High stone above Stárkov

Above Stárkov, a high and steep slope rises from the valley of the Dřevíče stream along its left bank, formed by mudstones (marbles) of the lower to middle Turonian. In the upper part there is a significant cleft with a length of more than 100m and a width of 5-15m. It creates a rocky gorge parallel to the direction of the slope. The wall of the dividing surface of the block slide is up to 20m high, divided into separate rock towers. The bottom of the fissure covers…