Befunde zur spätglazialen fluvial-limnischen Morphodynamik in kleinen Talungen Vorpommerns

Henrik Helbig & Pim De Klerk
The data presented in this study result from investigations in a gas-pipeline ditch north of the Pomeranian terminal moraines crossing the till plains of the Mecklenburgian stade. Small valleys and basin, dominated by peat formation during the Alleröd, were filled with minerogenic sediments (mainly fine sand, often with silt portions) during Dryas-III. This period, in comparison with the preceding Alleröd, is characterized by, at least seasonally, higher discharges, substantial higher water tables (about 1 to...