The Earth’s Core

The Willow File

There is a boundary layer or interface deep within the liquid core of the Earth where magnetic polarization occurs. This layer is denser or heavier than the liquid region above it (and possibly also below it). Normally, the wave-like magnetic regions are oriented so that north faces outward and south inward (see Fig. 2). During times of instability, however, more and more regions assume a metastable position of magnetization. This change shifts the burden of polarization to neighboring regions and causes this layer to move up and down to a certain degree. A complete magnetic reversal may take place.

As depolarization progresses, highly magnetized and high-density "clumps" form and sink downward toward the solid core. At a certain critical depth, a type of transformation occurs that causes them to be powerfully accelerated upward. Their movement is halted at the underside of the mantle, where they plug the fissures or fractures that lead to the surface. In the process, other fractures are created, but these run horizontally. This entire process is based on a kind of circulation of inner matter that moves from the core upward toward the crust.

The crust itself consists of layers of rock that rest on a semi-solid layer, which in turn sits on a solid material layer that acts like a lid on the liquid core. The solid and innermost part of the Earth’s core emanates three different types of pulsation. Two of them are reflected at the underside of the crust, but the third radiates outward into space. The (translator’s note: frequency/scale) ranges referenced above may lie in the molecular scale, in some ways comparable to ocean waves.

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