from softened or melted ore, as the atoms are free to line up end to end. The core of the Earth is perpetually in this
state, and thus it acts like a huge magnet, as large as the globe itself. Magnetic influences between planets are greater than humans imagine, because they use as their frame of reference objects on the surface. The Earth's crust is
magnetically diffuse, representing many different pole alliances over the eons, as magma hardened after volcanic
eruptions during pole shifts. The Earth's thick crust acts as a shield in this way, so that only sensitive needles on
compasses, floating freely, jiggle into alignment with the Earth's core.
A planet's magnetic influence is not encapsulated by its crust, but reaches beyond this even to the ends of the solar
system. Like the shields that men stood behind to watch an atomic blast, they may have avoided the radiation, but the
landscape behind them was devastated. The Earth's magnetism oozes around the various crustal plates acting as shields
to recreate its essential alignment out in space, considering any confusion the crust may have presented as no more
than an annoyance. A resonance is involved, so that the magnetic field can reestablish itself, filling in any blanks.
Thus, when magnetized planets encounter each other, such as when the 12th Planet passes near the Earth, the strength
of their reaction to each other is much greater than man might imagine.
Mankind's tiny magnets are but specks on the surface of thick crusts acting as shields. Below the surface, in the liquid
core of the Earth, and in resonance high above the surface, is where the real magnetic drama occurs.
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ZetaTalk: Gaseous Planets
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ZetaTalk: Gaseous Planets
Note: written during the 2001 sci.astro debates.
Gaseous planets work on the same principles driving their rotation, but due to the lack of a solid crust their cores and
atmospheres merge, where the rotation patterns on the surface of a planet with a solid crust is altered by the form and
shape that crust takes. In rotation within a liquid or mobile core, the rotation rate differs for the various parts of the
core. Rotation, as we have explained, is driven by parts of the core moving toward or away from elements outside of
the planet. Like runners in a race, some parts move faster and others more slowly, depending upon the strength of the
attraction or repulsion that is driving their motion within the core. There are also differences in mass, so that some
parts of the core float closer to the surface, and others fall to the center of the core. What does all this do to the
rotation of a gaseous planet, where the drama of rotation in the core expresses itself on the surface of the gaseous
giant?
Just as the oceans of the Earth pool about her Equator, due to being slung there by the motion of rotation, just so the
lighter elements in a gaseous planet pool about its equator, with the heavier elements lining up in bands toward the
poles. Motion in a liquid or gaseous core, once started, is driven also by the very motion itself. Around the equator, the
lighter elements rush to the surface, and there find they cannot leave due to the gravity pull of the planet, but also are
being pushed from behind by more of the same element rushing to the surface. What happens in a fast flowing river, to
the water along the banks which are being slung away from the pressure at the center? Eddy current occur, where the
pull of the flow at the center creates a relative vacuum in that there is a difference in water pressure along the fast
flow, so that water slung to the sides of the flow circle back into those spots of lesser water pressure. Likewise, eddy
currents occur in a gaseous planet’s latitude bands, so that the motion of rotation apparent on the surface appears to be
alternating bands with an east-west motion. The heaviest elements in such a planet pool at the core, and due to the
motion of rotation which slings the lighter elements toward the surface of the planet, these heavy elements also creep
up toward the poles. All else, the lighter elements, have left for the surface, and been pulled based on their relative
weight toward the equator of the planet. The poles, thus, reflect the overall rotation direction of the gaseous planet.
On Earth, these same patterns exist, but due to the buffering action of the crust the atmosphere operates independently.
Where the Earth moves under the atmosphere, the drag is from east to west, and as the atmosphere is not so inclined,
eddy currents, the prevailing westerlies, are created. Storms on Earth, created due to unequal pressure of air masses
and their relative humidity, last only as long as equalizing the factors takes - a matter of days. Storms on a gaseous
planet, noted by NASA in July, 2001 from recent images taken by a fly-by probe, seem to last for long periods. This is
because they are not driven simply by a thin and highly mobile air mass, but by elements disbursed in the entire core of
the planet. Equalization is not in a thin layer, but as deep as the planet itself, so the drama takes longer to resolve.
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ZetaTalk: Opposition
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ZetaTalk: Opposition
Note: written during the 2001 sci.astro debates. Planet X and the 12th Planet are one and the same.
Children playing with magnets soon discover that magnets brought in close proximity to each other want to snap
together, north pole to south pole, and can be positioned north pole to north pole only under force. Lined up side by
side, as long as a certain distance is maintained and friction against a table top or other surface is present, they can
coexist with without polar symmetry, however. Why the pressure to snap together and align when poles approach,
where not so in a side by side arrangement? An analysis of magnetic particle flow in magnets placed end to end show
the particles flow moving through the entire length of the linkup of magnets, creating a longer and larger field before the
particles return to the shared south pole at the end of the lineup. But what of the particle flow when magnets are
positioned side by side? The key here is the strength of the fields, and the closeness of the magnets.
If the magnets are of a strength and closeness to each other such that a returning particle finds itself fighting the
flow to do anything but go to the far edge of the overall mega-magnetic field created by the group, the magnets
will line up with their poles in the same direction.
If any of the magnets are of a significant strength, but the magnets are not so close that returning particles are
perforce forced to the outside of the overall mega-magnetic field created by the group, the returning particles will
take the path of least resistance and return via a magnet in opposition. In fact, this magnet will be in opposition in the grouping not because of its original orientation but because the returning flow creates a south pole handy to