| |
|
CONTINENTAL...............334 (0.042%)
|
| Thus, according to Q theory, C continental drift theory, | 992 QUANTAVOLUTION AND CATASTROPHE: PART 3: A Comment on the Q-C Test and Its Individual Items - - - |
| is slow now was once a continental cracking and rafting at considerable speed. | 995 QUANTAVOLUTION AND CATASTROPHE: PART 3: A Comment on the Q-C Test and Its Individual Items - - - |
| terrestrial object, or proposing that the continental crust of the earth has been creeping by tiny increments over most of the global surface over all of Earth's history. | 1153 QUANTAVOLUTION AND CATASTROPHE: PART 4: PROSPECTIVE CHANGES IN THE Q-C TEST - - - |
| constellation contamination continent continent, quantavolution of continental drift (rafting) continental margin continental plate continental shelf continental shield continental tropism, | 2303 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| continent, quantavolution of continental drift (rafting) continental margin continental plate continental shelf continental shield continental tropism, | 2304 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| of continental drift (rafting) continental margin continental plate continental shelf continental shield continental tropism, | 2305 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| drift (rafting) continental margin continental plate continental shelf continental shield continental tropism, | 2306 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| continental margin continental plate continental shelf continental shield continental tropism, | 2307 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| continental plate continental shelf continental shield continental tropism, | 2308 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| Dravidian Culture dream Dreamtime dress drift, continental drift, | 2590 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| done by Melvin Cook. V. rejected continental drift and his arguments against Darwinism were those well-elaborated by creationists and scientists of "saltationist" persuasion long before. | 11310 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| with them directly! Is this so? Continental shelves -- have they been filling and dropping ? | 11855 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| Ice Ages b) Natural Selection c) Continental Drift d) "In the Beginning," " | 12288 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| heretics, Deg accepted the theory of "continental drift" that triumphed in geology during the postwar generation. | 12326 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| Earth at the beginning of the continental movements, | 12328 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| with the gang of speculations about continental drift. | 12339 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| type of hard proof that the continental plates move under an Earth power that is sui generis and not originally extra-terrestrial, | 12360 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| support Dr. Velikovsky's view of continental drift, | 12363 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| As he says, "My position on continental drift was (and is ) intermediary between..." | 12365 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| come upon the best explanation of continental drift, | 12369 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| and had the basic components of continental rafting mechanisms in mind. | 12370 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| reality of these crises on a continental scale which I have tried to analyze. | 13823 COSMIC HERETICS: PART 4: - Chapter 12: THE THIRD WORLD OF SCIENCE - |
| 50 years from oceanography, and when continental drift theory was held in contempt by American geologists. | 19132 COSMIC HERETICS: PART 5: - Chapter 16: PRECURSORS OF QUANTAVOLUTION - |
| of the fact and age of continental drift by the bands of magnetic reversal found on the rocks of the ocean bottom, | 22467 CHAOS AND CREATION: - - CHAPTER 02: HIGH ENERGY FROM SPACE : THE BATTLE OVER TIME |
| heavily destructive tsunamis have struck the continental coasts during the present era (Solaria) and wonders at their great cumulative effect 26 . | 22478 CHAOS AND CREATION: - - CHAPTER 02: HIGH ENERGY FROM SPACE : THE BATTLE OVER TIME |
| oceans and carrying it up the continental shelves For the ocean bottoms are scarcely sedimented 4 . | 22743 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| an extreme catastrophist. For, allowing that continental land (or sial) covers only 40 of the globe and the sediments lay on the average only 4 miles thick upon the 20 mile thick sial, | 22756 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| shallow seas of Pangea, the wholly continental Earth-crust that we postulate in this book. | 22892 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : CORAL REEFS |
| quoting von Humboldt et al. 12. Continental drift theorists, | 24348 CHAOS AND CREATION: - - CHAPTER 04: A CATASTROPHIC CALENDAR : Notes (Chapter Four: A Catastrophic Calendar) |
| the term "Pangaea" to mean the continental crust, | 24349 CHAOS AND CREATION: - - CHAPTER 04: A CATASTROPHIC CALENDAR : Notes (Chapter Four: A Catastrophic Calendar) |
| the oceans have destroyed and buried continental material, | 24835 CHAOS AND CREATION: - - CHAPTER 05: SOLARIA BINARIA : THE WORLD OF PANGEA |
| a small fraction of the vast continental shelves and slopes. | 24844 CHAOS AND CREATION: - - CHAPTER 05: SOLARIA BINARIA : THE WORLD OF PANGEA |
| as half of the Earth's continental material exploded into the sky down to the same depth, | 26367 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE PASSAGE OF URANUS MINOR |
| the eruption of the Moon and continental drift 6 . | 26393 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| land that pushed into it. Conventional continental drift theory only lends confusion. | 26403 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| blows imposed upon the Earth's continental crust were reinforced by a worldwide deep friction as the Earth's rotation was interrupted and the globe was wrenched into a new axial position. | 26467 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| expanded. At a boundary between the continental sial and the upper mantle, | 26469 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| of molten Pacific basin, bereft of continental crust, | 26471 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| s volume, representing the mixture of continental sial and upper mantle magma that was wrenched from the Pacific basin during the encounter with "Uranus Minor". " | 26479 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| Wegener, the geophysicist who produced the continental drift theory in the 1920's touched briefly upon the missing sial of the Earth's structure, | 26503 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| outermost layer, re-presented by the continental blocks, | 26505 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| idea of Moon escaping, followed by continental rafting, | 26513 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| had not believed, erroneously, that the continental sial floats on the oceanic sima and could skate upon it. | 26514 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| this, that the sima approaches a continental block and dives beneath it. | 26517 