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

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EARTH'S SHIFTING CRUST
This extraordinary case is by no means unique, for Umbgrove
has pointed out that the sediments composing much
of Spitsbergen and Scotland come from the ocean west of
them, while those composing the west coast of Africa come
from a former land mass in the present South Atlantic. Most
interesting of all, he indicates that the deepest of the world's
deep-sea troughs (east of the Philippines), about seven miles
deep, gives evidence that it was once part of a very large continent
(430:38).
that a conti-
The evidence produced by Coleman, showing
nental ice sheet once invaded Africa from the sea, and that
the Indian ice sheet must have extended on land far to the
south of the present tip of India, is to the same effect. It
serves to answer conclusively the argument about continental
shelves. You can put just so much on a shelf.
evidence of re-
According to Umbgrove, there is ample
and downward oscillations of the floor of the
peated upward
entire Pacific (430:236). In a kind of rhythm, the great ocean
has become alternately shallower and deeper. In the absence
of any explanation of this phenomenon, Umbgrove becomes
geopoetic. There seems to him to be something almost mystical
in this slow pulsation of the living planet. He finds that
the unexplained upward and downward movements are not
limited to sea areas:
... It should be noted that blocks that were first submerged, then
elevated, and then once more submerged and elevated, are also met
with on the continents. The sub-Oceanic features and the similar
continental characteristics cannot be explained at present, for our
knowledge of pre-Cambrian history and terrestrial dynamics
yet extensive enough. . . . (430:241).
is not
Comparatively radical vertical changes in the positions of
land masses are evidenced by a considerable number of ancient
beaches (some of them, however, not very old) which
are now found at great elevations above sea level, and some-
times far inland from the present coasts. Thus the geologist
P. Negris claimed to have found evidences of beaches on
three mountains of Greece: Mt. Hymettus, Mt. Parnassus,