Regionale Bodendifferenzierungen während der Würmeiszeit

Karl Brunnacker
The different structures of the Würm-Glacial loess-profiles seem to correspond to differences in the climatic differentiation of time and room with respect to the particular position. According to that, we may distinguish a profile-differentiation as well from dry to humid soils, as from a continental to an oceanic climate. In consequence of the climatic differentiation from dry to humid, with oscillations, the loess-facies increases in the course of the Würm-Glacial with one resp. two enclosed...