Sudety Mts. and Fore-Sudetie Block constitute NE edge of the Bohemian Massif. Several large tectonic zones including the Sudetic Marginal Fault divide this area. Results or geodetic and seismic investigations show continuing tectonic movements that were at their peak in Neogene. During the 90-ties of 20th century, geodynamic investigations in this region intensified. Studies base on repeated satellite GPS measurements, gravimetric and relative (crack gauge) observations. This work focuses on presenting the conclusions or research carried out within the GEOSUD and GEOSUD II projects and concerns analysis or geometric, as well as, gravity changes on selected geodynamic profiles. Results obtained confirm recent activity or investigated tectonic zones.
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