Fig. 3From: Deciphering neotectonics from river profile analysis in the karst Jura Mountains (northern Alpine foreland)Schematic map of the northern Alpine river network organization from the Late Miocene (13.6–10 Ma) to present-day, modified from Ziegler and Fraefel (2009) and Giamboni et al. (2004a, b). a the entire Alpine foreland drained southwestward during the Late Miocene; b northeast deflection of the Swiss Molasse river network in response to the incipient Jura folding; c capture of a part of the Doubs, Danube and Rhine rivers in response of Upper Rhine Graben subsidence, and karst interactions (see Sect. 2.1.2 for further details)Back to article page