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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 />

he would have trouble in finding a reasonable basis for the<br />

latter conclusion.<br />

We can therefore conclude that, on the whole, the North<br />

American icecap is a good candidate for the position <strong>of</strong> prime<br />

mover in the last displacement <strong>of</strong> the crust. <strong>The</strong> argument<br />

will be strengthened when we consider, below, its detailed<br />

history, and the implications <strong>of</strong> the extraordinary tempo <strong>of</strong><br />

its development and <strong>of</strong> its subsequent decay. <strong>The</strong> essential<br />

argument in favor <strong>of</strong> icecaps is the time factor, for the rate<br />

<strong>of</strong> their accumulation and <strong>of</strong> their melting is obviously many<br />

times faster than that <strong>of</strong> any other process creating unbalance<br />

in the distribution <strong>of</strong> materials on the earth's surface.<br />

Horberg has recently collected and studied, as already<br />

mentioned, the radiocarbon dates bearing on the history <strong>of</strong><br />

the Wisconsin ice sheet. According to him, the following is<br />

its short and violent history (222:281):<br />

a. <strong>The</strong> first known advance <strong>of</strong> the icecap its first appearance<br />

in Ohio is dated at merely 25,100 years ago. This<br />

is called the "Farmdale Advance." It was formerly thought<br />

to have occurred as much as 100,000 or even 150,000 years<br />

ago. This date, then, cuts the time for the later history <strong>of</strong><br />

the ice sheet <strong>by</strong> about three quarters. Six different radiocarbon<br />

dates, all <strong>of</strong> the Farmdale Advance, show that the ex-<br />

pansion continued until at least 22,900 years ago, or for<br />

about 3,000 years. <strong>The</strong>n there was an unexplained interval<br />

<strong>of</strong> warm climate (which I will explain later on), called the<br />

"Farmdale-Iowan Interstadial." This warm period lasted<br />

about 1,500 years, during which the ice withdrew a certain<br />

distance.<br />

b. Following the recession, a new advance <strong>of</strong> the icecap<br />

occurred. This is referred to as the "lowan Advance." It<br />

began about 21,400 years ago, lasted about 700 years, and<br />

was interrupted <strong>by</strong> a new recession about 20,700 years ago.<br />

c. This second recession, after less than a thousand years,<br />

was succeeded <strong>by</strong> an extremely massive advance during the<br />

period from 19,980 to 18,050 years ago.<br />

<strong>The</strong>se dates must<br />

not be taken as absolutely exact; there is always a small mar-

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