“…On this basis, we can assume that a similar order of movements occurred after the Cretaceous inversion, which included the Bohemian Massif. On the basis of geological and geomorphological evidence, the authors expected to obtain confirmation of the trend (but not the size of displacements), where vertical crustal movements have continued to the present day (Zeuner, 1928;Schwarzbach, 1942;Oberc and Dyjor, 1969;Radwański, 1975;Batik et al, 1996;Ivan, 1996;Don, 1996;Žatecká, 1996;Przybylski, 1998;Sroka and Kowalska, 1998;Krzyszkowski et al, 2000;Ranoszek, 2001;Badura et al, 2004Badura et al, , 2007Kontny, 2004;Štěpančíková et al, 2008;Badura and Rauch, 2014). The results rather suggest that in the eastern part of the Central Sudetes subsidence prevails, which is consistent with the recent crustal movement models developed by Kowalczyk et al (2010).…”