Now back on Czech territory, the fault more or less follows the crest line of the Jeschken Mountains. At the Ještěd (Jeschken) is the highest point on the fault line, a topographical dominant that is visible from a long way off. The fault then runs eastwards, almost in a straight line, along the Ještěd-Kozákov Ridge - interrupted by the valleys of the Mohelka and the Jizera - to Kozákov in the Bohemian Paradise. In Malá Skála is the most notable geological outcrop along the fault, the Suché skály. Here the once horizontal sandstone beds were tilted vertically by the pressure of the fault and, today, form an impressive rock formation.