Articles | Volume 9, issue 4
https://doi.org/10.5194/esurf-9-795-2021
https://doi.org/10.5194/esurf-9-795-2021
Research article
 | 
29 Jul 2021
Research article |  | 29 Jul 2021

Tectonically and climatically driven mountain-hopping erosion in central Guatemala from detrital 10Be and river profile analysis

Gilles Brocard, Jane Kathrin Willenbring, Tristan Salles, Michael Cosca, Axel Guttiérez-Orrego, Noé Cacao Chiquín, Sergio Morán-Ical, and Christian Teyssier

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Cited articles

Anderson, T. H., Burkart, B., Clemons, R. E., Bohnenberger, O. H., and Blount, D. N.: Geology of the Western Altos de Cuchumatanes, Northwestern Guatemala, Geol. Soc. Am. Bull., 84, 805–826, https://doi.org/10.1130/0016-7606(1973)84<805:gotwac>2.0.co;2, 1973. 
Attal, M., Tucker, G. E., Whittaker, A. C., Cowie, P. A., and Roberts, G. P.: Modeling fluvial incision and transient landscape evolution: Influence of dynamic channel adjustment, J. Geophys. Res., 113, F03013, https://doi.org/10.1029/2007jf000893, 2008. 
Authemayou, C., Brocard, G., Teyssier, C., Simon-Labric, T., Guttierrez, A., Chiquin, E. N., and Moran, S.: The Caribbean-North America-Cocos Triple Junction and the dynamics of the Polochic-Motagua fault systems: Pull-up and zipper models, Tectonics, 30, TC3010, https://doi.org/10.1029/2010tc002814, 2011. 
Authemayou, C., Brocard, G., Teyssier, C., Suski, B., Cosenza, B., Moran-Ical, S., Gonzalez-Veliz, C. W., Aguilar-Hengstenberg, M. A., and Holliger, K.: Quaternary seismo-tectonic activity of the Polochic Fault, Guatemala, J. Geophys. Res.-Sol. Ea., 117, B07403, https://doi.org/10.1029/2012jb009444, 2012. 
Babault, J., Van Den Driessche, J., Bonnet, S., Castelltort, S., and Crave, A.: Origin of the highly elevated Pyrenean peneplain, Tectonics, 24, TC2010, https://doi.org/10.1029/2004TC001697, 2005. 
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Short summary
The rise of a mountain affects the circulation of water, both in the atmosphere and over the land surface, thereby affecting the erosion of the land surface. We document how the rise of a mountain in central Guatemala has affected the erosion of an older range nearby. The new range intercepts precipitation formerly delivered to the older range. River response to the uplift of the new range has decreased incision across the older one. Both have reduced hillslope erosion over the old range.
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