Abstract:
The ionosphere is a part of the Earth's atmosphere specific for the increased concentration of charged particles. By monitoring the reaction of these charges, primarily negatively charged electrons, to various disturbances coming from space or from the Earth's surface, conclusions can be drawn about the intensity, nature and origin of these disturbances. In this paper changes in the ionosphere caused by seismic activity were examined. The carrier of disturbances between the trembling soil and the ionosphere are gravito-acoustic waves.