On the oscillogram we clearly see that the front rise time and the length of the positive phase of acceleration increase with the distance from the charge. From the arrival time of the acceleration pulse, or from its peak value, we easily find the velocity of propagation of the seismic waves.Experience in test range measurements of the seismic waves due to blasting revealed that by this method we can reliably record accelerations up to 25 9 103g and velocities up to 50 m/sec. (By including an electronic integrator in the circuit we can make direct records of the velocity.)