Ist der Oberharz im Pleistozän vergletschert gewesen?

Klaus Duphorn
Thip paper deals with results concerning the problem of Pleistocene glaciation in the Harz Mountains. These results obtained by geological mapping in the upper Oder Valley proove the existence of a local glacier in the Pleistocene. Primarily the field work in the Oder Valley was concentrate to four end moraine lobes and to the deposits connected with them. This area can be subdivided into the following geological/ morphological units: 1) Proglacial outwash plain, 2) end...