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| globular gradiant introducing gravitational slide. The continental crust would flow down the lips of the concavity. | 26524 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| This map is merely suggestive. Submarine continental shelves are treated here as "land." | 26709 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| fractures, mountain ranges, volcanos, sea mounts, continental shelves, | 26712 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| The Arctic Sea stands mostly on continental shelves. | 26714 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| Area sizes are rough and include continental shelves. | 26731 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| The total ocean surface, less the continental shelves, | 26739 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| TOTAL 150 19 31 200 Destroyed continental sutfaces 200 New Ocean Basin Expansion 110 Total 510 Note on Table: | 26756 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| 110 Total 510 Note on Table: Continental Slopes are not considered continental, | 26760 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| Table: Continental Slopes are not considered continental, | 26760 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| subsequent to break-apart. However, where continental shelves are poorly defined, | 26761 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| where continental shelves are poorly defined, continental slope contributions to true Pangean land mass are estimated and included. | 26761 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| molten fingers stretched up toward the continental debris that was escaping into space and then dropped back as blisters upon the ocean basins. | 26806 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE TETHYAN WELT |
| the edges of the Northwest Atlantic continental slope penetrate "a succession of ash layers" before striking the basaltic lava of the true ocean bottom 52 . | 26813 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE TETHYAN WELT |
| at the edges of today's continental slopes. | 26968 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : OCEAN DEVELOPMENT |
| on, of the deluging of the continental shelves and slopes, | 27032 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : SUNKEN LANDS |
| map to the extreme North. All continental shelf lands were overwhelmed by water around 6, | 27085 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : SUNKEN LANDS |
| 9500 B. C.) and the Saturnian continental-shelf flooding of around 4000 B. | 27236 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE MOON IN MESO-AMERICA |
| du Toit's early defense of continental drift and ice cap depression as originating the Atlantic rupture, | 27637 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : Notes (Chapter Seven: Earth Parturition and Moon Birth) |
| Saturn", great stretches of now sunken continental land were still above the sea, | 27934 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN - |
| surface of the Earth included the continental shelves and slopes, | 28054 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN : THE "GOLDEN AGE" |
| enclosing all of the European northwestern continental platform from the Bay of Biscay to Scandinavia on the north, | 28120 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN : THE PEOPLES OF SATURNIA |
| the sweat of their brows." Numerous continental area, | 28239 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN : THE DOWNFALL OF SATURN : NOVA AND DELUGE |
| population which was living on the continental margins. | 28248 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN : THE DOWNFALL OF SATURN : NOVA AND DELUGE |
| For these suddenly became the vast continental slopes and shelves of the oceans. | 28248 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN : THE DOWNFALL OF SATURN : NOVA AND DELUGE |
| of a problem explaining away the continental-type rock found in several places in the Pacific Basin where the Moon would have erupted from. | 30543 CHAOS AND CREATION: - - CHAPTER 11: THE DEVIL'S ADVOCATE - |
| W. (1958), The Tectonic Approach to Continental Drift, | 31320 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| Approach to Continental Drift, Symposium on Continental Drift, | 31320 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| 1963), "Evidence for Recent Rupture of Continental Crust," | 31364 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| Letters, Part I, 74-77. ---- (1964), "Continental Drift: | 31367 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| Ionization," Pergamon, London. Kelly, Allen (1963), Continental Drift: | 31815 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| 8. ---- (1973), "Do the Pyramids Show Continental Drift?" | 32128 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| Cleavages 23.Canyons and Channels 24.Continental Tropism and Rafting 25. | 32675 THE LATELY TORTURED EARTH: - - - TABLE OF CONTENTS - |
| of the land we speak of continental drift or rafting, | 32951 THE LATELY TORTURED EARTH: - - CHAPTER 1: Quantavolutions - |
| a movement of its crustal shell (continental displacement). | 33556 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 2 The Gaseous Complex - |
| are the exponents and developers of continental drift. | 34423 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| author that what convinced him of continental drift was paleomagnetic measurements. | 34424 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| between the two rising elements of continental rock.) | 34466 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| crust, cleaved the globe, set the continental fragments into motion, | 34472 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| true north as an increment of continental drift and other seismic movement of the area. | 34563 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| rules of appraisal. Granites are the continental structure: | 35916 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| ash layers are now recognized in continental areas throughout the geological record," | 36018 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| encountered on the edge of the continental slope before striking the lava basalt of the true ocean bottom. | 36080 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| Might this not indicate that the continental slope was laid down subaerially, | 36081 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| the mass of all of the continental crust except for the basic granite within a few thousand years. | 36793 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| also 5.5 times that in continental igneous rock; | 36810 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| depositional and chemical environments ranging from continental and coastal soils to marsh and subtidal marine deposits, | 37517 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 9 Gases, Poisons and Foods - |
