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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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EARTH'S SHIFTING CRUST<br />

cap is largely or entirely uncompensated isostatically. <strong>The</strong><br />

other assumption is that at some point below the crust a weak<br />

layer exists that will permit the displacement<br />

<strong>of</strong> the crust<br />

over it. <strong>The</strong> first assumption is capable <strong>of</strong> verification, and<br />

may even be verified in the course <strong>of</strong> the current Geophysical<br />

Year. This will depend, however, on whether the new gravity<br />

data that are to be collected during this year are reduced <strong>by</strong><br />

formulas based on correct assumptions. <strong>The</strong>re is no present<br />

prospect <strong>of</strong> direct verification <strong>of</strong> the second assumption.<br />

However, the body <strong>of</strong> geological evidence presented in this<br />

book provides very strong indirect support for both these<br />

assumptions.<br />

As to the mechanics <strong>of</strong> crust displacements, Campbell has<br />

provided the necessary constructions. To some, the simplicity<br />

<strong>of</strong> his thought may be unnerving, but I feel assured that in<br />

the end this simplicity itself will be the justification for reposing<br />

wide confidence in this theory. For it appears that no<br />

recondite principle can vitiate it. Who can argue with formulas<br />

so simple that a high school student can, and usually<br />

does, master them?<br />

In addition to the support provided <strong>by</strong> evidence from the<br />

field, our theory receives support from logic. It has been<br />

recognized<br />

that one characteristic <strong>of</strong> sound new theories is<br />

the simplicity <strong>of</strong> their basic assumptions, and another is their<br />

capacity to explain a greater number <strong>of</strong> facts or a greater<br />

range <strong>of</strong> problems than previous theories. It was the sim-<br />

plicity <strong>of</strong> this theory that first aroused the interest <strong>of</strong> Einstein,<br />

in whose philosophy <strong>of</strong> science simplicity was a prime con-<br />

sideration. It appeared to him also that it might explain a<br />

far greater number <strong>of</strong> facts than were explainable <strong>by</strong> the<br />

various theories that have been produced to explain the lead-<br />

ing problems <strong>of</strong> the earth separately.<br />

I shall have to admit that the full development <strong>of</strong> the im-<br />

plications <strong>of</strong> crust displacements, for all the affected fields,<br />

has carried me much further than I originally expected.<br />

When I resurvey the structure that has now been erected on<br />

the basis <strong>of</strong> the simple basic theory, I feel exactly as Sir James

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