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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 349<br />

wedge, which has the effect <strong>of</strong> multiplying the effect <strong>of</strong> an<br />

applied force. This principle is usually given as follows:<br />

<strong>The</strong> wedge is a pair <strong>of</strong> inclined planes united <strong>by</strong> their bases. In the<br />

application <strong>of</strong> pressure to the head or butt end <strong>of</strong> the wedge, to<br />

cause it to penetrate a resisting body, the applied force is to the<br />

resistance as the thickness <strong>of</strong> the wedge is to its length (249:512).<br />

This statement means that a wedge multiplies the splitting<br />

power (or bursting stress) produced <strong>by</strong> an applied force in<br />

the proportion <strong>of</strong> the length <strong>of</strong> the wedge to its thickness at<br />

the butt end. Figure XV shows the application <strong>of</strong> this principle<br />

to the earth. <strong>The</strong> formula for calculating the wedge<br />

effect is presented at the extreme left, where P = pressure (as<br />

thrust <strong>of</strong> the icecap transmitted to the crust), Q = the mutual<br />

pressure between crust and bulge, or bursting stress, h = the<br />

height (that is, the length) <strong>of</strong> the wedge, and b = the base or<br />

butt end. <strong>The</strong> bursting stress equals the pressure applied to<br />

the butt and multiplied <strong>by</strong> the ratio <strong>of</strong> the thickness <strong>of</strong> the<br />

butt end to the length <strong>of</strong> the wedge. <strong>The</strong> length <strong>of</strong> the wedge,<br />

in this case, is about 6,000 miles, and its thickness at the butt<br />

end is 6.67 miles, so that the ratio is about 1,000:1, and the<br />

quantity <strong>of</strong> the thrust <strong>of</strong> the icecap should consequently be<br />

multiplied <strong>by</strong> 1,000; however, there are two wedges, one on<br />

each side <strong>of</strong> the earth, and therefore the thrust is multiplied<br />

only 500 times. Nevertheless, the significance <strong>of</strong> such a multi-<br />

is self-evident.<br />

plication <strong>of</strong> the effect <strong>of</strong> the icecap<br />

It was not a simple matter to apply the principle <strong>of</strong> the<br />

wedge to the earth. As in the case <strong>of</strong> the principle <strong>of</strong> the<br />

parallelogram, the formula could not simply be copied from<br />

a textbook; it had to be imaginatively applied. For example,<br />

in the diagram P, or is pressure, shown exerted on the butt<br />

end, like a sledge hammer hitting the butt end <strong>of</strong> a wedge to<br />

split a log. But obviously, the thrust <strong>of</strong> the icecap is not, in<br />

the first instance, applied in this way. It takes an act <strong>of</strong> the<br />

to realize that in effect it amounts to the same<br />

imagination<br />

thing. <strong>The</strong> icecap is really pushing or pulling the crust<br />

toward the equator on both sides <strong>of</strong> the earth, but the matter

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