This paper deals with red clays in Hungary, which are younger than the Upper Pannonian (Upper Miocene) but older than the Pleistocene. Their origin and stratigraphical position is still debated. Based on geomorphological position and mineralogical
Geomorphology and drainage of the S-Gömör-Torna karst region in view of an environmental hazard
Geomorphology and changing environments in Central Europe
The geomorphology and underground drainage of the Szilice and Alsó-hegy (Lower Plateau) have been studied within a long-term project in order to estimate the extent of ecological risks. With knowledge on geomorphological-hydrological links
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
Multi-phase geomorphological evolution of the Keszthely Mountains (SW-Transdanubia) and karstic recharge of the Hévíz lake
Geomorphology and changing environments in Central Europe
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
Through the interpretation of sedimentological, geomorphological, paleoclimatic and tectonic information the geomorphic evolution of the Transdanubian Mountains from the Cretaceous to the Quaternary is presented. Several sedimentary cycles occurred
Geomorphology and changing environments in Central Europe
This paper investigates how geomorphological conditions and human activities influence the extent of nitrate contamination of groundwater. An attempt was made to plot a map of nitrate-contamination hazard. The areal distribution of heavy metal
Geomorphology and changing environments in Central Europe
Until recently only geomorphological features and mammal fossils had been known as evidence to the long-debated dry-warm semidesert or hot desert climate in the Carpathian basin following the filling up of the Pannonian Lake. A comparison of samples
Geomorphology and changing environments in Central Europe
. The A. investigates the area where the density of dolines is highest and investigates the relationships between doline occurrence and geological/geomorphological conditions.