Six monitored faults displayed continuous activity and high sensitivity to stress field changes in the Slovenský karst and Ochtiná karst. We observed three mutual periods with increased stress in half of 2013, 2014/2015 and half of 2017. The most significant one was the 2014/2015 period. This period enabled us to compute NW-SE stress orientation at localities the Drienovská Cave and the Skalistý potok Cave. On the other hand, the long-term regime represents the NE-SW striking extension. It is obvious from prevailing eastern blocks subsidence in the Skalistý potok Cave. The fourth period represents stress relaxation at the end of 2018. It was documented by subsidence at the Skalisty potok 1 and 2 sites, fault opening at the Drienovská 1 site, and subsidence in the Krásnohorská Cave. That relaxing period was preceded by a calm period, without any significant displacements. Furthermore, recent results show that displacements reach a hundredth and tenth of mm per year.