Sedimentological and lithostratigraphical investigations in the gravel pit "Hinterste Mühle" at Neubrandenburg, northeastern Germany
The investigated gravel-pit lies in the hinterland of the Pomeranian end-moraine zone. The structures in the sediment are strongly influenced during the glacier's recession. Especia11y the margins of the pit show strong deformation. Until now the sediments have been interpreted as subglacial tunnel deposits. Moreover the whole sequence is considered to be discontinuous. It has been suggested t