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

Legend: a. Kamenitza develops, which can increase reverse to the slope line, its water is carried by widening Rinnens. b. As a consequence of kamenitza growth the original surface will only be retained on the upper margin of the boulder since truncated little hills will remain on the surface between rinnen. 1. Boulder 2. Surface bordering sedimentary boulder 3. Kamenitza 4. Rinnen 5. Upper margin of the boulder non-truncated 6. Truncated part of the boulder 7. Margin inselbergs of the margin zone 8. Denudational little hills of lower part of the boulder truncated by solution 9. Solutional depression (Rinnen?) separating marginal „inselbergs" Figure 12: Morphological map of the Szentbékkalla-block field with the sites investigated Legend: 1. Fractured rock 2. Group of different boulders (at least 4 m in size) 3. Separate group of the boulders (up to 4 m in size) 4. Sandstone surface dissected by crevices which rises 0,5 m above its surroundings 5. Group of little bit tilted boulders which rise above the surface by 0,2-1 m 6. Evenly developed rock surface with soil cover in patches 7. Evenly developed rock surface with soil or sediment cover, with occasional sandstone outcrops 8. Quarrying surface 9. Contour line 10. Joint, crevasse 11. The boundary of different type block fields 12. The cross-section from the side of the boulder 13. The cross-section from the pseudokarren features 14. Gravel size investigation along the cross-section 15. Site of the morphological map using a planimetric map 16. Site of the morphological map where the measuring was performed with implement 17. Rock sampling site 18. Water sampling site Figure 13: The cross-section from the side wall of the boulder (Szentbékkállai-block field) Legend: a. View from above: 1. Corridor 2. The slope line of dip 3. Line of the crosssection (with direction) 4. Soil and vegetation b. In profile 5. Medium-grain conglomerate 6. Fine-grain conglomerate 7. Sandstone 8. Spherical hollow (tafoni) 9. Solutional platform 10. Soil a The direction of dip of the bands Figure 14: Cross-section of a side of the boulder (Szentbékkállai-block field) Legend: 1. Medium-grain conglomerate 2. Fine-grain conglomerate 3. Sandstone 4. Soil 5. Solutional platform 6. Kamenitza a the direction of dip of the bands Figure 15: Sandstone polygonal forms from a boulder (Szentbékkállai-block field) Legend: 1. Margin of the boulder 2. 'Semi-pipe' 3. Rinnen 4. Kamenitza 5. Open kamenitza 6. Sandstone conical (pseudokarren „inselberg") 7. Sandstone polygonal from (the crevasses of the sandstone are less than 1 cm) 8. Sandstone polygonal form (the width of the crevasses of the sandstone are between 1-3 cm) 9. Soil 10. Angle of dip and angle of direction of the boulder Figure 16: Morphological map of a boulder (Szentbékkállai-block field) Legend: 1. Side of the boulder with depth data (m) 2. Countour line 3. Joint 4. Angle of the direction of the surface of the boulder 5. Kamenitzas with depth (cm) 6. Inner kamenitza 7. Gently sloping side of the kamenitza 8. Vertical sloping side of the kamenitza 9. Overhang of the kamenitza 10. Ridge between the kamenitzas 11. Rinnen 12. Lower vegetation (moss, lichen) 13. Graminous vegetation 14. Cross-section (where specific solution is calculated) 15. Cross-section (along which the longest axis of the gravels are measured in a 5 cm sequence)