Table 2: The relation between the spatial position of the shafts surrounding Hárskút and the geological characteristics of their host rock.

Site and/or shaft State Shaft Characteristics of host rock Difference Shaft development
Type Direction Dip Direction of fracture, fault Bed
Dip direction Dip angle Along fracture Along bedding plane
Zsivány cave of Gyenespuszta Fossile, its doline is denuded Complex

60°-240° (a)

85°-265° (b)

130°-310° (c)

26° (a)

90° (b)

15° (c)

125°-305° 350° 15°

65 (a)

40 (b)

-

-

-

4° (c)

Along fracture (a,b) and bedding plane (c)
Doline marked G-5 Recent Simple

196°

-16°

45° ? 192° 42° - Along bedding plane
Kisharaszti-shaft (doline marked Gy-12) Recent Simple 177°-357° 90° 177°-357° 177°-357° 0°-5° - Along fracture
Doline marked H-1 Recent Simple 140°-320° 50°

2°-182°

134°-314°

123°-303°

11° 27° 13° - Along fracture or bedding plane
Doline marked Ho-1 (cave of Homód valley) Recent Complex 120°-300°

10° (a)

15° (b)

90° (c)

? 115° 11° ?

5° (a)-

5° (b)

-

Along fracture (c) and bedding plane (b,c)

Notice: Letters a, b, c indicate shaft parts with different position; ?: No data available.