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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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56<br />

EARTH'S SHIFTING CRUST<br />

have three cores taken some distance apart that seem, never-<br />

theless, to agree pretty well with each other, even though<br />

there are evidences <strong>of</strong> some disturbance, and their evidence<br />

is strengthened <strong>by</strong> their agreement<br />

with the Arctic cores to<br />

be discussed later on.<br />

From our point <strong>of</strong> view, the precise accuracy <strong>of</strong> the dating<br />

is less important than the evidence that, in very recent time,<br />

there was deposition <strong>of</strong> temperate type sediment in the Ross<br />

Sea <strong>of</strong>f the Antarctic coast.<br />

6. Conclusion<br />

It is clear that none <strong>of</strong> the great glaciations <strong>of</strong> the past can<br />

be explained <strong>by</strong> the theories hitherto advanced. <strong>The</strong> only<br />

ice age that is adequately explained is the present ice age in<br />

Antarctica. This is excellently explained. It exists, quite obvi-<br />

ously, because Antarctica is at the pole, and for no other<br />

reason. No variation <strong>of</strong> the sun's heat, no galactic dust, no<br />

volcanism, no subcrustal currents, and no arrangements <strong>of</strong><br />

land elevations or sea currents account for the fact. We may<br />

conclude that the best theory to account for an ice age is<br />

that the area concerned was at a pole. We thus account for<br />

the Indian and African ice sheets, though the areas once occupied<br />

<strong>by</strong> them are now in the tropics. We account for all ice<br />

sheets <strong>of</strong> continental size in the same way.<br />

Stokes has provided an excellent list <strong>of</strong> specifications for a<br />

satisfactory ice age theory, every one <strong>of</strong> which is met <strong>by</strong> the<br />

assumption <strong>of</strong> crust displacements as the fundamental cause<br />

(405:815-16):<br />

a. An initiating event or condition.<br />

b. A mechanism for cyclic repetitions or oscillations within<br />

the general period <strong>of</strong> glaciation.<br />

c. A terminating condition or event.<br />

d. It should not rely upon unprovable, unobservable, or<br />

unpredictable conditions, when well-known or more<br />

simple ones will suffice.

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