Re: OK Nancy, Where Is It?
In Article <CGF18.6339$k86.166627@weber.videotron.net> Greg Neill wrote:
> The problem with moving the crust over several
> hours is that the imparted energy does not disappear;
> energy can be neither created nor distroyed. The
> energy imparted to move the crust must be dissipated
> by the crust as it slows to its new postion.
The Zetas have said:
Where mountain building occurs when the plates stop
moving, the stoppage is not simply a sudden jolt, like
a car hitting a brick wall. All is in motion, and the
stoppage is more like a car hitting a barrier of sand
filled plastic barrels - a series of small jolts, occurring
in quick succession.
ZetaTalk, Pole Shift
(http://www.zetatalk.com/poleshft/p21.htm)
Since you're missing the point, and are an intelligent man, they wish to
expand on this a bit.
When riding in a train, where ALL are moving at 60
mph, do you devastate and KILL a fellow passenger
whom you happen to jossle while walking to the wash
room? This jossle is no more devastating than any
other, because you are BOTH moving. Translate this
to the crust of the Earth, pulled into motion en mass
when the core suddenly moves into opposition with
the passing Planet X. ALL are in motion. When the
impetus to move stops and slowing begins, does this
result in a sudden stop? It results in a series of
bumpings, where the strong parts of the Earth's crust
survive intact and the weak points give way and
crumble. Places where plates are already subducting
have the drama scripted for them as the forward force
cause the subducting plates to drive further UNDER -
an increase in mountain building. Since the Pacific
is deep and water has less resistance than land, the
Pacific will shorten. The push of solid plates into this
void will cause the subducting plates around the
Pacific to move futher than they would under the
earthquakes in man's recent memory. Once a break
is established, between plates, this tends to become
the weak point where the stress if directed.
Regardless, the motion stops not in a jolt, but in a
series of bumps, such that each stoppage is softened
because it reverts into motion forward again.
ZetaTalk