The Earth's Shifting Crust by Charles Hapgood - wire of information

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EARTH'S SHIFTING CRUST
as a sector of the crust approaches a pole. Where this happens,
the surplus surface must fold. Thus it is the force of
gravity, over a large area, that folds the crust in a small area.
It may help the reader to grasp this idea if he will visualize
a flat area on the equator which, in process of being displaced
with the crust as far as a pole, has been folded enough to produce
mountains six miles high. Now, actually, the peaks of
those mountains are no farther from the center of the earth
than the flat area was at the equator. Their altitude, with
reference to the earth's center, is unchanged. What has
changed altitude, however, is the rest of the surface, outside
the mountain chain. That has been pulled down six miles.
What pulled it down, obviously, was the force of gravity, and
the reason it was pulled down was that it was first shifted
horizontally to a place where gravity could act upon it.
Here, then, is the answer to the long-standing enigma of
the source of the energy for mountain folding. The moun-
tains are not lifted up at all; the surface is pulled down, the
force of gravity does the pulling, and folding results where
there happens to be excess of surface.
JF. Existing Fracture Systems as Evidence for the Theory
It is ordinarily considered a strong argument in favor of
a hypothesis if it enables one to anticipate the discovery of
phenomena. Campbell has shown that the theory of displacements
of the earth's crust calls for the existence of great sys-
tems of parallel fractures, intersected by other fractures at
right angles to them. It was some time after Mr. Campbell
began to consider this matter, and quite independently of
him, that I became aware of the fact that such fracture pat-
terns do, in fact, extend over the whole face of the globe,
and that geologists are in agreement that their origin is un-
explained. Many years ago Hobbs pointed out that they
must have been the result of the operation of some world-
wide force: