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Date: Fri Jun 25 06:28:05 2004Message Thread:
From: Sam making steam and pace.
Subject: This time in a train!I supposeI should re-read the following, but I'd rather
you be laying on the train-tracks---been a few hours writing.
Prefatory: "How Earth became made from matter" is mainly in
another story of mine. Much of the following I theorised.
WHY SANDSTONE MOUNTAINS.
Earth moves through Space as Nothing and of matter.
Earth bar perhaps some gasses from magma was all magma as a
product of "fall-in" as magma/Earth heating. That Magma-ball
then had No crust above it.---( Magma was Not as described in the dictionary.
) Gas was perhaps above, surrounding this magma-ball. Earth made own heat.
Earth when of very little atmosphere was gathering Space-gas Earth's atmosphere
touched or perhaps was near enough at times
for forces to bring to Earth.
That magma-fall-in makes forces ( magnetic or other as "N"? )
which going into the direction of Space touch same-type-
forces from the sun or other planets.
The Sun is a less dense magma ( of more gas? ) than the Earth was and is of
Now.
That touch touching of those forces perhaps imbuing somewhat
or become part of each other somehow causes continual
orbiting?
Question is: Can those forces be used for teletransportation of
matter or whatever? Will we by untilizing those forces reach
other galaxies, planets, etc.?
Fall-in is ball-shaped due to fall-in falling in and in Space as Nothing falling.
The times Earth gathered amounts of Space-gas atmosphere
grew deeper. And atmophere grew very deep---each large
consecutive depth mostly cooler than the prior depth.
Atmosphere getting deeper and cooler was cooling Earth's outer magma which when
the atmosphere was deep enough became a
thin crust of No magma nor mountains. And that crust easily cracked which caused
pour-outs of magma. Weights shifting caused by various atmospheric changes volitile
or other caused much of those cracks. Air at night cooling to heavier cracked
the then thin crust.
And deeper the atmosphere became. And deeper that crust
became, very deep. Magma-outbreaks, crust-up-lifts, foldings, quakes and cooler
magma outbreaks more like lava were contributing factors forming huge swooping
valleys and some
of that crust; but No mountains the size of today's; but very
much the solid, gigantic masses of rocks in today's lower areas.
And the atmosphere grew deeper and out of that atmosphere water came and began
filling lower areas that became seas.
The atmosperic depth grew more to enough that caused the freezing of Earth's
Poles ( made also as sphere-tips was farther from warmer sunned-areas ).
And Atmospheric layers layering then would Not be strong enough and/or undisturbed
enough to move a compass needle?
In those Seas and on Land while Earth was gathering more and more atmosphere
life eventuated ( that is a long story ). That
life as plant-life and creature-life grew to prolific.
The atmosphere became so deep as to cause colder conditions
that caused more ice at the poles. And so massive weight-shifts accurred by
quickly shrinking-seas thus causing outbreaks of
lava that at this stage mainly becomes sandy rock, the lighter
less dense rock These lava-out-breaks became what are now today's Sandstone
Mountains Not made only out of deposits
from rivers and sea. Nor did the rivers as said eroding cause so much the valleys
between Sandstone Mountains... Some Sandstones were very easily washed apart,
away but were as mountains to begin with. hahaha
A grand happenning of lava-outbreaks is when limestone that
life living had made melts and boils with lava and its sometimes
denser masses, etc. causing volatile spits of flint or soap-stone
into the air, many coated in limestone, many not, many later become tools due
to the perfect flight-made and/or landing-
made shape that were used by humans. Circumstances at about these later times
killed many of the larger dinosaurs.
Magma/Lava is a mixture that when cooler expands
and separates. The first crust from cooling of magma on Earth was harder than
most of the later crusts from the cooling of lava.
Lava cools to as mainly of lighter rocks than does magma cool
to as. The close in lava under the crust was of a lower
temperature than the more inward magma. The lava-outbreaks were when the crust
was at a certain depth. Sometimes or often amounts of magma was with lava; then
if cooled made more variety of stones.
Lava more than magma makes the type of rock one would
break- down and add to compost so to make mud, certain sands.
Copyright 2004 Sam as G.H. All Rights Reserved.
Was prior sent to one of my internet addresses where from put to hardcopy.