Zur stratigraphischen Gliederung der jungpleistozänen Sedimente im nördlichen Oberrheintalgraben

Erich Becker
In the Quarternary the northern Upper Rhine rift valley was filled with the fluviatile deposits (pebbles and sands) of the rivers Rhine, Main and Neckar. During the Würm ice age and in the Holocene the surface of these fluviatile deposits was covered with eolian sand plains and dune fields of varying thickness and extension. The most complete stratigraphie sequence of the eolian cover was found in the Lower Main district. In this region the eolian...