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

CONCLUSIONS

8. The caves in valley sides of the mountains have formed by the subsequent exposure of cavities originally formed in the zone of flowing karst water. In the mountains spring caves are not characteristic. Some small-scale spring may occur in the sides of blocks if karst storeys formed. At the outlets of main karst water small passages (eg. Tapolcafő) have not developed into spacious spring caves. No information is available on older spring caves formed higher than the present emergence level of main karst water.