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

EARLIER DISPLACEMENTS OF CRUST
40 50
1000 YEARS -
60 70 eo 90
Fig. X. North Atlantic Cores A 172-6, A 199-4, A 180-75
period back to about 100,000 years ago. We will assume that
this warm phase in the Atlantic represents the period, or at
least the latter part of the period, when Alaska was at the
pole.
We note, too, that the temperature in the Atlantic during
this warm period was not, at the sites of these cores, as high
as the temperatures now prevailing there, except for two
very brief spurts in Cores A 180-75 and A 179-4.
Yet we
have seen that the Urry core P- 12 6(5) indicated clearly that
the water was warmer at that time than it is at present. How
is this conflict to be solved? Shall we be forced to discredit
the reliability of one finding or the other? Not at all. Our
theory offers the possibility of eliminating this apparent contradiction
in the evidence.
Let us consider the present and past latitudes of these
cores. P-i26(5) was taken in about the latitude of St. John's,
Newfoundland; the others were taken in very low latitudes.