Geomorphological Mapping and Spatial Analyses of an Upper Weichselian Glacitectonic Complex Based on LiDAR Data, Jasmund Peninsula (NE Rügen), Germany

摘要: Glacitectonic deformation in the Upper Weichselian led to tectonic framework of large-scale folds and displaced thrust sheets Maastrichtian (Upper Cretaceous) chalk Pleistocene glacial deposits southwestern Baltic Sea region. They form surface expressions sub-parallel ridges elongated valleys between on Jasmund Peninsula. Geomorphological mapping detailed landform analyses give another insight into arrangement formation history these proglacial structures. Light detection ranging (LiDAR) digital elevation models (DEM) analysis techniques were applied a rather than subglacial environment. Results suggest division northern part with morphological striking NW–SE southern SW–NE trending ridges. The observation partly truncated northerly their superimposition by sub-complex that was generated earlier part. spatial tools used develop new, self-consistent genetic model integrating all parts 100 km2 large Complex. more consistent terminology for setting revised Jasmund, including three evolutional stages are characterized different ice flow patterns.