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  • It was established that each type of soil can be characterised by a specific distribution of mineral phases with definite structural-mineralogical indications being inherited from its parent material and syngenetic with soil formation
  • of past cryogenic features has a practical side as well. Extant landforms on loess areas often may only be explained with active cryogenic processes preceding loess deposition.
  • to determine the vegetation and other conditions during the deposition of loess it is important to take into consideration the palaeofloristic data as well.
  • by their grain size parameters and their carbonate content. Parallel to these genetic units the sequence was subdivided from a faunistic point of view, too. The results correlate well with those of the numeric approach.