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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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THE SHAPE OF THE EARTH 163<br />

ment within the rigid crust itself. <strong>The</strong>y remark: ". . . it<br />

for the strains due to the re-<br />

requires several thousand years<br />

moval <strong>of</strong> the ice load to be reduced to half" (195:101). This<br />

and the preceding statements may serve to establish the rea-<br />

sonable presumption that any icecap, at the height <strong>of</strong> its<br />

rapid accumulation, must be largely uncompensated.<br />

But even if, during the rapid growth <strong>of</strong> the present An-<br />

tarctic icecap, a degree <strong>of</strong> isostatic adjustment has taken<br />

place, this does not end the matter for us. We must ask,<br />

Where does this plastic rock go? Presumably it flows out,<br />

under the crust below the ocean bed, beyond the fringes <strong>of</strong><br />

the ice-covered continent, at a depth <strong>of</strong> twenty to forty miles<br />

below the surface <strong>of</strong> the earth. It may raise the crust somewhat<br />

for a distance beyond the edges <strong>of</strong> the ice sheet. Dr.<br />

Harold Jeffreys gave it as his opinion that, if a gravity survey<br />

<strong>of</strong> Antarctica should be undertaken, we might expect to<br />

find marked positive anomalies around the coasts (241). But,<br />

since in general the plastic rock under the crust is not flowing<br />

into any area <strong>of</strong> deficient mass, the flow, upraising the coasts<br />

or the sea bottoms <strong>of</strong>f the coasts, must still constitute excess<br />

matter, and must exert a centrifugal effect about equal to<br />

the former effect <strong>of</strong> the ice that has now been brought into<br />

equilibrium.<br />

Let us consider this point a little further. We have noted,<br />

above, that according to the definition <strong>of</strong> isostasy, the process<br />

is a response to the transfer <strong>of</strong> material from one region to<br />

another: sediment is removed from an area <strong>of</strong> "denudation"<br />

and transferred to an area <strong>of</strong> "deposition." <strong>The</strong> area <strong>of</strong> deposition,<br />

then, sinks under the load, and a flow <strong>of</strong> rock under<br />

the crust moves back to the area <strong>of</strong> denudation, compen-<br />

sating for the material that has been removed, and restoring<br />

the equilibrium. But where can the plastic rock displaced<br />

<strong>by</strong> the icecap flow? No adjacent area ha$ been lightened <strong>by</strong><br />

the removal <strong>of</strong> sediment; the plastic rocK must, then, wherever<br />

it flows, create a distortion, a surplus <strong>of</strong> matter, which<br />

will have a centrifugal effect.<br />

From the standpoint <strong>of</strong> the theory presented in this book,

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