Die Entwässerung der Baltischen Eisrandlagen im mittleren Norddeutschland

R. Brinkmann
Measurements of current bedding in würmian fluvioglacial sediments point to a general northerly slope in north-eastern Mecklenburg. This observation suggests a backward subglacial drainage of the ice in the later stages of the last glaciation and offers an explanation for the different development of outwash plains in the Frankfurt and Pommern stages.