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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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CAMPBELL'S MECHANISM 371<br />

feet will tend to propel a mass in this equipotential surface<br />

toward the equator, and no gravitational effect will tend to<br />

propel it toward the poles. <strong>The</strong> fact that the force <strong>of</strong> gravity<br />

is absolutely much greater than the centrifugal effect <strong>of</strong> the<br />

rotation is shown <strong>by</strong> the fact that the flattening <strong>of</strong> the earth<br />

is very slight. <strong>The</strong> equatorial bulge amounts to 6.7 miles in<br />

comparison with the earth's mean radius <strong>of</strong> 4,000 miles. This<br />

is a ratio <strong>of</strong> only .017 per cent.<br />

<strong>The</strong> past century has been notable for extensive studies<br />

<strong>of</strong> the effects <strong>of</strong> gravity at the earth's surface. <strong>The</strong> theory <strong>of</strong><br />

isostasy has been developed, and the actually existing state <strong>of</strong><br />

balance <strong>of</strong> the surface features <strong>of</strong> the earth's crust has been<br />

measured in various ways and for various purposes. As we<br />

have seen, there are various difficulties with the theory <strong>of</strong><br />

isostasy, some <strong>of</strong> which may be soluble in terms <strong>of</strong> the theory<br />

presented in this book. At the same time, but independently,<br />

studies <strong>of</strong> centrifugal effects at the earth's surface have been<br />

undertaken. Eotvos investigated the centrifugal effects that<br />

would arise if a given mass had its center <strong>of</strong> gravity above<br />

the equipotential surface. This could occur even with masses<br />

in isostatic equilibrium. To visualize this case, we may take<br />

the example <strong>of</strong> a block <strong>of</strong> ice floating in water.<br />

Ice is lighter than water. When a block <strong>of</strong> ice falls into<br />

a body <strong>of</strong> water it displaces its own weight <strong>of</strong> water, and<br />

then floats with a tenth <strong>of</strong> its mass above the water level. It<br />

is now in equilibrium, or in isostatic adjustment, even<br />

though its upper part projects a considerable distance up out<br />

<strong>of</strong> the water. This upper tenth, in the meantime, has dis-<br />

placed air, not water. It is a solid mass <strong>of</strong> far greater density<br />

than the air it has displaced. Its center <strong>of</strong> gravity, midway<br />

between its summit and the water surface, is farther from<br />

the axis <strong>of</strong> rotation <strong>of</strong> the earth than was that <strong>of</strong> the mass<br />

<strong>of</strong> water it has displaced. Since points move faster with the<br />

earth's rotation the farther they are from this axis, this mass<br />

has now been given added velocity. Added velocity means<br />

an increase in the centrifugal effect, and one not compensated<br />

<strong>by</strong> gravity, since the amount <strong>of</strong> mass is the same as before,

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