Reconstruction of the development history of karstic water networks on the southern part of the Gšmšr-Torna karst on the basis of ruined caves and landforms
Móga János - (28/2,1999)
The author demonstrates the surface development of the Gomor-Torna karst situated on the Hungarian-Slovakian border from the Tertiary until the present day. He follows the process of transition from the covered karst conditions to the open karst on the karst plateau, and its effect upon the landforms and the karstic water network. He studied the evolution of surface and sub-surface water networks, and the regularity of the movements of underground rivers based on water tracing. He reconstructed the ancient surface outflow directions of the covered karst from the scarce remains of the epigenetic valleys inherited from cover deposits onto the limestone surface, from ruined swallow hole lines in valleys, as well as from decaying water conducting tubes generated in earlier phases.