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

KARSTIFICATION

Fig. 31. Cross-sections (I) and plan views (II) of some characteristic cave remnants Legend: 1. enclosing rock; 2. spherical cauldron; 3. channel; 4. debris; 5. soil, weathering residue; 6. rock wall with depth; 7. slope of entrance; a. cave remnant exposed by stream erosion (C-3 or Rejtett-fülke, Cuha Valley); b. cave remnant with several entrances exposed by the denudation of the valley side (K-8 or Kovölgy-sziklaüreg); c. cave remntant exposed by denudation of valley side and eroded into ruined cave remnant (Km-1 or Átjáró Cave, Csesznek); d. cave remnant exposed by denudation of valley side and eroded into ruined cave remnant (M-4 or Likas-kő, Magos Hill); e. cave remnant exposed by the denudation of fault scarp and divided into ruined and truncated cave remnants (M-5 or „Csapóné konyhája"); f. cave remnant exposed by denudation of the valley side and divided into ruined cave remnants (C-4 or Remete-lik). Cave maps from reports of the Cholnoky Caving Group for 1977 and 1978 ches or ceiling remnants (Pict. 43; Fig. 36). Truncated or ruined cave remnants of some metres' length will come about. The cave remnants which lose their ceilings entirely became cave ruins (Picts. 44, 45), bordered by steep rock walls on all sides. They are common features and there are hundreds or even a thousand of them in the valley walls of the Ördög-árok. According to their groundplan they are of corridor or chamber nature. Cave ruins also originate from cavedin subsurface cavities which do not form a feature without drainage, ie. a collapse doline (VERESS-FUTÓ 1987, Figs. 32,33).