Page 34 - Spirit and Mind. Vol 1
P. 34

Nicolai Levashov. Spirit and mind. Vol.1

            night (non-illuminated) surface continues to have the same dimensionality gradient
            between  the  atmosphere  and  surface.  Thus  a  dimensionality  gradient  occurs
            between  the  lit  and  unlit  surfaces  of  the  planet.  A  horizontal  dimensionality
            gradient  parallel  to  the  planetary  surface  is  created.  As  a  result,  molecules
            forming  in  the  ionosphere  begin  moving  along  this  gradient,  thereby  creating  an
            atmospheric  movement  of  air  masses.  Let  us  examine  the  subject  of  gravity  for  a
            better grasp of this phenome-non.

                  What is gravity or gravitational force? Why does it exist and what is its nature,
            as a result of which objects drop down and do not fly up? What makes objects move
            in  a  certain  direction?  To  clarify  this,  let  us  return  to  the  process  of  planetary
            formation in a nonuniform zone of space created by a supernova explosion.

                  Consecutive merging of seven forms of matter in such a zone gives rise to the
            formation  of six hybrid forms.  In this process, space nonuniformity  is neutralized.
            There is one peculiarity to be noted: hybrid matter differs in quality from the free

            matter  which  forms  it.  Therefore,  free  matter  forms  continue  flowing  through  the
            nonuniform zone but, at the same time, no further hybrid matter is created.

                  Synthesis occurs only when the quantity of hybrid matter, for some reason or
            other,  decreases.  After  the  balance  is  restored,  synthesis  ends.  The  process  is
            constantly  perpetuated  because  our  planet  keeps  losing  matter  due  to  nuclear
            reactions and partial loss of atmosphere. Not only comets -but also planets — have a
            gaseous tail. This is the cause of a planet's atmospheric loss.

                  When moving in a nonuniform zone, free forms of primary matter go from a
            higher to a  lower dimensionality  level.  What is  the consequence  of this behavior?
            Because  free  matter  forms  react  differently  on  one  and  the  same  gradient  of

            dimensionality, turbulence occurs periodically in a non-uniformity zone.

                  The  turbulence  of  the  fluxes  and  the  spatial  nonuniformity  give  rise  to
            movement  of  the  earth's  crust  and  volcanic  eruptions:  hence,  the  correlation
            between solar and tectonic activity of

            the planet. Solar storms lead to fluctuation in potential of the fluxes.

                  At the same time, qualitative barriers between the planetary levels have varying
            degrees of permeability to  different matter fluxes. This  leads to a disproportionate

            accumulation of free matter forms at these barriers, giving rise to inner turbulence,
            which induces tectonic activity.

                  Let  us  take  as  an  illustration  a  cascade  of  six  proportional  ponds  having  the
            dimensions of a water reservoir. Each one is larger than its neighbor by one and the
            same value. As the upper-most reservoir is filled, water overflows and begins to fill
            the lower one which is twice the size of its up-per neighbor. When the second fills up,
            the water overflows to the third and so on, until all six reservoirs are filled.

                  Even when all the reservoirs are filled, inflowing water will keep on moving and
            overflow  to  the  next  lower  reservoir.  At  the  same  time,  all  reservoir  levels  will
            remain  the  same,  but  the  water  will  create  turbulence  inside  the  reservoir.  The
            incoming water will replenish the water evaporated from the reservoir surface. Such a
            system  can  go  on  indefinitely  or,  at  least,  for  a  long  period  of  time.  Increase  in





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