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

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Copyright 1958 by Charles H. Hapgood Published by Pantheon Books Inc. 333 Sixth Avenue, New York 14, N. Y. Published simultaneously in Canada by McClelland & Stewart, Ltd., Toronto, Canada Library of Congress Catalog Card No. 58-5504 Manufactured in the U.S.A.
to FRED, WILLIE, PRU, and MARY G.
Page 1 and 2: PAGES MISSING WITHIN THE BOOK ONLY
Page 7: Earth's Shifting Crust A Key to Som
Page 11 and 12: the Earth, 116; 9. Changing Sea Lev
Page 13 and 14: LIST OF ILLUSTRATIONS Fig. I. The C
Page 15 and 16: FOREWORD by Albert Einstein I frequ
Page 17 and 18: AUTHOR'S NOTE: To the Layman and th
Page 19 and 20: ACKNOWLEDGMENTS When it comes time
Page 21 and 22: ACKNOWLEDGMENTS 7 correspondence, a
Page 23 and 24: ACKNOWLEDGMENTS 9 lord Simpson, Maj
Page 25 and 26: INTRODUCTION 11 cists. The new idea
Page 27 and 28: INTRODUCTION 1$ the earth. They hav
Page 29 and 30: INTRODUCTION 15 time, a point near
Page 31 and 32: INTRODUCTION 1? eccentricity would,
Page 33 and 34: INTRODUCTION 19 first step must be
Page 35 and 36: INTRODUCTION 21 of displacement, to
Page 37 and 38: TABLE I The Geological Periods INTR
Page 39 and 40: PAST THEORIES OF POLAR SHIFT 25 pos
Page 41 and 42: PAST THEORIES OF POLAR SHIFT 2? lon
Page 43 and 44: PAST THEORIES OF FOLAR SHIFT 2Q gra
Page 45 and 46: PAST THEORIES OF BOLAR SHIFT gl of
Page 47 and 48: PAST THEORIES OF POLAR SHIFT gj the
Page 49 and 50: THEICEAGES 35 yet no theory is gene
Page 51 and 52: THEICEAGES 37 extended 1100 miles t
Page 53 and 54: THEICEAGES 39 conflict with basic p
Page 55 and 56: THE ICE AGES 41 or third region; bu
Page 57 and 58: THE ICE AGES 43 canic dust and carb
Page 59 and 60:
THEICEAGES 45 years. To a geologist
Page 61 and 62:
THEICEAGES 47 revelation that the l
Page 63 and 64:
THEICEAGES 49 Recent geological lit
Page 65 and 66:
THE ICE AGES 51 The period 133,000-
Page 67 and 68:
THEICEAGES 53 bottom of the Ross Se
Page 69 and 70:
THE ICE AGES 55 tween 6,000 and 4,0
Page 71 and 72:
THE ICE AGES 57 e. It must solve th
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ANCIENT CLIMATES 59 can, however, b
Page 75 and 76:
ANCIENT CLIMATES 6l directions of o
Page 77 and 78:
ANCIENT CLIMATES 6j region: ' 'Larg
Page 79 and 80:
Wallace describes the flora of the
Page 81 and 82:
ANCIENT CLIMATES 67 in earlier ages
Page 83 and 84:
ANCIENT CLIMATES 69 nian to the Eoc
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ANCIENT CLIMATES 71 Pauly cites ano
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ANCIENT CLIMATES 73 zones at the pr
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ANCIENT CLIMATES 75 tive tool with
Page 91 and 92:
ANCIENT CLIMATES 77 Very possibly M
Page 93 and 94:
IV : THE MOUNTAINS PART I. The Fold
Page 95 and 96:
THE MOUNTAINS 8l Sierra Nevada Moun
Page 97 and 98:
THE MOUNTAINS 8j the earth. The dou
Page 99 and 100:
THE MOUNTAINS 87 ing. Joly attempte
Page 101 and 102:
THE MOUNTAINS 91 ments and possibly
Page 103 and 104:
THE MOUNTAINS 93 termine the precis
Page 105 and 106:
