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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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206<br />

EARTH'S SHIFTING CRUST<br />

upper atmosphere to be distributed around the world. Apparently,<br />

the amount <strong>of</strong> dust produced <strong>by</strong> the eruption <strong>of</strong><br />

Mt. Katmai in Alaska in 1912 was sufficient slightly to lower<br />

the temperature <strong>of</strong> the whole earth's surface for a period <strong>of</strong><br />

two or three years (87:270; 231:569). For long-range effects<br />

a continuous series <strong>of</strong> explosions would be necessary, because<br />

volcanic dust settles out <strong>of</strong> the atmosphere in periods <strong>of</strong> the<br />

order <strong>of</strong> three years. Humphreys presents a great deal <strong>of</strong> evi-<br />

dence correlating variations in average annual global tem-<br />

peratures through the nineteenth century, with specific volcanic<br />

eruptions. He establishes the fact that the eruptions<br />

certainly had an important influence.<br />

If this is true <strong>of</strong> our times, what should we expect to result<br />

from the activation <strong>of</strong> very great numbers <strong>of</strong> volcanoes dur-<br />

ing a displacement <strong>of</strong> the crust? Not only would the temperature<br />

fall, and perhaps very drastically, but continuing vol-<br />

canic outbursts would keep it low. At the same time, the<br />

alternation <strong>of</strong> periods <strong>of</strong> massive outbursts with periods <strong>of</strong><br />

quiet would produce violent variations <strong>of</strong> the climate, between<br />

extremes <strong>of</strong> cold and warmth.<br />

Here we have our explanation <strong>of</strong> the five or six major<br />

readvances <strong>of</strong> the Wisconsin ice sheet (there were, appar-<br />

ently, many more minor ones). In all probability, they resulted<br />

from the long continuation <strong>of</strong> massive outbursts <strong>of</strong><br />

volcanism. <strong>The</strong> readvances <strong>of</strong> the ice are explained <strong>by</strong> vol-<br />

canism, and the volcanism is explained <strong>by</strong> the displacement<br />

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

It is not necessary, however, for us merely to assume with-<br />

out evidence that there must have been unusual volcanic<br />

activity at the end <strong>of</strong> the ice age. On the contrary, there is a<br />

rather remarkable amount <strong>of</strong> evidence <strong>of</strong> excessive volcanism<br />

It comes from<br />

during the decline <strong>of</strong> the Wisconsin icecap.<br />

many parts <strong>of</strong> the earth. For North America it is particularly<br />

rich. From radiocarbon dating we have learned that during<br />

the last part <strong>of</strong> the ice age there were active volcanoes in our<br />

northwestern states. One <strong>of</strong> the greatest eruptions was that<br />

<strong>of</strong> Mt. Newberry in southern Oregon less than 9,000 years

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