Fig. 5From: Ground motions induced by pore pressure changes at the Szentes geothermal area, SE HungaryHydraulic head measurements (a) and PS-InSAR time series of descending satellite orbits (b) in/near well K-652 located in the southern part of the Szentes geothermal field. For the InSAR time series plot, PS points within 500 m distance from well K-652, with a standard deviation < 2 mm/year are included. For the location of the geothermal well, see Figs. 2 and 4Back to article page