FORESEEING EARTHQUAKES LONG TERM EARTHQUAKE FORECAST NEUTRALIZING EARTHQUAEKES
When the Earth was formed, it was in a state of burning heat. As time went by, temperature on the planet's surface was falling due to radiation and heat transfer, and various components (crusts) began taking solid form at the Earth's poles. The formation of crusts took place at the Earth's poles, because the stirring of burning and fluid masses on the surface of the Earth was significantly slighter there than it was on the equator. Due to centrifugal force and Coriolis Effect, these solid masses headed towards the equator; those originating from the North Pole followed a south-western course, while those originating from the South Pole followed a north-western course and there they rotated from west to east at a lower speed than the underlying burning and liquid earth, because of their lower initial linear velocity, their solid state and inertia.
Because inertia is proportional to mass, the initially larger solid body swept all new solid ones, incorporating them to its western side. The density of the new solid masses was higher, because the components on the surface would freeze and solidify first, before the underlying thicker components. As a result, the western side of the initial islet of solid rocks submerged, while the east side elevated.
As a result of the above, this initial islet began to spin in reverse, and after taking on the shape of a sphere, it formed the "heart" of the Moon. The Moon-sphere, rolling on the equator, would sink the solid rocks that continued to descend from the Earth's poles. The sinking rocks partially melted because of higher temperatures in the greater depths that the Moon descended to, while part of the rocks' mass bonded with the Moon and also served as a heat-insulating material, preventing the descended side of the sphere from melting. Combined with the Earth's liquid mass that covered its emerging eastern surface, new sphere-shaped shells were created, with increased density and very powerful structural cohesion (Fig. 1).
As this sphere (the Moon) continued to grow, the Earth-Moon system was displaying a double-planet image. The Moon's reverse rolling velocity increased according to the increase of its mass and volume. As the temperature on the surface of the Earth continued to fall, a larger number of bigger sized solid masses were descending from the poles towards the equator, and the Moon could no longer aggregate them. The gathering and interference of solid rocks of great mass acted as the catapult on which the Moon bounced off the Earth and was put into orbit around it. During its detachment, the Moon maintained its form, because its successive layers obtained great cohesion to each other, as they were created under conditions of great pressure and temperature. (Fig. 1)
During the Moon's detachment from the Earth, an umbilical cord of liquid mass was created between the Earth and the Moon, which was of greater density than the mass on the two bodies' surfaces, because it mainly originated from the area where the Moon's side was sunken.(Fig. 1)
As the Moon moved away from the Earth, the cord was severed and the part which remained with the Moon spread across its visible side, it evened its surface and created the Moon's "seas," while it changed the Moons' sphere-like shape, as its radius was increased and its centre of gravity moved 2.5 kilometres towards its visible side. During this procedure, small satellites were created from the cord's liquid mass. Some of them later fell on the Earth, while others fell on the Moon, creating its huge, but very shallow - because of the Moon's powerful structure - craters. The Moon's rock strata are distributed according to their density, to successive spherical shells, with lower density in the Moon's centre and higher on its surface.
The visible side of the Moon where its seas are has even higher density, due to the origin of the material that covered it (which originated from the mantle of the Earth). Because of the above, a gravity connection was created between the visible side of the Moon and the Earth. Furthermore, the Moon has no spin effect and regardless of the time it takes to rotate around the Earth, it will always show its one side.
After the Moon's detachment, the process of rock solidification continued at the Earth's poles, as well as their descent towards the equator. No new sphere was created during this phase, because the quantity and amplitude of solid masses were large, there was no rolling and the initial continent was formed, which increased rapidly in amplitude and mass. As a result, the shape of the Earth changed from spherical to oval, and the initial continent, on which gravity was significantly lower than on the rest of the Earth's surface, formed the top of the Earth. The increase of the coagulation rate gradually created a solid oceanic crust on the western, northern and southern part of the initial continent, and this crust gradually covered the Earth's entire surface. The oceanic crust is younger than the initial continent, and so it is denser than it.
When the oceanic crust became significantly thick and the temperature on its surface decreased, the steams at the Earth's atmosphere liquefied and fell on the planet. They remained there, thus creating the ocean which covered the entire planet, except for the initial continent. (Fig.2)
Due to favourable conditions (temperature, humidity and especially low gravity) plant and animal life on Earth exploded. Then, one of the small satellites (of those that were created by the umbilical cord during the Moon's detachment) fell on the initial continent. As a result of this impact, the initial continent was split and the new parts that were formed (continents) were now thinner and wider; the western part (America) rose, because the oceanic crust was swept out and gravity increased proportionally.
The splitting of the initial continent and the oceanic crust was followed by:
- Large tidal waves.
- Vaporization of great quantities of water, due to the crust's contact with the pyrosphere in areas where this was temporarily uncovered.
- Cataclysmic rainfalls that swept plants and animals from the surface of the continents, burying them at the shores together with plankton, in areas where continental parts converged. This is how petroleum deposits were formed. Plants and animals that were buried in valleys and mountain plateaus formed coal, when the waters ran off. The quantity of petroleum and coal corresponds to the size of the converged areas. (In Greece, the largest petroleum deposits are north of Crete, where huge North African areas converge, as well as in the Thermaic Gulf, while a little to the Gulf's north there are coal deposits).
Calm was restored on the Earth's surface and life developed and evolved for a long period of time. Relatively recently, one of the satellites which were created during the Moon's detachment (the last one) was approaching the Earth, because of its decaying orbit. At that time, humans could calculate the place (Mediterranean) and time of impact, and many of them took steps to deal with this challenge. They migrated to the eastern shore of Asia. There, they built covered vessels (arks) and moved away from the shore, sailing into the ocean, in order to tackle with the powerful tremors caused by the impact and the large tidal wave that followed. Those who survived later returned to the west (Indo-Europeans).
The most important geological effect of this impact was the displacement of the American continent to the west, where it remained. Also, the shape of the Earth became spherical. The quantity of water that vaporized was smaller this time, as the pyrosphere that was temporarily uncovered was only in the area of the Atlantic Ocean and it cooled and stabilized quickly. This is why the oceanic crust of the Atlantic is younger and denser than that of the Pacific.