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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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322<br />

EARTH'S SHIFTING CRUST<br />

To recapitulate what has already been said, if drastic climatic<br />

and geographical change is the most obvious factor<br />

to which to look for changes in life forms, then it is to the<br />

acceleration <strong>of</strong> that factor that we must look for the accelera-<br />

tion <strong>of</strong> evolution. In the previous chapters we have been led<br />

again and again <strong>by</strong> the force <strong>of</strong> the evidence to the concept<br />

<strong>of</strong> displacements <strong>of</strong> the earth's crust. <strong>The</strong>re is no reasonable<br />

doubt as to the effect that such displacements, at relatively<br />

short intervals, would have on the tempo <strong>of</strong> evolution. <strong>The</strong>y<br />

could not fail enormously to accelerate the several aspects <strong>of</strong><br />

the evolutionary process. Let us now examine some <strong>of</strong> these<br />

special aspects in more detail.<br />

Wright has pointed out that the rate <strong>of</strong> evolutionary<br />

change may have been accelerated at various times through<br />

the mass transformation <strong>of</strong> one kind <strong>of</strong> plant or animal into<br />

another (115:314). This requires that all over the area <strong>of</strong><br />

distribution <strong>of</strong> the life form in question there must be strong<br />

pressure for change in the same direction. This means that<br />

similar new varieties would appear simultaneously and independently<br />

in countless localities or that well-adapted new<br />

varieties would spread and become established rapidly. Quite<br />

this would tend to accelerate evolution.<br />

obviously<br />

But how would such mass transformation be brought<br />

about? It could only result from pr<strong>of</strong>ound transformation <strong>of</strong><br />

the environment. <strong>The</strong> required change would have to be<br />

general and would have to tend in the same direction for a<br />

considerable period <strong>of</strong> time. No short-range fluctuations and,<br />

above all, no merely local climatic changes would suffice. A<br />

displacement <strong>of</strong> the crust appears to meet all these requirements.<br />

For a period <strong>of</strong> many thousands <strong>of</strong> years, some areas,<br />

moving toward the equator, would be growing warmer;<br />

others, moving toward the poles, would be growing colder.<br />

In the areas moving toward the equator (not necessarily<br />

reaching the equator, however, or even the tropics) the increase<br />

<strong>of</strong> sunlight would mean more luxuriant life condi-<br />

tions; for many species this might mean increased food<br />

supplies and an extended distribution. It would also be likely

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