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Tectonic contact between Paleozoic and Triassic rocks south of Podolseva, which passes prominent cliffs over the left bank of Savinja river (Klemenca pec, Jamnikova pec, Golerjeva pec, Strevceva pec and Huda pec), is on the basis of the new mapping a steep fault, dipping to the north. In the last phase, the fault was dextral strike - slip active, before was probably reverse, and can represent accompanying structure of Periadriatic lineament. It was under transpresive tectonic regime and complies with model of positive flower structure. We named it Podolsevski prelom (Podolseva fault).