Abstract
The karst of the horsts of the Bakony Region belonging to horst types of different development is described. Horsts elevated to the summit position are characterised by the most widespread and diverse karstification (with covered karst, cave-ins and shafts). Cryptopeneplains affect the karstification of horsts elevated to the summit position, but karst features also occur in their areas. On threshold surfaces of marginal position, the hypogene branches of regional flow systems influenced the development of spring caves. The karstification of basaltic mountains has been mainly governed by the properties of the basalt caprock (the major features being ponors with blind valleys and caprock dolines).
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