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

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

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EARTH'S SHIFTING CRUST<br />

If we assume that Alaska was at the pole during this warm<br />

period in the Atlantic, the site <strong>of</strong> this core would then have<br />

been farther from the pole than it is now; that is, it would<br />

have been south <strong>of</strong> its present latitude. Quite naturally the<br />

water would have been warmer. A glance at the globe will<br />

suffice to make this plain.<br />

On the other hand, if we now consider Core A 180-75,<br />

taken in the eastern Equatorial Atlantic, nearly on the<br />

equator, the opposite situation is revealed. A pole<br />

in Alaska<br />

would displace this core southward from the equator, pos-<br />

sibly as far as the 2Oth parallel <strong>of</strong> South Latitude (depending,<br />

<strong>of</strong> course, on the precise location <strong>of</strong> the pole in<br />

Alaska).<br />

Quite probably, the water would be colder then than it is at<br />

present, other things being equal.<br />

<strong>The</strong> two Caribbean cores would, with the Alaskan pole,<br />

have had approximately the same latitude as at present; the<br />

uncertainty as to the precise location <strong>of</strong> that pole makes it<br />

impossible to draw any reliable conclusions from them.<br />

Both the Caribbean cores indicate a temperature minimum<br />

about 55,000 years ago, which would correspond well<br />

with the date we have tentatively assigned for the arrival <strong>of</strong><br />

Greenland at the pole; they both show the temporary warm<br />

period that was shown in the Arctic cores, which we have<br />

interpreted as marking the breakup<br />

<strong>of</strong> the Greenland conti-<br />

nental icecap. <strong>The</strong>y then show a gradual temperature decline<br />

from about 40,000 to about 1 1,000 years ago, which may cor-<br />

respond, first, to the growth <strong>of</strong> the Wisconsin continental<br />

icecap and, finally, to the movement <strong>of</strong> the ice center <strong>of</strong> that<br />

icecap eastward into Labrador during the declining phases <strong>of</strong><br />

the glaciation.<br />

At this point it is important to consider a contradiction<br />

between the Caribbean cores and the core from the eastern<br />

Atlantic. It appears that the ocean temperature reached its<br />

minimum, after the early warm period, in the eastern Atlantic<br />

about 20,000 years before it did in the Caribbean.<br />

This is a very important difference. How is it to be ex-<br />

plained?

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