THE MOUNTAINS 95 NORTH POLE POSITIO
Page 107 and 108:
THEMOUNTAINS 97 see, fractures in a
Page 109 and 110:
THEMOUNTAINS 99 would rise in the c
Page 111 and 112:
THE MOUNTAINS 1O1 The amount of the
Page 113 and 114:
THE MOUNTAINS There is still one de
Page 115 and 116:
THE MOUNTAINS 105 The recognition w
Page 117 and 118:
THE MOUNTAINS 107 displacement, and
Page 119 and 120:
THE MOUNTAINS Europe was nowhere ne
Page 121 and 122:
THE MOUNTAINS 111 PART II. Volcanis
Page 123 and 124:
THE MOUNTAINS 11$ all the way from
Page 125 and 126:
THE MOUNTAINS 117 of the earth. Sma
Page 127 and 128:
THE MOUNTAINS to its present latitu
Page 129 and 130:
ward by a shift of the whole crust,
Page 131 and 132:
THE MOUNTAINS 12$ crust, and these
Page 133 and 134:
THE MOUNTAINS 125 It follows that w
Page 135 and 136:
In another place he says: THE MOUNT
Page 137 and 138:
THE MOUNTAINS 12Q plete. It has bee
Page 139 and 140:
THE MOUNTAINS 1J1 much more continu
Page 141 and 142:
CONTINENTS AND OCEAN BASINS 1J3 avo
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CONTINENTS AND OCEAN BASINS 135 ref
Page 145 and 146:
CONTINENTS AND OCEAN BASINS 137 dee
Page 147 and 148:
CONTINENTS AND OCEAN BASINS 13 feel
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CONTINENTS AND OCEAN BASINS 141 It
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CONTINENTS AND OCEAN BASINS 143 and
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CONTINENTS AND OCEAN BASINS 145 one
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CONTINENTS AND OCEAN BASINS 147 reg
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CONTINENTS AND OCEAN BASINS 149 the
Page 159 and 160:
CONTINENTS AND OCEAN BASINS 15! com
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CONTINENTS AND OCEAN BASINS 153 cha
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CONTINENTS AND OCEAN BASINS 155 Fig
Page 165 and 166:
CONTINENTS AND OCEAN BASINS 157 It
Page 167 and 168:
THE SHAPE OF THE EARTH 159 ance and
Page 169 and 170:
THE SHAPE OF THE EARTH l6l to yield
Page 171 and 172:
THE SHAPE OF THE EARTH 163 ment wit
Page 173 and 174:
THE SHAPE OF THE EARTH 165 ing gene
Page 175 and 176:
THE SHAPE OF THE EARTH 167 of water
Page 177 and 178:
THE SHAPE OF THE EARTH 169 as winte
Page 179 and 180:
THE SHAPE OF THE EARTH 171 the flow
Page 181 and 182:
THE SHAPE OF THE EARTH 173 the crus
Page 183 and 184:
THE SHAPE OF THE EARTH 175 lithosph
Page 185 and 186:
THE SHAPE OF THE EARTH 177 gravitat
Page 187 and 188:
THE SHAPE OF THE EARTH 179 distorti
Page 189 and 190:
THE SHAPE OF THE EARTH l8l is a dev
Page 191 and 192:
THE SHAPE OF THE EARTH 183 supposes
Page 193 and 194:
THE SHAPE OF THE EARTH 185 justment
Page 195 and 196:
THE SHAPE OF THE EARTH 187 siderabl
Page 197 and 198:
: his : rock It is not easy to reco
Page 199 and 200:
THE SHAPE OF THE EARTH 1Q1 I have n
Page 201 and 202:
VII : NORTH AMERICA AT THE POLE In
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NORTH AMERICA AT THE POLE he could
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NORTH AMERICA AT THE POLE 1Q7 An ei
