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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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290<br />

EARTH'S SHIFTING CRUST<br />

side may have been nonglacial. Thus sediment <strong>of</strong> both kinds<br />

could be deposited in different parts <strong>of</strong> the Ross Sea at the<br />

same time, depending, perhaps, to some extent, on the local<br />

peculiarities <strong>of</strong> bottom topography and bottom currents. It<br />

cannot be assumed, <strong>of</strong> course, that the outlines <strong>of</strong> the continent,<br />

or the depths <strong>of</strong> the surrounding oceans, were the same<br />

at that time as they are now. However, those who may still<br />

be inclined to discount the theory presented in this book<br />

must be reminded that all the phenomena discussed in this<br />

chapter and all the principal phenomena discussed in this<br />

book have been hitherto unexplained. It is not a question<br />

<strong>of</strong> choosing between explanations. <strong>The</strong>re is, at the present<br />

time, no other explanation than ours <strong>of</strong> these facts.<br />

a. Cores from the San Augustin Plains<br />

A good deal <strong>of</strong> evidence from other cores supports this suc-<br />

cession <strong>of</strong> polar positions in Greenland and Hudson Bay.<br />

Let us consider first a very interesting study recently made in<br />

New Mexico. <strong>The</strong>re a group <strong>of</strong> scientists have been studying<br />

a very long sedimentary core taken from the San Augustin<br />

Plains. On these plains, sediments have accumulated to a<br />

great depth without consolidating into rock, so it has been<br />

possible to bore down about 645 feet and get a cross section<br />

<strong>of</strong> all the deposits to that depth. <strong>The</strong>se sediments contain<br />

pollen <strong>of</strong> various trees and plants, which, as is well known,<br />

does not easily disintegrate, but remains preserved in the soil<br />

for very long periods. In this core, different kinds <strong>of</strong> pollen<br />

in the different layers indicated changes in the species <strong>of</strong> trees<br />

and plants growing in the region, and <strong>of</strong> course changes in<br />

the kinds <strong>of</strong> plants growing in a region indicate changes <strong>of</strong><br />

climate. For the upper and most recent part <strong>of</strong> the core, it<br />

was possible to use the radiocarbon method to date the<br />

changes in pollen types, and therefore in climate.<br />

Figure VIII (opposite page), prepared <strong>by</strong> Drs. Clis<strong>by</strong> and<br />

Sears (84), shows the climatic curve for the upper 330 feet<br />

<strong>of</strong> the core. <strong>The</strong> radiocarbon date at 27,000 years ago plus

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