Zur Gliederung des Auelehms im Flußgebiet der Weser

Gerd Lüttig
While making new geological maps of some parts of the Weser river area, the Holocene of this river and his affluents has been mapped. The flood loam („Hochflut- or Auelehm") could be divided into at least three different formations. The sedimentation of the oldest flood loam begins in each area at different times, but usually it is at work in the second half of the Atlanticum, and ends at the beginning of the Subatlanticum. Two...