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NORTH AMERICA AT THE POLE than is t
Page 209 and 210:
NORTH AMERICA AT THE POLE 2O1 gin o
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NORTH AMERICA AT THE POLE 2OJ Assum
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NORTH AMERICA AT THE POLE 205 A spe
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NORTH AMERICA AT THE POLE ago (242:
Page 217 and 218:
NORTH AMERICA AT THE POLE 2OQ think
Page 219 and 220:
NORTH AMERICA AT THE POLE 211 facts
Page 221 and 222:
NORTH AMERICA AT THE POLE radiocarb
Page 223 and 224:
NORTH AMERICA AT THE POLE 215 that
Page 225 and 226:
NORTH AMERICA AT THE POLE 217 rebou
Page 227 and 228:
NORTH AMERICA AT THE POLE the meeti
Page 229 and 230:
NORTH AMERICA AT THE POLE 221 varia
Page 231 and 232:
NORTH AMERICA AT THE POLE 22J from
Page 233 and 234:
NORTH AMERICA AT THE POLE 225 by th
Page 235 and 236:
VIII : THE GREAT EXTINCTIONS When t
Page 237 and 238:
THE GREAT EXTINCTIONS 229 2. The Ma
Page 239 and 240:
THE GREAT EXTINCTIONS 231 tions fro
Page 241 and 242:
THE GREAT EXTINCTIONS favorable cir
Page 243 and 244:
THE GREAT EXTINCTIONS standing. The
Page 245 and 246:
THE GREAT EXTINCTIONS 237 it is not
Page 247 and 248:
THE GREAT EXTINCTIONS 239 perfect c
Page 249 and 250:
THE GREAT EXTINCTIONS 241 Siberian
Page 251 and 252:
THE GREAT EXTINCTIONS 24$ "Lovelock
Page 253 and 254:
THE GREAT EXTINCTIONS 245 tinguishe
Page 255 and 256:
THE GREAT EXTINCTIONS 247 trict. .
Page 257 and 258:
THE GREAT EXTINCTIONS 24Q mainly on
Page 259 and 260:
THE GREAT EXTINCTIONS 251 we would
Page 261 and 262:
THE GREAT EXTINCTIONS 253 enough du
Page 263 and 264:
THE GREAT EXTINCTIONS 255 following
Page 265 and 266:
THE GREAT EXTINCTIONS 257 this isn'
Page 267 and 268:
THE GREAT EXTINCTIONS 259 imbedded
Page 269 and 270:
THE GREAT EXTINCTIONS g6l limestone
Page 271 and 272:
THE GREAT EXTINCTIONS 263 greater o
Page 273 and 274:
THE GREAT EXTINCTIONS 265 tected co
Page 275 and 276:
THE GREAT EXTINCTIONS 267 in which
Page 277 and 278:
THE GREAT EXTINCTIONS 269 be preser
Page 279 and 280:
THE GREAT EXTINCTIONS 271 are today
Page 281 and 282:
EARLIER DISPLACEMENTS OF CRUST 273
Page 283 and 284:
Page 285 and 286:
Page 287 and 288:
Page 289 and 290:
Page 291 and 292:
Page 293 and 294:
Page 295 and 296:
Page 297 and 298:
Page 299 and 300:
SAND > POLLEN PERCENTAGE 10 20 30 4
Page 301 and 302:
EARLIER DISPLACEMENTS OF CRUST 2Q3
Page 303 and 304:
EARLIER DISPLACEMENTS OF CRUST P-12
Page 305 and 306:
EARLIER DISPLACEMENTS OF CRUST 2Q7
Page 307 and 308:
EARLIER DISPLACEMENTS OF CRUST teri
Page 309 and 310:
EARLIER DISPLACEMENTS OF CRUST 40 5
Page 311 and 312:
EARLIER DISPLACEMENTS OF CRUST It a
Page 313 and 314:
Page 315 and 316:
Page 317 and 318:
Page 319 and 320:
EARLIER DISPLACEMENTS OF CRUST Jll
Page 321 and 322:
EARLIER DISPLACEMENTS OF CRUST the
Page 323 and 324:
X : LIFE In the preceding chapters
Page 325 and 326:
LIFE 317 an entirely accidental pro
Page 327 and 328:
LIFE totally inconceivable unless i
Page 329 and 330:
LIFE 321 to find the conditions the
Page 331 and 332:
LIFE 323 to mean increased competit
Page 333 and 334:
