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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 2O1<br />

gin <strong>of</strong> error. This new expansion, called the "Tazewell Advance/'<br />

apparently carried the Wisconsin icecap to its maximum<br />

extension and greatest volume.<br />

d. <strong>The</strong> Tazewell Advance was interrupted <strong>by</strong> a prolonged<br />

period <strong>of</strong> warmth and recession called the "Brady Interval"<br />

or "Brady Interstadial." This lasted between three and four<br />

thousand years. It began before 16,720 years ago, and ended<br />

sometime after 14,042 years ago. <strong>The</strong> ice retreated a long<br />

way.<br />

e. A fourth advance <strong>of</strong> the ice sheet beginning about<br />

13,600 years ago, and continuing to about 12,120 years ago<br />

(called the "Gary Advance"), was followed <strong>by</strong> the "Two<br />

Creeks Interstadial," an interval <strong>of</strong> warmth and recession,<br />

about 11,404 years ago.<br />

f. A fifth advance <strong>of</strong> the ice, referred to as the "Mankato<br />

Advance," appears to have taken place between 10,856 and<br />

8,200 years ago. <strong>The</strong> high point <strong>of</strong> this advance is called the<br />

"Mankato Maximum." Another writer, Emiliani, finds that<br />

a sixth expansion <strong>of</strong> the ice sheet, the "Cochrane Advance,"<br />

took place less than 7,000 years ago (132).<br />

g. <strong>The</strong>re was a sudden, virtually complete disappearance<br />

<strong>of</strong> the ice sheet (which had, however, according to Flint, been<br />

getting thinner ever since the Tazewell Advance) (375:177).<br />

It disappeared in an extraordinarily short period, as shown<br />

<strong>by</strong> a postglacial date from Cochrane, Ontario, 6,380 years ago.<br />

h. <strong>The</strong> significance <strong>of</strong> the postglacial date from Ontario<br />

(close to the center <strong>of</strong> the former ice sheet) is increased when<br />

we it compare with the date <strong>of</strong> the postglacial Climatic Op<br />

timum, which Flint finds to have occurred between 6,000 and<br />

4,000 years ago. <strong>The</strong> climate during the Optimum, according<br />

to Brooks (52:296-97), averaged about 5 degrees warmer<br />

than at present. <strong>The</strong>re is a very difficult problem here <strong>of</strong> ac-<br />

counting for the velocity <strong>of</strong> these events. It is obvious that<br />

the cold glacial climate <strong>of</strong> North America must have warmed<br />

up to something like the present prevailing temperatures<br />

before it could warm up still further to the point reached<br />

in the Optimum. But if so, could the whole wanning process

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