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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 323<br />

to mean increased competition with other forms. Many<br />

effects would depend upon whether the displacement carried<br />

the area in question into the wet tropics or into the dry horse<br />

latitudes, or merely from an arctic into a temperate climate.<br />

Meanwhile, <strong>of</strong> course, in areas displaced poleward, opposite<br />

trends would exist; here the forms <strong>of</strong> life would have to adapt<br />

to diminishing light, to increased cold, to decreased food<br />

supplies.<br />

What is important is that these changes <strong>of</strong> climate would<br />

apply over great areas <strong>of</strong> the earth. In one movement <strong>of</strong> the<br />

crust, two opposite quarters <strong>of</strong> the earth's surface would be<br />

moving equatorward while two others were moving poleward.<br />

Thus the climatic changes would be in the same direc-<br />

tion over very great areas: the entire distribution, perhaps,<br />

<strong>of</strong> many plants and animals. Mass transformation <strong>of</strong> life<br />

forms might therefore be expected to occur; not mass trans-<br />

formations <strong>of</strong> all life forms, <strong>of</strong> course, but merely one or two<br />

short steps in the mass transformation <strong>of</strong> one or a few kinds<br />

<strong>of</strong> plants or animals. New varieties might be established in<br />

great numbers, during a single movement <strong>of</strong> the crust; but<br />

<strong>by</strong> this I do not mean to imply that many new "species"<br />

would be. <strong>The</strong> latter may be the end results <strong>of</strong> a considerable<br />

number <strong>of</strong> displacements <strong>of</strong> the crust. I hope that the reader<br />

will not ask me to define "species." In this book I use the<br />

term simply to denote forms <strong>of</strong> life that are reasonably dis-<br />

tinct and relatively permanent.<br />

We must remember that the different areas <strong>of</strong> the earth's<br />

surface would be unequally shifted in a crust displacement.<br />

I have explained (Introduction) that the amount <strong>of</strong> the dis-<br />

placement would depend on whether an area was near to, or<br />

distant from, the meridian <strong>of</strong> displacement. Selection pres-<br />

sures would vary accordingly.<br />

Since we consider displacements to have taken place in<br />

short periods <strong>of</strong> the order <strong>of</strong> 10 or 20 thousand years, it seems<br />

likely that most plants and animals in areas radically dis-<br />

placed <strong>by</strong> a given movement would be unlikely to succeed<br />

in adapting. Some would migrate into areas having climates

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