The blast vibrations were studied in the soil of quaternary sediments
and in Ordovician limestone in mining area. The measurements were perf
ormed by seismograph DS-277 Blast-Mate Series II of Instanter Inc. and
seismograph UVS-1500 of ABEM Instruments AB. The analysis of measured
data pointed at a good correlation between vibration velocity and sca
led distance from charges. The formulas for prediction of vibration ve
locity and far maximum charge weights were elaborated for both vibrati
on media - soil and limestone.