Lithologie, Stratigraphie und Paläoökologie des Mittelpleistozäns von Uichteritz im Markröhlitzer Tal (Lkr. Weißenfels/Sachsen-Anhalt)

Stefan Meng & Stefan Wansa
The river history of the Markröhlitz valley has been discussed for about 100 years. New litho-logical and malacological studies of the Pleistocene sequence in the Uichteritz gravel and sand pit allow one to distinguish three fluvial gravel units. The fluvial gravel units are characterised by different structures, pebble assemblages and weathering. The gravel units are separated by silt layers (oxbow sediments, flow material) and alluvial fan deposits. The Lower Gravel Unit is free of Nordic...