The main purpose of studies presented in the paper is the estimation of the statistical relation between seismic activity induced by underground mining and lineaments determined from satellite pictures. The studies were performed on the basis of mining tremors of energy above 108 Joules within the years 1985-2004 in the Upper Silesian Coal Basin (USCB) region. The monitoring and analysis of seismic activity showed the bi-modality of tremors energy distribution. Low-energy tremors are connected directly with stress field caused by mining while high-energy tremors are caused by an overlay of two factors: mining and tectonic stress field in rock mass. The lineaments observed on the satellite pictures are characteristic lines, which may be identified with lines that reflected neotectonic phenomena in the bedrock. The effect of such phenomena is transferred on younger sediments and on the surface. Some studies report that location of tremors is related with lineaments especially while crossing each other. In the paper, a correlation of lineaments with epicenters of strongmining tremors in several regions of USCB is presented. The correlation is proved by statistical parameters. In some regions of tremors location, geophysical anomalies: gravimetric and magnetic are also observed. The results of studies have practical meaning. They should be applied in planning of land development as well as in planning of underground exploitation.