The object of this study was to develop methods for investigating recent geomorphodynamics of aggradation processes on debris flow cones, alluvial cones and braided gravelbed streams by dendrogeomorphological analyses of the stems and the roots
In the Bayerischer Wald, where no tephra occures, the AA. try to reconstruct the late-glacial geomorphodynamic by radiocarbon-dating of peats, which are stratified with the periglacial slope deposits, by IRSL-dating and in combination with moraines