This paper presents results of the statistical analysis of the high energy seismicity relation to lineaments in the areas of the Upper Silesian Basin. Four parameters are chosen, i.e.: lineament azimuth, fault azimuth, tremors vector azimuth (TVAA) (the vector initial point was the epicenter of strong tremors with energy greater than E > 108 J, and the terminal point was the epicenter of strong tremors with energy greater than E > 5.5 ź 105 J but less than 108 J), tremors vector azimuth (TVAB) (the vector initial point was the epicenter of strong tremors with energy greater than E > 5.5 ź 105 J but less than 108 J, and the terminal point was the epicenter of strong tremors with energy greater than E > 108 J). Calculations aremade on the basis of a set of 31 high energy tremors with energy of E > 108 J within the area of the Upper Silesian Basin. The catalogue of tremors includes the position of the epicenters and their energy. The research reveals a significant relation of the lineament azimuth to the azimuth of tremor vectors after a high energy tremor (TVAA). This relation may prove the theory of the dip-slip tremor mechanism. The fault plane of such a strong tremor may be revealed in the form of a lineament.