2. Late Pleistocene evolution of the Danube valley in the Visegrd Gorge.
Place: Verőce, Visegrad Gorge, Hungary
Aim: Identificating the fluvial terraces based on fluvial and eolian sediments. Complex geographical, geological, paleopedological – micromorphological and chronometrical investigations.
Methods: Chronometric dating (TL), complex lithostratigraphy, DEM and geomorphology, secondary carbonates analysis, cluster analysis, micromorphology, spectromorphometry and thermalanalysis.