IV V For we must suppose that the wind in the earth has effects similar to those of the wind in our bodies whose force, when it is pent up inside us, can cause tremors and throbbings (…)

Assessing the stability state of fault interfaces is a task primary interest not only for seismic hazards, but also understanding how earthquake machine works. Nowadays it well known that relationship exists between slow and fast earthquakes; moreover, more evident such connection quite diffuse all over Earth. In this paper, we perform spatial temporal analysis both geodetic seismic—non-volcani...