Abstract
Coal mining realised in Upper Silesian Coal Basin is the main course of occurrence of bumps and rock-bumps. Geodynamical phenomena described as the rock-bumps occur in the area of GZW from the end of the 19th century. The mechanism of the rock-bumps phenomenon, due to the complexity, didn’t allow elaborating the completely effective method of its forecasting. However, increasing amount and the scale of rock-bumps, due to the development of mining, have extorted the scientific circles to perform works devoted to the elaborating newer and newer and better and better methods of the assessment of liability to rock-bumps, likewise methods of rock-bumps hazard assessment.
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