Search

The area of the Polická basin is in fault and tectonic structures region. Neotectonic and recent long-term movements occur along the geomorphological systems. Endogenous and exogenous processes are the main reason of tectonic activity in the area. Polická basin and its look is influenced by geomorphological processes and represents a perfect region for the study of active fault structures. This area is influenced by physical-geographic characteristics of the region and reflects with long-term processes which determine the development of this area. Two large systems of Polický and Skalský fault run across the selected area. The course of these systems is confirmed by previous studies, and it is indicated in geological maps. The area of faults crosses is area with the most affected geomorphological elements of the relief. Ostaš, Hejda and Kočičí skaly mesas is greatly influenced by Polický fault zone, mainly due to fault close location to the selected geomorphological surface forms. Result of the fault zones pressure is observed on various structures and their form. During the relief and surface features analysis and examination were used various methods, which confirmed the influence of fault zones. The fracture systems showed the same orientation as the Polický fault orientation (SSE - NNW)....