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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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NORTH AMERICA AT THE POLE<br />

he could see any logical alternative to crust displacement<br />

as the explanation <strong>of</strong> these facts. He replied that he was persuaded<br />

<strong>of</strong> the soundness <strong>of</strong> the method <strong>of</strong> crust radioelement<br />

dating developed <strong>by</strong> Pr<strong>of</strong>essor Urry, and that he saw no other<br />

reasonable explanation <strong>of</strong> the evidence (see page 364). A third<br />

line <strong>of</strong> evidence is that presented <strong>by</strong> Dr. Pauly, already dis-<br />

cussed (Chapter III).<br />

A fourth line <strong>of</strong> argument is developed <strong>by</strong> Lawrence Dil-<br />

lon, who shows, first, that the essential condition governing<br />

the growth <strong>of</strong> ice sheets seems to be not the average year-<br />

around temperature, nor the amount <strong>of</strong> annual precipitation,<br />

but the mean summer temperature (114:167). He points out<br />

that no ice sheets form at the present time in areas with mean<br />

summer temperatures <strong>of</strong> 45 F. or higher, and suggests that<br />

they probably didn't in the past. He cites, as a good illus-<br />

tration <strong>of</strong> this principle, the northeastern section <strong>of</strong> Siberia,<br />

which is unglaciated despite the fact that it is the "cold pole"<br />

<strong>of</strong> the world, and although it has a higher annual precipita-<br />

tion than Greenland or Antarctica. But the summer tempera-<br />

ture is high, and this he thinks is the controlling factor.<br />

Dillon points out, next, that the existence <strong>of</strong> the Wisconsin<br />

glacier would have demanded a decrease <strong>of</strong> 25 C. in average<br />

summer temperatures as they exist now (114:167). But he<br />

notes that according to Antevs the average temperature de-<br />

crease in late Pleistocene time along the iO5th meridian in<br />

southern Colorado and northern New Mexico as compared<br />

with the present was only 10 F., while (according to Meyer)<br />

the average temperatures during the glacial period in the<br />

equatorial Andes were only 5 or 6 F. lower than at present<br />

(114).<br />

Thus Dillon shows that there was no uniform decrease <strong>of</strong><br />

summer temperatures during the glacial period. No world-<br />

wide factor, such as variations in solar radiation, reduced the<br />

temperature. <strong>The</strong> range <strong>of</strong> summer temperatures<br />

would be<br />

understandable if the ice sheet were a polar icecap, however,<br />

and the range appears to require that assumption.

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