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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™