SUPPLEMENT TO THE INVESTIGATION OF THE THERMAL COMPONENT ORIGIN OF RADONIC SPRINGS IN NI KA BANJA

The thermal water sources in Ni ka Banja, Glavno vrelo and Suva banja, consist of three water components each, namely, the thermal component, the cold permanent component and the cold occasional torrent - karst component. The genesis of warm component is not yet elucidated. There are present the opposite professional meanings. According to one researchers the warm component is descendible, the others think that is juvenile. The genesis of the cold components is in great measure explained. In this work there are systemized and documentary represented the results of searching the genesis of warm component during the twentieth century as a base and tendency for the further investigations. Particularly are analyzed the up-to-date results about the pulsation of water s temperature as a potential indicator of the rhytmical springing.