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  • Lake Balaton being a recreation area of international significance, research on the influx of sediments and solutes as well as on pollution and eutrophication is very important. Methods include a detailed analysis of a test area typical for the N
  • The research was focused mainly on surveying lake deposits, as well as the morphology and structure of the Pre-Quaternary lake deposits and the morphology and structure of the Pre-Quaternary basement of Lake Balaton. Paleontological investigations
  • (pollen, diatoms, ostracods) in the 4 subbasins of the lake allowed the reconstruction of the ecological history of the area as well providing detailed stratigraphic information. Radiocarbon dating of peat helps to date the beginning of lake formation
  • related to topography as well as to the type of cultivation since the beginnings of collectivization.
  • influences on present-day slope evolution : rocks, geological structure, slope parameters, drainage and human pressure. A detailed mapping of the area and map analyses have proven that the diversity of slope evolution is reflected by morphodynamics as well