Fig. 9
Map of the Loue River (a), its longitudinal profile (b) and ksn evolution (c). Lithological, karst and structural details have been reported on the along the Loue path. Knickpoints (red circles) have been located and classified in size by their intensities (ksn values). Each knickzone has been interpreted regarding geological, topographic and hydrological maps in term of potential lithological, structural, anthropogenic and karst forcing (color code, see legend on the figure). The Loue River is a karst river mainly fed by the Doubs River (Fig. 6). See Sect. 4.3 for further details