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- W2005707325 abstract "In the Touques drainage basin, five alluvial terraces have been distinguished. A multiscale approach in a continental basin was undertaken, combining different stratigraphic and geomorphic analyses. Stratigraphic and sedimentologic analyses play an essential role, because of the interaction between climate and sea-level variations and tectonics. In the Touques valley, the alluvial sheets cover the Middle and Upper Quaternary. Each fluvial sequence is correlated with a glacialinterglacial climatic cycle. The numerous episodes of channel entrenchment and terrace formation arise from a Quaternary regional uplift. Valuable information is obtained through detailed analysis of the morphology (morphometric and drainage pattern analyses). The longitudinal profiles of the rivers and the hypsometric integrals are related to the immaturity of the drainage basins subjected to recurrent sea-level changes. Dans le bassin versant de la Touques, les changements climatiques durant le Quaternaire et les mouvements verticaux sont décryptés par des indices stratigraphiques et par la géométrie des nappes fluviatiles ainsi que du réseau hydrographique. Nous présentons la réponse d'un milieu fluviatile aux rythmes de l'érosion et de la sédimentation en caractérisant la part due aux contrôles climatique et tectonique. La succession de phénomènes d'érosion et de dépôt, liée au glacio-eustatisme et à une surrection tectonique constante, est à l'origine de l'étagement des terrasses et de l'instabilité récurrente des versants de la Touques." @default.
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- W2005707325 date "1998-05-01" @default.
- W2005707325 modified "2023-09-25" @default.
- W2005707325 title "Évolution géomorphologique d'un bassin versant côtier: l'exemple de la Touques (Basse-Normandie)" @default.
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- W2005707325 doi "https://doi.org/10.1016/s1251-8050(98)80251-6" @default.
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