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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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LIFE 331<br />

could utilize it, but after two billion or more years <strong>of</strong> evolu-<br />

tion, such primeval biological vacuums are few indeed. Life<br />

niches have, in general, been very well occupied for a very<br />

long time. Something is required, therefore, to empty them.<br />

This is where our theory comes in. <strong>The</strong> effects <strong>of</strong> a dis-<br />

placement can be visualized in two stages. In the first, a<br />

movement <strong>of</strong> a large continental area through many degrees<br />

<strong>of</strong> latitude might well cause a very general extermination<br />

<strong>of</strong> the inhabitants. We have seen how, in several instances,<br />

this occurred during the late Pleistocene (Chapter VIII).<br />

<strong>The</strong> consequence <strong>of</strong> the extermination <strong>of</strong> many kinds <strong>of</strong><br />

plants and animals (which is not to say their extinction, for<br />

would be to leave<br />

many <strong>of</strong> them might survive in other areas)<br />

their life niches empty.<br />

<strong>The</strong> second stage, initiated <strong>by</strong> a new movement <strong>of</strong> the<br />

crust, would be marked <strong>by</strong> the opening up <strong>of</strong> avenues for the<br />

immigration<br />

<strong>of</strong> life forms from other land areas. Life forms<br />

entering the continent would now enjoy a field day. <strong>The</strong>y<br />

would multiply; they would occupy rapidly a tremendous<br />

area and all manner <strong>of</strong> habitats; they would produce variant<br />

forms, and the variant forms would occupy appropriate<br />

niches. Thus explosive evolution would take place. <strong>The</strong> new<br />

forms need not always be immigrants; they could equally<br />

well be local survivors <strong>of</strong> the period <strong>of</strong> depopulation, <strong>of</strong> the<br />

displacement, who had somehow managed to hold their own<br />

under unfavorable conditions. It seems highly probable,<br />

indeed, that displacements <strong>of</strong> the earth's crust are the ex-<br />

planation <strong>of</strong> explosive evolution.<br />

We have already made mention <strong>of</strong> the fact that an interrelationship<br />

between the revolutionary periods in evolution and<br />

the critical phases <strong>of</strong> change in other geological areas has<br />

been noted <strong>by</strong> many observers. Lull, for example, says,<br />

. . . <strong>The</strong>re are times <strong>of</strong> quickening, the expression points <strong>of</strong> evo-<br />

lution, which are almost invariably coincident with some great geological<br />

change, and the correspondence is so exact and so frequent that<br />

the laws <strong>of</strong> chance may not be invoked as an explanation (278:687).

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