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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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THE MOUNTAINS 111<br />

PART II. Volcanism and Other Questions<br />

In the preceding part <strong>of</strong> this chapter we have sketched the<br />

principal problems that are basic to the formation <strong>of</strong> the<br />

folded mountains and block mountains, and have examined<br />

the planetary fracture systems in the light <strong>of</strong> Campbell's<br />

mechanism for crust displacement. <strong>The</strong>re are, however, a<br />

number <strong>of</strong> other aspects <strong>of</strong> this general problem that must<br />

now engage our attention. We must consider, in turn, the<br />

remarkable phenomena <strong>of</strong> volcanism, in their relationship to<br />

crust displacement. In connection with the creation <strong>of</strong> vol-<br />

canic mountains we must consider briefly the question <strong>of</strong> the<br />

origin <strong>of</strong> the heat <strong>of</strong> the earth, an unsolved problem <strong>of</strong> great<br />

interest. We must then examine the relationship <strong>of</strong> crust<br />

displacement and mountain building to the question <strong>of</strong><br />

changes in the sea level. Finally, we must consider the problem<br />

<strong>of</strong> the chronology <strong>of</strong> mountain building.<br />

6. Volcanism<br />

We have seen that one kind <strong>of</strong> mountain is the volcanic<br />

mountain. Volcanic phenomena cover a wide range; all <strong>of</strong><br />

these must be considered in order to see how far they can be<br />

related to a general cause. <strong>The</strong> phenomena that need ex-<br />

plaining include volcanic eruptions, the creation (sometimes<br />

rapid) <strong>of</strong> volcanic mountains on land or in the sea, the genesis<br />

<strong>of</strong> volcanic island arcs, and last but not least the vast lava<br />

flows or lava floods that have at times in the past inundated<br />

great areas <strong>of</strong> the earth's surface.<br />

Since volcanoes occur frequently, and are the most<br />

dramatic manifestations <strong>of</strong> volcanism, they<br />

have been thor-<br />

oughly studied, and a whole literature has been devoted to<br />

them. It is astonishing, therefore, that neither the causes <strong>of</strong><br />

volcanoes nor the present distribution <strong>of</strong> volcanic zones on

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