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J. Golonka, M. Krobicki, A. Waśkowska, M. Cieszkowski & A. Ślączka reply: We welcome the comments by our Slovakian colleagues and their critique of our results, particularly as we have discussed and published papers together several times about our ideas, sometimes, more or less, disputable (Aubrecht et al. 2003, 2006; Krobicki et al. 2003; Krobicki, Aubrecht & Golonka, 2003; Golonka et al. 2006; Pieńkowski et al. 2008). We are pleased to see such warm reaction to our work/paper, which is focused on one of the rudimentary questions in the Pieniny Klippen Belt (PKB) area. How many/what kind of olistoliths/olistostromes occur within the inner structure of the PKB, and when and why did they originate mostly during the Palaeogene part of the Mesozoic–Cenozoic history of this region? We expected this discussion earlier. The content of our paper was presented at the 6th Meeting of the Central European Tectonic Studies Group (CETeG) in Upohlav, Pieniny Klippen Belt, Slovakia (Cieszkowski et al. 2008), and later, at the XIX Congress of the Carpathian–Balkan Geological Association in Thessaloniki, Greece (Cieszkowski et al. 2010; Golonka et al. 2010). Some ideas were also briefly mentioned in the paper by Cieszkowski et al. (2009) in a journal issue edited by D. Plašienka. We assume that the comments are based on recent investigation, because the authors list the grants received to conduct the research. Therefore, the submitted comments sometimes present a point of view different from that published previously by some of the authors of the comments (RA, JM) (see Aubrecht et al. 2003; Krobicki, Aubrecht & Golonka, 2003; Wierzbowski et al. 2006; Pieńkowski et al. 2008). The statement, ‘Certainly there are many still unresolved problems in the geology of the PKB, and it ought to be said that the co-authors of this discussion also do not fully agree with all interpretations formulated and illustrated by the first author’ perhaps explains this controversy. Of course, we agree that ‘there are many still unresolved problems in the geology of the PKB’. We also agree with the statement ‘olistostromes and olistoliths are quite frequent, but not omnipresent’. We depicted the distribution of the olistoliths and their relationship to the non-olistolith tectonic units of the PKB in Golonka et al. (2015, figs 3, 8).