H. dr. Harmat Beáta (szerk.): A Bakonyi Természettudományi Múzeum Közleményei 20. (Zirc, 2001-2003)

VERESS MÁRTON: Adalékok a homokkő anyagú kőtengerek (Káli-medence) pszeudokarrjainak morfogenetikájához

Figure 17: Gravel-size distribution along the cross-section A-Ä and B-B' on a boulder surface (Szentbékkállai-block field) Legend: 1. The longest axis of the gravel measured along the cross-section (cm) 2. The mean value of the longest axes of the gravels (cm) 3. Moss Figure 18: The depths of the kamenitzas, developed on the surface of the sandstone and sandstone with conglomerate of Szentbékkálla, as a function of their avarage horizontal size. B. Realiability K. Correlation coefficient S. Error varience Figure 19: The depths of the kamenitzas, developed on the surface of fine-grain-, and fine-medium grain conglomeratal of Szentbékkálla as a function of their avarage horizontal size. B. Realiability K. Correlation coefficient S. Error varience Figure 20: The depths of the kamenitzas, developed on the surface of the medium-grain conglomeratal of Szentbékkálla, as a function of their avarage horizontal size. B. Realiability K. Correlation coefficient S. Error varience Figure 21: The depths of the kamenitzas, developed on boulders smaller than 1.5 m

2 in their horizontal size of Salföld, as a function of their avarage horizontal size. B. Realiability K. Correlation coefficient S. Error varience Figure 22: The depths of the kamenitzas, developed on boulders bigger than 1.5 m

2 in their horizontal size of Salföld, as a function of their avarage horizontal size. B. Realiability K. Correlation coefficient S. Error varience Figure 23: The depths of the pipes, developed on boulders smaller than 1.5 m

2 in their horizontal size of Salföld, as a function of their avarage horizontal size. B. Realiability K. Correlation coefficient S. Error varience Figure 24: The depths of the pipes, developed on boulders bigger than 1.5 m

2

in their horizontal size of Salföldas a function of their avarage horizontal size. B. Realiability K. Correlation coefficient S. Error varience Figure 25: The development of some pseudokarren forms of the blockfields Legend: a. The development of the forms, with different grain size. b. The development of the form if they develop in fine-grain conglomerate and sandstone, c. The development of the form, if it develops in such two fine-grain conglomeratal beds, which are separated by a sandstone band. d. The development of the forms if the dip direction of the surface of the boulder and the dip direction of the different size-grain beds differ from each other by 90°. e. Steps can develop if between the dip direction of the surface of the boulder and the dip direction of the different size-grain beds are differ from each other by 180°. f. Solutional notches, pockets, tafonis can develop if the dip direction of the wall of the boulder and the dip direction of the different size-grain beds differ from each other by 180°. I. Original state II. Current state fa. From above, p: Profile, 1. Sandstone 2. Fine-grain conlomerate 3. Medium-grain conglomerate 4. Precipitated silica 5. Soil, non-cementated material 6. Joint 7. The dip of the boulder 8. The lake of the kamenitza 9. Outflowing water 10. Water percolating into the rock 11. Water drainage from the boundary surface to the boulder, drainage from the boulder 12. Kamenitza has gently side 13. Kamenitza has steep side 14. The