Abstract: The scales that allow for the shear planes (first scale), the rock and/or crust geometry (second scale), and the change of the geometries as earthquake systematics (third scale) are the basis for prediction and reduction of intensity. Actions to generate mini-movements to reduce the intensity of earthquakes are then concentrated on those areas where the stress concentrations generate jerky movements to alter the rock geometry (third scale). Based on the scale, the large-scale areas that influence the local stress concentrations and are involved in the jerky movements are thus taken into consideration.