LIFE .325 lifted, the sea will with
Page 335 and 336:
LIFE 327 continent of Asia, but als
Page 337 and 338:
LIFE 329 reconsider it in terms of
Page 339 and 340:
LIFE 331 could utilize it, but afte
Page 341 and 342:
LIFE 333 species can be compared wi
Page 343 and 344:
LIFE 335 the pre-Cambrian, and ther
Page 345 and 346:
LIFE 337 If a species becomes extin
Page 347 and 348:
LIFE 339 of crust displacement is q
Page 349 and 350:
CAMPBELL'S MECHANISM 341 will overc
Page 351 and 352:
CAMPBELL'S MECHANISM 343 examine wi
Page 353 and 354:
CAMPBELL'S MECHANISM 345 crust alon
Page 355 and 356:
CAMPBELL S MECHANISM 347 NORTH POLE
Page 357 and 358:
CAMPBELL'S MECHANISM 349 wedge, whi
Page 359 and 360:
CAMPBELLS MECHANISM 351 place to pl
Page 361 and 362:
CAMPBELL'S MECHANISM 353 ment sugge
Page 363 and 364:
CAMPBELL'S MECHANISM 355 near the e
Page 365 and 366:
CAMPBELL'S MECHANISM 357 more impro
Page 367 and 368:
CAMPBELL'S MECHANISM 359 itself, bu
Page 369 and 370:
CAMPBELL'S MECHANISM 361 being push
Page 371 and 372:
CAMPBELL'S MECHANISM 363 the earth,
Page 373 and 374:
CAMPBELL'S MECHANISM 365 considerab
Page 375 and 376:
CAMPBELL'S MECHANISM 367 tributes t
Page 377 and 378:
CAMPBELL'S MECHANISM 369 hoping tha
Page 379 and 380:
CAMPBELL'S MECHANISM 371 feet will
Page 381 and 382:
CAMPBELL'S MECHANISM 373 surface. A
Page 383 and 384:
CAMPBELL'S MECHANISM 375 as a resul
Page 385 and 386:
CAMPBELL'S MECHANISM 377 termined b
Page 387 and 388:
XII : CONCLUSION i. Looking Forward
Page 389 and 390:
CONCLUSION 381 sized by Brown, that
Page 391 and 392:
CONCLUSION 383 the progressive weak
Page 393 and 394:
CONCLUSION 385 while to mention Ewi
Page 395 and 396:
CONCLUSION 387 present time are dis
Page 397 and 398:
CONCLUSION 389 Frazer, author of th
Page 399 and 400:
Dear Mr. Hapgood, APPENDIX Princeto
Page 401 and 402:
GLOSSARY ANOMALY, Positive: An exce
Page 403 and 404:
GLOSSARY 395 suit from the adaptati
Page 405 and 406:
BIBLIOGRAPHY 397 17. Bailey, Thomas
Page 407 and 408:
BIBLIOGRAPHY 399 58. Bucher, Walter
Page 409 and 410:
BIBLIOGRAPHY 4O1 98. Daly, R. A., O
Page 411 and 412:
136. Emiliani, Cesare, personal com
Page 413 and 414:
BIBLIOGRAPHY 405 sonian Institution
Page 415 and 416:
BIBLIOGRAPHY 407 *io. Hess, H. H.,
Page 417 and 418:
BIBLIOGRAPHY 409 of the American As
Page 419 and 420:
BIBLIOGRAPHY 411 The Shifting in Po
Page 421 and 422:
BIBLIOGRAPHY 413 3i6a. Nddai, Arpad
Page 423 and 424:
BIBLIOGRAPHY 415 354. Reid, Harry F
Page 425 and 426:
BIBLIOGRAPHY 417 404. Stetson, H. C
Page 427 and 428:
BIBLIOGRAPHY 419 438. Urey, Harold
Page 429 and 430:
INDEX OF NAMES Abrons, Stanley Howa
Page 431 and 432:
Hubbert, M. King, 160 Humphreys, W.
Page 433 and 434:
INDEX OF SUBJECTS Academy of Scienc
Page 435 and 436:
continents, ancient (Brooks the- or
Page 437 and 438:
Antarctica, asthenosphere, burst- i
Page 439 and 440:
Greenland, amphibians INDEX OF SUBJ
Page 441 and 442:
measurements of in Greenland, 381;
Page 443 and 444:
ocean basins, origin unexplained, 1
Page 445 and 446:
selection pressure, mild, 318; stro
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