The Tübingen research group of the MABIS project examined mass movements on the Swabian Jurassic escarpment, the Keuper cuesta and the glacially formed Deggenhausen valley, using geomorphologic and pedologic field mapping, differentiation
Geomorphologic and pedologic field mapping, differentiation of solifluction layers and mineralogical analyses were employed to examine the mass movements. The goal of the investigations was to distinguish between Holocene and Pleistocene landslides