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  • A hierarchy of geomorphic processes is set up including material transport due to rainwater (with varying intensities), neutral geomorphic evolution, landslides, deluvial or fluvial accumulation, deflation processes and lacustrine-paludal
  • The main findings of laboratory investigations are: in the two loess profiles the sedimentary layers and fossil soils are located at similar depths, but paludal processes are more intensive in the sequence below 73 m measured in 1979, than