Morphological analysis of the drainage system in the Eastern Alps

• Published in: Tectonophysics Vol. 460; no. 1; pp. 263 - 277
• Main Authors: Robl, Jörg, Hergarten, Stefan, Stüwe, Kurt
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 15.11.2008
• Subjects: channel profiles; drainage network; Eastern Alps; erosion modelling; glacial impact on the drainage system; reorganisation of the drainage network; stream power modelling; uplift of the Eastern Alps; Europe, Danube R; Europe, Pannonian Basin; Europe, Rhine Graben; Europe, Rhine R; drainage network; stream power modelling; uplift of the Eastern Alps; Eastern Alps; reorganisation of the drainage network; channel profiles; glacial impact on the drainage system; erosion modelling
• ISSN: 0040-1951; 1879-3266
• DOI: 10.1016/j.tecto.2008.08.024

We study the morphology of the major rivers draining the Eastern Alps to test whether the active tectonics of this part of the orogen is reflected in the shape of channel profiles of the river network. In our approach we compare channel profiles measured from digital elevation models with numerically modelled channel profiles using a stream power approach. It is shown that regions of high stream power coincide largely with regions of highest topography and largest uplift rates, while the forelands and the Pannonian Basin are characterised by a significantly lower stream power. From stream power modelling we conclude that there is young uplift at the very east of the Eastern Alps, in the Bohemian Massif and in the Pohorje Range. The impact of the Pleistocene glaciations is explored by comparing properties of rivers that drain in proximal and distal positions relative to the ice sheet during the last glacial maximum. Our analysis shows that most knick points, wind gaps and other non-equilibrium features of catchments covered by ice during the last glaciations (Salzach, Enns) can be correlated with glacial processes. In contrast the ice free catchments of the Mur and Drava are characterized by channels in morphological equilibrium at the first approximation and are showing only weak evidence of the strong tectonic activity within these catchments. Finally, the channel profiles of the Adige and the divide between the upper Rhine and Danube catchments differ significantly from the other catchments. We relate this to the fact that the Adige and the Rhine respond to different base levels from the remainder of the Eastern Alps: The Adige may preserve a record from the Messininan base level change and the Rhine is subject to the base level lowering in the Rhine Graben.