100 000 years or more, landscapes may drastically change. Sediments preserved in these landscapes have a cosmogenic radionuclide inventory that tell us when and how fast such changes took place. In this paper, we provide first evidence of an elevated long-term erosion rate of the northwestern Campine Plateau (lowland Europe), which can be explained by the loose nature of the subsoil.
Over very long timescales, 100 000 years or more, landscapes may drastically change. Sediments...