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

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EARTH'S SHIFTING CRUST
he says, is evidenced by the folding there of the young sedi-
mentary rocks (97:391-92).
Daly does not suggest a possible cause for this lateral compression
of the whole peninsula; such a compression, part of
the process of mountain building, he has already character-
ized as "utterly mysterious." But it must be clear that it is
precisely the type of distortion that might be expected to result
from a displacement of the earth's crust. Such a movement
could very well account both for the depression of
lower India and for the uncompensated elevation of the
Himalayas. It can be said, moreover, that no displacement of
the crust could possibly take place without creating, at some
points on the earth, precisely such deep-lying gentle undulations
of the crust.
But still another point may be urged in support of this
solution of the problem. We shall see, later on, that the last
movement of the crust appears to have been approximately
along the goth meridian, with North America moving southward
from the pole. This movement would have subjected
India to maximum displacement and to maximum compression.
In this last movement India would have been moved
across the equator and northward toward the pole, to its
present latitude.
Daly's suggestion that compression may increase the tensile
strength of the crust opens up most interesting possibilities.
We may find here, in connection with the theory of crust dis-
placement, a solution to very puzzling problems
of isostatic
theory. The crust of the earth shows enormous differences
from place to place in its degree of isostatic adjustment and
in its sensitivity to the addition or removal of loads. Applying
Daly's suggestion, we may infer that the differences may
owe their origin to recent displacements of the crust. Areas
recently moved poleward, having undergone compression
and still retaining compression, would, according to Daly's
suggestion, have greater strength to sustain the distortions;
areas recently displaced equatorward, having undergone
extension, or stretching, would have less strength to resist