On the age of the young morainic morphology in the area ascribed to the maximum extent of the Weichselian glaciation in north-eastern Germany

摘要: Abstract In this case study, the first numerical ages from area ascribed to maximum extent of Weichselian glaciation in north-eastern Germany are presented. The were derived fluvioglacial (sandur) sediments Luckenwalde using Optically Stimulated Luminescence dating techniques for quartz. reveal a primary formation outwash plain Warthe stage Saalian (130–150 ka) and limited reworking mainly linked meltwater activity during glaciation. Due insufficient zeroing OSL signal sediments, timing that event can only be determined by age around 35 ka. Nevertheless is accordance with results Beelitz cone, indicating an ice advance MIS 2. luminescence measurements supported additional stratigraphical petrographical findings. It likely considerable number landforms attributed originally age, partly overridden but not reshaped process. With transformation relief processes, implies very thin, probably warm-based cover fast paced short lived adapting pronounced morphology.