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  • Macromorphologically, the study area in Pannonian Croatia is basically a mountain-and-basin region. Geologically, it is on the W border of the Pannonian Basin, in contact with Forealpian structures. Special importance is rendered to tectonic
  • movements in the origin of geological and geomorphological features. Various types of structures have been selected for study and recognised as particular types of morphostructure. Examples of relief properties suggest a relationship between orography
  • , geological structure and faults. The consequences of extension, compression and transgression, especially along transcurrent faults are investigated.
  • 1997
  • Environmental geological research in the Lake Balaton region
  • 1997
  • Geological structure ; Hungary ; Lithology ; Periglacial features ; Plant cover ; Pleistocene ; Slope exposure ; Slope gradient ; Soil water
  • between individual factors : geological structure, rocks, slope type and exposure, early Pleistocene topography, climatic conditions and percentage vegetation cover. Under identical conditions it was found that there is a striking regional asymmetry
  • 1997
  • The A. draws a clear distinction between relief classification and typology. Relief types are units clearly delimited in space, which show characteristic features of the groups theoretically formed by classification criteria (geological conditions
  • 1997
  • in the hydrogeological system of the Hévíz lake. The paleogeographical reconstruction was based on large-scale geological models. A special attention was paid to the geomorphological control on sedimentation and karstification. The consequences of differential erosion
  • 1997
  • 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
  • 1997
  • . The A. investigates the area where the density of dolines is highest and investigates the relationships between doline occurrence and geological/geomorphological conditions.
  • 1997