FLEURY , Jules

The evolution of continental relief results from the combined action of tectonic and climatic forcings. These processes do not act continuously but often through punctual events (earthquakes, major floods, landslides) whose integrated action over time (100 Kyr to Myr) leads to the formation of landscapes. The distribution of these extreme...

Abstract. Long-term landscape evolution is controlled by tectonic and climatic forcing acting through surface processes. Rivers are the main drivers of continental denudation because they set the base level of most hillslopes. The mechanisms of fluvial incision are thus a key focus in geomorphological research and require accurate...

Investigating landscapes evolution and their responses to tectonic or climatic perturbation requires accurate representations and models of surfaces processes. Rivers are keys agents of the transmission of external forcing through landscape and the main drivers of continental denudation. For these reasons the mechanisms of fluvial incision have...

L'évolution des paysages résulte de l'action conjointe des forçages tectoniques et climatiques. Ces processus n'agissent pas de manières continus mais via des événements ponctuels (séismes, glissements de terrains, crues majeurs) qui, intégrés sur des temps longs conduisent à la formation des reliefs. L'incision fluviale contrôle la dénudation...

The Provence region, located in the south-east of France, has experienced a few destructive earthquakes during the last centuries, such as the 1909 Lambesc earthquake or the 1509 and 1708 Manosque earthquakes. However, faults in the area experience slow slip rates (< 0.1 mm/yr) that preclude quantification of deformation using geodetic...