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

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EARTH'S SHIFTING CRUST
5. New Proposals of Polar Shift
Since truth cannot be suppressed forever, it was inevitable
that accumulating facts should eventually bring the polar
issue again into the foreground. Gutenberg suggested that
while continents cannot drift, perhaps they can creep (194:
211). The British astronomer Gold postulated that the earth's
wobble on its axis could cause a plastic readjustment of its
mantle sufficient to move the poles 90 degrees in a million
years (176). The French geographer Jacques Blanchard suggested
the possibility of extensive polar changes due to more
pronounced wobbling of the earth in the past (38). Ting Ying
H. Ma, of Formosa, raised the idea of a combination of conti-
nental drift with displacement of the outer shells of the
earth (285-290). Bain thought of displacements of the crust
to account for facts of ancient plant geography and fossil soils
and suggested a mechanism to try to account for them (18).
Pauly (342) revived the suggestion made by Eddington (124)
that the earth's crust may have been displaced by the effects of
tidal friction. Kelly and Dachille, in a provocative work on
collision geology entitled Target Earth, offered the hypothesis
of displacements of the earth's crust as the result of collisions
with planetoids (248).
The most important recent contribution to the controversy
has certainly been the evidence produced by geophysicists in-
vestigating terrestrial magnetism.
This new evidence is so im-
pressive that it has brought about a reversal of opinion in high
geological quarters on the question of the permanence of the
poles. One of the leading specialists in this field, Dr. J. W.
Graham, has recently remarked:
. . . Within the past couple of years there have appeared a num-
ber of serious papers dealing with the subject of polar wanderings by
which is meant a shift of the geographic features of the earth's surface
with respect to the axis of spin. Classical geophysical treatments of
the type pioneered by Sir George H. Darwin early in this century
have been re-examined in the light of our more recent knowledge of