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

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EARTH'S SHIFTING CRUST
to start a movement of the crust, it will simply continue to
grow, drawing upon the endless resources of the oceans until
it is big enough.
3. A Suggestion from Einstein
From the foregoing, it is clear that there is a basis for the
presumption that the Antarctic icecap is largely
an uncom-
pensated mass (an extra weight on the surface of the earth),
that it has grown continuously since the disappearance of
nonglacial conditions in the Ross Sea area only
a few
thousand years ago, and that it is growing now. Einstein
recognized, in the Foreword to this book, the centrifugal
momentum that such an uncompensated mass, situated eccen-
trically to the pole, would create when acted upon by the
earth's rotation, and he saw that the centrifugal momentum
would be transmitted to the crust. But he also raised, in the
last paragraph of the Foreword, another interesting question.
If an icecap can have such an effect, so can any other uncom-
pensated mass. It is necessary to investigate any existing distortions
within the crust itself and to learn whether it may
contain uncompensated masses of a magnitude comparable to
the Antarctic icecap, and thus capable of causing comparable
centrifugal effects. For the inference is obvious: if such masses
are in existence, but have not moved the crust, it follows that
the crust may be anchored too solidly to be moved by the
centrifugal effect of icecaps.
One of the troubles with the theory of isostasy is that the
failures of the crust to adapt to gravitational balance have
been found to be more numerous and more serious than ex-
pected. Daly lists and discusses a large number of them. It
that the whole chain of the Hawaiian
appears, for example,
Islands, with their undersea connecting masses of heavy
basalt, are uncompensated (97:303). These islands rise from
the deep floor of the Pacific, and their peaks tower two and a
half miles above sea level. Their gigantic weight rests upon