The latest geodynamical measurements in Krsko Valley

On the basis of triangular measurements done in 1954 and GPS measurements done in 1994 the neotectonic shifts along Orliśki fault were determinated. These measurements were used by Gelogogists who have determined the stabile points for the future measurements. Measurement points have been stabilised on the new way. Ali directions and distances in the net have been determined. Up to now three measuremts were completed. On the basis of the adjustmet the new coordinates have been obtained and by those the shifts along the Orliśki fault have been determined. The GPS geodynamic net was also stabilised and observed. This net covers the whole environment of the Krsko valley. Unfortunatelly, only the zero measurement was observed so far.