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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<br />

ago (242:23). Other late glacial or early postglacial volcanic<br />

activity in Oregon was reported <strong>by</strong>* Hansen (199). Farther<br />

south the story is the same:<br />

In Arizona, New Mexico and southern California there are very<br />

fresh looking volcanic formations. <strong>The</strong> lava flow in the valley <strong>of</strong> the<br />

San Jose River in New Mexico is so fresh that it lends support to<br />

Indian traditions <strong>of</strong> a "river <strong>of</strong> fire" in this locality (235:113).<br />

Volcanic disturbances in South America about 9,000 years<br />

ago have been dated <strong>by</strong> radiocarbon (242:45). Huntington<br />

reported "lava flows <strong>of</strong> the glacial period interstratified with<br />

piedmont gravel" in Central Asia (232:168). Ebba Hult de<br />

Geer quoted Franz Firbaz as follows: "<strong>The</strong> volcanic eruptions<br />

that produced the Laacher marine volcanic ash are<br />

about 11,000 years old, or a little older. . . ." (108:515).<br />

Hibben suggested that the extinctions <strong>of</strong> animals in Alaska<br />

at the end <strong>of</strong> the ice age may have been due to terrific vol-<br />

canic eruptions there, <strong>of</strong> which the evidence is plentiful<br />

(218). We will return to his account later.<br />

Volcanic dust is not the only important product <strong>of</strong> volcanic<br />

eruptions. <strong>The</strong>y also produce vast quantities <strong>of</strong> carbon dioxide<br />

gas. Tazieff, for example, estimated that in one eruption<br />

he observed in Africa, along with about seventy-eight mil-<br />

lion tons <strong>of</strong> lava, the volcano emitted twenty billion cubic<br />

yards <strong>of</strong> gas (416:217), not all <strong>of</strong> which, <strong>of</strong> course, was carbon<br />

dioxide.<br />

<strong>The</strong> carbon dioxide emitted <strong>by</strong> volcanoes has an important<br />

effect on global temperature, but one quite different from<br />

the effect <strong>of</strong> the volcanic dust. Being a translucent gas, it does<br />

not interfere with the entrance <strong>of</strong> sunlight, <strong>of</strong> radiant heat,<br />

into the atmosphere. But it is opaque to the radiation <strong>of</strong><br />

the earth's heat into outer space. A small quantity <strong>of</strong> the<br />

gas will act effectively to prevent loss <strong>of</strong> heat from the earth's<br />

surface. A considerable increase in this small percentage will<br />

tend to raise the average temperatures <strong>of</strong> the earth's surface.<br />

Carbon dioxide differs from volcanic dust also in the fact<br />

that because it is a gas it will not settle out <strong>of</strong> the atmosphere.

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