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The Earth's Shifting Crust by Charles Hapgood - wire of information

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428<br />

displacements <strong>of</strong> crust (Cont.)<br />

57, 176, 200, 203ff, 207ff,<br />

EARTH'S SHIFTING CRUST<br />

219, 237, 24gff, 287, 314, 390,<br />

and Chs. IX, XI, XII passim;<br />

approximate equality<br />

<strong>of</strong> extent,<br />

86; basic assumptions <strong>of</strong> hypothesis,<br />

377, 387!!; cause local in-<br />

creases in crust strength, 176;<br />

discontinuous, 351-52; economic<br />

consequences <strong>of</strong> theory, 38<strong>of</strong>f;<br />

effects, 95-96, Figs. II, V, VI,<br />

Ch. XII; evidence for, passim;<br />

topics cited in evidence, 387;<br />

evolution and, 322ff, Ch. X pas-<br />

sim; explain acceleration <strong>of</strong> geological<br />

processes, 49, 309; and<br />

block mountains, no; and<br />

changes in sea level, 120-26, 196,<br />

311-12; and "Climatic Optimum/'<br />

209-10; and climatic<br />

variation, 40, 65, 70, 78, 285,<br />

310, 312; and changes in oxygen<br />

content <strong>of</strong> atmosphere, 208; and<br />

conflict between Antevs and de<br />

Geer findings, 213; and differ-<br />

ences in extent <strong>of</strong> European vs.<br />

American glaciations, 213-15;<br />

and difficulties in isostasy the-<br />

ory, 178-79; and distribution <strong>of</strong><br />

species, 329, 339; and emptying<br />

<strong>of</strong> ecological niches, 33 iff; and<br />

epeirogenic uplifts, 121; and<br />

extinctions, 251-56, 332, 334,<br />

336ff, 339; and fracture patterns,<br />

91-110; and gaps in fossil rec-<br />

ord, 338-39; and geographical<br />

isolation <strong>of</strong> species, 32224, 339;<br />

and geosynclines, 90; and growth<br />

<strong>of</strong> continents, 122, i53ff; and<br />

heat <strong>of</strong> earth, 116-19; and in-<br />

constancy <strong>of</strong> climatic zones, 70,<br />

303; and inconstancy <strong>of</strong> icecap<br />

locations, i7iff, 287; and "interstadials,"<br />

209-10; and land<br />

bridges, i38ff; and lateral compression<br />

<strong>of</strong> sedimentary rock in<br />

India, 176; and mountain<br />

ranges, i38ff; and rapid crustal<br />

warping, 216; and "sea mounts/'<br />

i47ff; and structure <strong>of</strong> crust,<br />

152-53; and tempo <strong>of</strong> evolution,<br />

322ff, 339; and various<br />

anomalies, 175-76; and Virenz,<br />

332ff, 339; and volcanism, 43,<br />

111-15, 196, 204-8, 269; and<br />

world-wide lowering <strong>of</strong> temperature,<br />

43; future, <strong>of</strong> Antarctic<br />

icecap, 380-86; impending ac-<br />

tivity, evidence for, 382!!; intervals<br />

between beginnings <strong>of</strong>,<br />

about 40,000 years, 277, 284,<br />

38<strong>of</strong>f; intervals variable, 380;<br />

isostasy and, i59ff, 365-78; in<br />

North America, see Wisconsin<br />

glaciation and Ch. VII passim;<br />

northward in Siberia, 271 and<br />

Ch. VIII passim; Pennsylvanian<br />

cycles and, 313; periodicity, 85-<br />

86; perpetual, 304, 314; physical<br />

mechanism, Campbell hypoth-<br />

esis, 388, Ch. XI passim; objec-<br />

tions to this explanation, 22;<br />

answered, i97ff, 352-78; possibly<br />

responsible for all fundamental<br />

features <strong>of</strong> crust and<br />

earth's history, 314; prior to<br />

Wisconsin glaciation, Ch. IX<br />

passim; proposed causes, 15, 32,<br />

70; icecap as one <strong>of</strong> these, 17-<br />

21 and Ch. XI passim; rearward<br />

buildup <strong>of</strong> ice prolonging ac-<br />

tivity, 353-54, 3 8 5~ 86 ; su s-<br />

pended if both poles are in<br />

oceans, 354ff; this objection an-<br />

swered, 354-55; throughout<br />

Paleozoic, 313; time element, 97,<br />

128-31, 277, 284, 38<strong>of</strong>f; viscosity<br />

<strong>of</strong> asthenosphere no great ob-<br />

stacle to, ig<strong>of</strong>f. See also anomaly,

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