FORESEEING EARTHQUAKES LONG TERM EARTHQUAKE FORECAST NEUTRALIZING EARTHQUAEKES
When a large quantity of components (H2O, H2S, SO2, etc)is concentrated on the western side of a projection, sometimes, because of oscillation, a few hours before a large earthquake, small quantities of those components escape and cause small tremors (Foreshocks.
When a powerful earthquake occurs on the western side of a negative projection (mountain foundations and submergence of lithospheric plates) this projection breaks, creating many other smaller ones, with such angles, that quantities of elements passing from beneath them trigger many shocks of lower intensity, because of their smaller capacity (Aftershocks).
Aftershocks of bigger magnitude than the initial earthquake occur on the submergence front (Fig. 4b) on either side of the initial hypocentre, as the first powerful concussion creates a long fault towards north and south, and with the water indraught the seismic activity is prolonged. The frequency and magnitude of these aftershocks decrease with the passing of time, because the angles of these projections are dampened by their frequent collision with the pyrosphere. (Figure 3A-3B,3Β-4Β).
Figure 3Α
Figures 4Α
Figure 3B
Figure 4B