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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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NORTH AMERICA AT THE POLE 205<br />

A special phase <strong>of</strong> the volcanism must now attract our at-<br />

tention. Most volcanoes produce dust, sometimes in vast<br />

quantities (87:271). This dust is rapidly distributed through<br />

the atmosphere. <strong>The</strong> effects <strong>of</strong> volcanic dust on the climate<br />

have been the subject <strong>of</strong> intensive studies (231, 375). We must<br />

stop for a moment to summarize the essential results <strong>of</strong> these<br />

studies.<br />

<strong>The</strong> fundamental work on the relationship <strong>of</strong> volcanic<br />

dust to climate is <strong>The</strong> Physics <strong>of</strong> the Air, <strong>by</strong> Humphreys,<br />

which has been cited in earlier chapters. Humphreys shows<br />

that volcanic dust can have a remarkable effect in lowering<br />

temperature. He points out that the effect <strong>of</strong> the particles<br />

depends upon whether they happen to be more efficient in<br />

intercepting the sun's light and reflecting it back into space<br />

than they are in preventing the radiation <strong>of</strong> the earth's heat<br />

into outer space. What is important is the size and shape <strong>of</strong><br />

the dust particles as compared with the wave lengths <strong>of</strong> the<br />

radiation. Particles <strong>of</strong> a given length will have great reflecting<br />

and scattering power on sunlight, and none on the<br />

radiation <strong>of</strong> heat from the earth (which, <strong>of</strong> course, is not<br />

in the form <strong>of</strong> light). Humphreys concludes that it is neces-<br />

sary to determine the approximate average size <strong>of</strong> the individual<br />

grains <strong>of</strong> floating volcanic dust, as well as the wave<br />

lengths <strong>of</strong> the radiation involved. He accomplishes this satisfactorily.<br />

After mathematical treatment <strong>of</strong> the various factors<br />

he concludes: ". . . the shell <strong>of</strong> volcanic dust, the particles<br />

all being <strong>of</strong> the size given, is some thirty fold more effective<br />

in shutting out solar radiation than it is in keeping terrestrial<br />

radiation in. . . ." (231:580). He also points out:<br />

. . . <strong>The</strong> total quantity <strong>of</strong> dust sufficient ... to cut down the<br />

intensity <strong>of</strong> solar radiation <strong>by</strong> 20% ... is astonishingly small only<br />

<strong>of</strong> a cubic mile. . . .<br />

i74th part <strong>of</strong> a cubic kilometer, or the 727th part<br />

(231:583).<br />

This, <strong>of</strong> course, means that the sun's radiation is reduced<br />

to this extent over the whole surface <strong>of</strong> the earth. It re-<br />

quires only a few days for volcanic dust projected into the

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