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PAGES MISSING WITHIN THE BOOK ONLY
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Earth's Shifting Crust A Key to Som
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to FRED, WILLIE, PRU, and MARY G.
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the Earth, 116; 9. Changing Sea Lev
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LIST OF ILLUSTRATIONS Fig. I. The C
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FOREWORD by Albert Einstein I frequ
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AUTHOR'S NOTE: To the Layman and th
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ACKNOWLEDGMENTS When it comes time
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ACKNOWLEDGMENTS 7 correspondence, a
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ACKNOWLEDGMENTS 9 lord Simpson, Maj
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INTRODUCTION 11 cists. The new idea
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INTRODUCTION 1$ the earth. They hav
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INTRODUCTION 15 time, a point near
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INTRODUCTION 1? eccentricity would,
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INTRODUCTION 19 first step must be
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INTRODUCTION 21 of displacement, to
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TABLE I The Geological Periods INTR
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PAST THEORIES OF POLAR SHIFT 25 pos
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PAST THEORIES OF POLAR SHIFT 2? lon
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PAST THEORIES OF FOLAR SHIFT 2Q gra
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PAST THEORIES OF BOLAR SHIFT gl of
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PAST THEORIES OF POLAR SHIFT gj the
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THEICEAGES 35 yet no theory is gene
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THEICEAGES 37 extended 1100 miles t
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THEICEAGES 39 conflict with basic p
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THE ICE AGES 41 or third region; bu
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THE ICE AGES 43 canic dust and carb
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THEICEAGES 45 years. To a geologist
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THEICEAGES 47 revelation that the l
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THEICEAGES 49 Recent geological lit
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THE ICE AGES 51 The period 133,000-
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THEICEAGES 53 bottom of the Ross Se
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THE ICE AGES 55 tween 6,000 and 4,0
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THE ICE AGES 57 e. It must solve th
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ANCIENT CLIMATES 59 can, however, b
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ANCIENT CLIMATES 6l directions of o
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ANCIENT CLIMATES 6j region: ' 'Larg
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Wallace describes the flora of the
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ANCIENT CLIMATES 67 in earlier ages
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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
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ANCIENT CLIMATES 77 Very possibly M
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IV : THE MOUNTAINS PART I. The Fold
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THE MOUNTAINS 8l Sierra Nevada Moun
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THE MOUNTAINS 8j the earth. The dou
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THE MOUNTAINS 87 ing. Joly attempte
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THE MOUNTAINS 91 ments and possibly
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THE MOUNTAINS 93 termine the precis
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THE MOUNTAINS 95 NORTH POLE POSITIO
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THEMOUNTAINS 97 see, fractures in a
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THEMOUNTAINS 99 would rise in the c
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THE MOUNTAINS 1O1 The amount of the
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THE MOUNTAINS There is still one de
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THE MOUNTAINS 105 The recognition w
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THE MOUNTAINS 107 displacement, and
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THE MOUNTAINS Europe was nowhere ne
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THE MOUNTAINS 111 PART II. Volcanis
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THE MOUNTAINS 11$ all the way from
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THE MOUNTAINS 117 of the earth. Sma
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THE MOUNTAINS to its present latitu
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ward by a shift of the whole crust,
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THE MOUNTAINS 12$ crust, and these
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THE MOUNTAINS 125 It follows that w
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In another place he says: THE MOUNT
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THE MOUNTAINS 12Q plete. It has bee
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THE MOUNTAINS 1J1 much more continu
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CONTINENTS AND OCEAN BASINS 1J3 avo
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CONTINENTS AND OCEAN BASINS 135 ref
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CONTINENTS AND OCEAN BASINS 137 dee
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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
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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
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CONTINENTS AND OCEAN BASINS 157 It
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THE SHAPE OF THE EARTH 159 ance and
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THE SHAPE OF THE EARTH l6l to yield
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THE SHAPE OF THE EARTH 163 ment wit
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THE SHAPE OF THE EARTH 165 ing gene
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THE SHAPE OF THE EARTH 167 of water
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THE SHAPE OF THE EARTH 169 as winte
