Veress Márton: A Bakony természettudományi kutatásának eredményei 23. - Covered karst evolution... (Zirc, 2000)

KARSTIFICATION

Mg. 42. Morphology or block with row or cones, tilted unidirectionally (bgett Hill, VERESS lyyl) Legend: 1. contour line; 2. semiexhumed cone; 3. exhuming cone; 4. exhuming relict terrain; 5. pseudodepression; 6. reworking; 7. karst depression; 8. water conduit in karst depression cones is of moderate scale since only small amounts of sediment from valley floors above the sites of karstification are transported beyond the cone (by overflow) and also because karst depressions are only able to store small amounts of sediment. On the summit level of the exhumed cone subsidence dolines sometimes also occur. This subtype of karstification is typical of eg. the Szilfakő Valley in the central Hárskút Plateau (Pict. 13). - During longitudinal exposure the valley forms either above or between cones. In the former case, the sides of inactive well-developed superimposed valleys formed in unconsolidated deposits erode rapidly. Thus, the background area for karst depressions on the valley floor is destroyed and, therefore, the depressions are truncated (Fig. 49), their water