Stratigraphy of Late Quaternary fluvial terraces at the confluence of the Lech and Danube valleys

Patrick Schielein, Gerhard Schellmann & Johanna Lomax
The main purpose oft the study is the Würmian Lateglacial and Holocene valley development at the confluence of the Lech and Danube valleys, located in the Northern Alpine Foreland. The morphological features in the study area were surveyed by field mapping and high resolution Digital Elevation Models. The deposits of both rivers were examined in numerous outcrops and dated using radiocarbon and luminescence measurements. Also archaeological data and historical maps were taken into account. The...