Figure 10. Faults in the Pannonian deposits (photograph by A. Grachev). A system of small normal faults in deposits of the upper Pannonian (Mt. Kish-Hedis-te, Hungarian Midmountains). Motions are largest on fault planes with a dip azimuth of 310o and dip angles of 45-50o. It is noteworthy that Pannonian deposits are intact in the quarry wall orthogonal to the photo plane. A step normal fault in deposits of the upper Pannonian is seen to the right (a quarry in the Himeshhaza village area east of the town of Pecs).