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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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CONCLUSION 387<br />

present time are discussing polar shift, but none <strong>of</strong> them has<br />

as yet suggested an acceptable mechanism.<br />

<strong>The</strong> general evidence for displacements <strong>of</strong> the crust is ex-<br />

ceedingly rich. In turn, the assumption <strong>of</strong> such displacements<br />

serves to solve a wide range <strong>of</strong> problems, such as the causes<br />

<strong>of</strong> ice ages, warm polar climates, mountain building; it pro-<br />

vides a mechanism that may account for changes in the eleva-<br />

tions <strong>of</strong> land areas and in the topography <strong>of</strong> the ocean floors;<br />

it also provides a basis for the resolution <strong>of</strong> conflicts in iso-<br />

static theory. For the period <strong>of</strong> the late Pleistocene, the theory<br />

permits the construction <strong>of</strong> a chronology <strong>of</strong> polar shifts, with<br />

three successive tentative polar positions in Alaska, Green-<br />

land, and Hudson Bay preceding the present position <strong>of</strong> the<br />

pole. <strong>The</strong> evidence for the location <strong>of</strong> the Hudson Bay<br />

region at the pole during the last North American ice age is<br />

overwhelming, and this fact in itself provides the principal<br />

support for the assumption <strong>of</strong> the earlier shifts. <strong>The</strong> tempo<br />

<strong>of</strong> change indicated for the late Pleistocene is reflected in<br />

evidence from earlier geological periods.<br />

<strong>The</strong> theory is able to explain not only the general succes-<br />

sion <strong>of</strong> climatic changes in various parts <strong>of</strong> the world in the<br />

late Pleistocene; it can account also for the detailed history<br />

<strong>of</strong> the last North American icecap. It can explain the fluctua-<br />

tions <strong>of</strong> that icecap, its repeated retreats and readvances. It<br />

shows that the effects <strong>of</strong> volcanism were directly responsible<br />

for the oscillations. It shows also that these same effects,<br />

added to the effects <strong>of</strong> gradual climatic change, were responsible<br />

for the widespread extinctions <strong>of</strong> species at the end <strong>of</strong> the<br />

Pleistocene, and from this we may assume that the same<br />

cause was responsible for numerous extinctions in earlier<br />

geological periods. By providing<br />

a reasonable basis for the<br />

assumptions <strong>of</strong> rapid climatic change and rapid topographical<br />

change (including the existence <strong>of</strong> former continents and<br />

land bridges), the theory provides solutions for many prob-<br />

lems in the evolution and distribution <strong>of</strong> species.<br />

Our theory <strong>of</strong> displacement depends upon two assump-<br />

tions, and on two only. One <strong>of</strong> these is that a continental ice-

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