Glazilimnische Kames in Schleswig-Holstein

Abstract

In the area of Weichselian glaciation in Schleswig-Holstein in the past years several occurrences of compared with their ein irons highly situated undisturbed basin sediments were found during geological mapping. Mostly occur silty clays, fine sand striped silts and silt striped fine sands, which during the ice decay were originally deposited in blanks in the glacier ice (dead ice), and became hills after the complete down melting of the glacier due to relief inversion. Three typical occurrences are described.