Metamorphic phenomena formed geological and tectonical structure of the Śnieżnik Kłodzki Massif, Kłodzko Valley, SW Poland. In 1992 twenty seven points of local geodynamical network were founded for determination the Śnieżnik Massif crust activity. Points of this network were located in Czech and Polish sides of the Massif. Researches were provided by repeated periodic satellite GPS measurements, total station, gravimetric, clinometric and crack gauges observations and precise levelling technique. Śnieżnik Massif is crossed by the section of tectonic faults zone in direction NW-SE. Several transverse faults are located near the major tectonic zone. Long term research material (data) allows to interpretation and evaluation of the object surface deformation., Olgierd Jamroz., and Obsahuje bibliografii