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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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46<br />

EARTH'S SHIFTING CRUST<br />

much evidence, but it was ignored. When the Swedish scien*<br />

tist Gerard de Geer established <strong>by</strong> clay varve counting that<br />

the ice sheet was withdrawing from Sweden as recently as<br />

13,000 years ago, the implications were not really accepted,<br />

nor were his results popularly known. Books continued to appear,<br />

even thirty years afterwards, with the original estimates<br />

<strong>of</strong> the age <strong>of</strong> the icecap.<br />

<strong>The</strong>n, following World War II, nuclear physics made pos-<br />

sible the development <strong>of</strong> new techniques for dating geolog-<br />

ical events. One <strong>of</strong> these was radiocarbon dating.<br />

<strong>The</strong> method <strong>of</strong> radiocarbon dating was developed <strong>by</strong><br />

Willard F. Lib<strong>by</strong>, nuclear physicist <strong>of</strong> the University <strong>of</strong> Chi-<br />

cago, now a member <strong>of</strong> the United States Atomic Energy<br />

Commission. It uses an isotope <strong>of</strong> carbon (Carbon 14) which<br />

has a "half-life" <strong>of</strong> about 5,568 years (115:75). A "half-life"<br />

is the period during which a radioactive substance loses half<br />

its mass <strong>by</strong> radiation. Among the very numerous artificial<br />

radioactive elements created in nuclear explosions some have<br />

half-lives <strong>of</strong> millionths <strong>of</strong> seconds; others, occurring<br />

in na-<br />

ture, have half-lives <strong>of</strong> millions <strong>of</strong> years. For geological dating<br />

it is necessary to have radioactive elements that diminish significantly<br />

during the periods that have to be studied, and<br />

that occur in nature.<br />

Since radiocarbon exists in nature, and has a relatively<br />

short half-life, the quantity <strong>of</strong> it in any substance containing<br />

organic carbon will decline perceptibly in periods <strong>of</strong> a few<br />

centuries. By finding out how much carbon was contained<br />

originally in the specimen and then measuring what still re-<br />

mains, the date can be found to within a small margin <strong>of</strong><br />

error.<br />

When this method was first developed <strong>by</strong> Lib<strong>by</strong>, it could<br />

date anything containing carbon <strong>of</strong> organic origin back to<br />

about 20,000 years ago.<br />

Since then the method has been im-<br />

proved, through the efforts <strong>of</strong> many scientists, and its range<br />

has been nearly doubled.<br />

<strong>The</strong> first major result <strong>of</strong> the radiocarbon method was the

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