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THE SHAPE OF THE EARTH 171 the flow
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THE SHAPE OF THE EARTH 173 the crus
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THE SHAPE OF THE EARTH 175 lithosph
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THE SHAPE OF THE EARTH 177 gravitat
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THE SHAPE OF THE EARTH 179 distorti
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THE SHAPE OF THE EARTH l8l is a dev
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THE SHAPE OF THE EARTH 183 supposes
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THE SHAPE OF THE EARTH 185 justment
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THE SHAPE OF THE EARTH 187 siderabl
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: his : rock It is not easy to reco
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THE SHAPE OF THE EARTH 1Q1 I have n
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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
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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:
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NORTH AMERICA AT THE POLE 2OQ think
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NORTH AMERICA AT THE POLE 211 facts
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NORTH AMERICA AT THE POLE radiocarb
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NORTH AMERICA AT THE POLE 215 that
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NORTH AMERICA AT THE POLE 217 rebou
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NORTH AMERICA AT THE POLE the meeti
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NORTH AMERICA AT THE POLE 221 varia
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NORTH AMERICA AT THE POLE 22J from
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NORTH AMERICA AT THE POLE 225 by th
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VIII : THE GREAT EXTINCTIONS When t
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THE GREAT EXTINCTIONS 229 2. The Ma
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LIFE 333 species can be compared wi
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LIFE 335 the pre-Cambrian, and ther
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LIFE 337 If a species becomes extin
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LIFE 339 of crust displacement is q
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CAMPBELL'S MECHANISM 341 will overc
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CAMPBELL'S MECHANISM 343 examine wi
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CAMPBELL'S MECHANISM 345 crust alon
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CAMPBELL S MECHANISM 347 NORTH POLE
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CAMPBELL'S MECHANISM 349 wedge, whi
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CAMPBELLS MECHANISM 351 place to pl
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CAMPBELL'S MECHANISM 353 ment sugge
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CAMPBELL'S MECHANISM 355 near the e
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CAMPBELL'S MECHANISM 357 more impro
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CAMPBELL'S MECHANISM 359 itself, bu
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CAMPBELL'S MECHANISM 361 being push
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CAMPBELL'S MECHANISM 363 the earth,
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CAMPBELL'S MECHANISM 365 considerab
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CAMPBELL'S MECHANISM 367 tributes t
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CAMPBELL'S MECHANISM 369 hoping tha
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CAMPBELL'S MECHANISM 371 feet will
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CAMPBELL'S MECHANISM 373 surface. A
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CAMPBELL'S MECHANISM 375 as a resul
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CAMPBELL'S MECHANISM 377 termined b
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XII : CONCLUSION i. Looking Forward
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CONCLUSION 381 sized by Brown, that
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CONCLUSION 383 the progressive weak
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CONCLUSION 385 while to mention Ewi
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CONCLUSION 387 present time are dis
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CONCLUSION 389 Frazer, author of th
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Dear Mr. Hapgood, APPENDIX Princeto
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GLOSSARY ANOMALY, Positive: An exce
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GLOSSARY 395 suit from the adaptati
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BIBLIOGRAPHY 397 17. Bailey, Thomas
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BIBLIOGRAPHY 399 58. Bucher, Walter
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BIBLIOGRAPHY 4O1 98. Daly, R. A., O
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136. Emiliani, Cesare, personal com
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BIBLIOGRAPHY 405 sonian Institution
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BIBLIOGRAPHY 407 *io. Hess, H. H.,
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BIBLIOGRAPHY 409 of the American As
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BIBLIOGRAPHY 411 The Shifting in Po
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BIBLIOGRAPHY 413 3i6a. Nddai, Arpad
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BIBLIOGRAPHY 415 354. Reid, Harry F
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BIBLIOGRAPHY 417 404. Stetson, H. C
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BIBLIOGRAPHY 419 438. Urey, Harold
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INDEX OF NAMES Abrons, Stanley Howa
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Hubbert, M. King, 160 Humphreys, W.
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INDEX OF SUBJECTS Academy of Scienc
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continents, ancient (Brooks the- or
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Antarctica, asthenosphere, burst- i
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Greenland, amphibians INDEX OF SUBJ
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measurements of in Greenland, 381;
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ocean basins, origin unexplained, 1
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selection pressure, mild, 318; stro