The Earth's Heartbeat

The Earth’s heartbeat is known as the Schumann Resonance, which has been recorded at approximately 7.83 cycles per second for presumably thousands of years.  In recent years, the Schumann Resonance has been rising and was recently recorded as high as 8.50.

Speculation infers that the Earth may stop rotating once the Schumann Resonance reached 13 cycles per second.  At that point, the Earth would stop rotating for 3 days and then start spinning in the opposite direction, causing a magnetic reversal of the poles.

Under this premise,  a magnetic pole reversal may affect the way the hemispheres in our brain interact.  Three possible scenarios exist in such a situation:

1. Nothing happens to our brains.
2. The hemispheres of our brains instantly interact with one another, opening up synapses to higher metaphysical abilities.
3.  We all become insane!
It is estimated to take between 1,000 to 10,000 years for a complete magnetic pole reversal to occur. Our current version has been ongoing since the early 1900’s. While the ultimate completion may not occur for another 900 to 1990 years, its effects may already be seen.

The latest studies from the University of California, Berkeley state that it could take 100 years or less, adding that the current weakening magnetic field will precede the pole flip.

What we can readily observe are the facts:

The magnetic poles have been reversing since the early 1900’s
The Schumann Resonance has been rising.
There has been a recent phenomenon regarding our perception of time. Could this be related to the magnetic pole shift?

If “as above, so below” can be interpreted as, “as within, so without” then we can surmise that major changes are happening both in the cosmos, on our planet and, ultimately, within ourselves.

Earth has a strong internal magnetic field that appears to be generated by electrical currents in the liquid outer iron core that are driven by internal heat sources. The magnetic field resembles that of a bar magnet or “dipole field” with an axis tilted about 11.5 degrees from the spin axis, so, the magnetic poles are not the same as the geographic poles. Earth’s magnetic field strength was first measured by Carl Friedrich Gauss in 1835 and has been measured repeatedly since then. The field has shown a relative decay of about 10% over the last 150 years. The locations of the magnetic poles are not static; they wander as much as 55 kilometers every year.

The geomagnetic field is influenced by the sun and moon’s rotations, solar flares and probably interplanetary influences. Animals, including birds, can detect Earth’s magnetic field and use it to navigate during migration. It has been shown, for example, that cows and deer, when grazing, tend to align their bodies north-south in response to the earth’s magnetic field.

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