| with the flood and eventually triggered continental drift, ( | 38215 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| and eventually triggered continental drift, (2) continental drift itself, | 38216 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| thrusts contributed largely in the pre-continental drift stage, | 38220 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| welting and overthrusting in the pre-continental drift stage being strong in this region, | 38224 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| front of the thrust blocks during continental drift itself and the tremendous upheavals strongest here in the final readjustment stage. | 38226 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| and applies weathering rates for the continental masses from wind, | 38564 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| into America in the course of continental drift and, | 38637 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| of Appalachia and the North American continental shelves by instant burning in passage, | 38670 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| broad guidelines. 'Weathering rates estimated for continental masses and great mountains are about 80 meters per million years, | 38767 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| being scraped and relaid by the continental plates at least over the past two hundred million years or less; | 39133 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| of the oceans as conceivably of continental origins. | 39147 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| Granite, the rock that underlies the continental sediments, | 39181 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| not properly abyssal but belonging to continental sial was flooded up to present shorelines. | 39287 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| and by promoting off- flow of continental water supplies -but also a more grave problem, | 39300 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| hitherto unsuspected natural trend of the continental crust to lose its water holdings, | 39301 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| occurs beneath much of the Atlantic continental self." | 39356 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| Fresh waters were trapped in the continental rocks as they made way toward the abyss and are probably trapped in the debris of the continental slope as well. | 39368 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| trapped in the debris of the continental slope as well. | 39369 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| sunk in the flooding of the continental shelves by the Noachian Deluge. | 39545 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 13 Deluges - |
| origin of the oceanic waters. The continental slopes and shelves were permanently inundated at some point in time, | 39977 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| new water needed to cover the continental slopes and shelves. | 39993 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| drop in the form of snow. Continental drift has been argued as the cause of ice ages: " | 40787 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| earth cleaved, lost most of its continental crust, | 40870 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| ice cap would have shoved the continental crust on a wedge principle to be mechanically acceptable 13 .) | 41000 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| overhanging rock or crust of the continental and oceanic bottoms? | 41260 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| currents in a later chapter on continental drift. | 41279 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| the volcanos of yesteryear?" If the continental and oceanic plates break up and drift apart, | 41887 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| preceded Wegener with the idea of continental drift.) | 41924 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| was Pangea, a globe covered by continental crust that carried shallow freshwater seas, | 42142 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| falling and flooding waters. Where the continental fragments do not remain to be fitted obviously together, | 42153 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| land was blasted away or sunk. Continental sial has been extracted on occasion from the deep bottoms in the Atlantic and Pacific Ocean; | 42154 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| reconstruction of the area prior to continental movements, | 42191 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| of the best contemporary oceanographers, found continental land far beneath the Tyrrhenian waves, | 42268 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| globe. With the new theory of continental drift and splitting of the Old World from the New by the Atlantic Ocean, | 42283 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| waters and a great amount of continental crust is missing. | 42367 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| this idea with the notion of continental drift, | 42437 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| notion of continental drift, and hence continental drift in recent times, | 42437 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| this: the debris of the Pangean continental breakup is scattered around the Pacific as its fundamental morphology; | 42665 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| rock, such as rhyolite, are of continental origin and found on Easter Island. | 42686 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| Western south America had once been continental sial. | 42688 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| kilometers thick; this is characteristic of continental crust, | 42690 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| is possible that the area is continental sial, | 42693 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| of human manufacture, as well as continental species of flora and fauna. | 42707 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| Warren Carey, The Tectonic Approach to Continental Drift (U. | 42902 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands : Notes (Chapter Eighteen: Sinking and Rising Lands) |
| as a mechanism to account for continental drift. | 43043 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| million years cannot be explained by continental drift on the surface of the present- sized earth." | 43075 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| the supposed original supercontinent before its continental elements drifted apart, | 43077 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| drifted apart, he retrojects the present continental map as it must have drifted and shows that the present arrangement could not have emerged from the reconstruction. | 43078 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| produce a concurrent breakup of the continental mass and an expansion of the globe. | 43097 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| accumulate is critical, whether on the continental surfaces, | 43217 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| attributed. That is the tendency of continental margins to stretch out over the ocean basins. | 43232 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| exploring the seismic structure of the continental margin off France, | 43237 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| that the upper part of the continental crust of margins has been fractured into a remarkable pattern of narrow sedimentary basins bounded by listric faults, | 43239 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| with depth. He suggested that the continental crust at the margin was extended at the time of rifting by up to 20 per cent." | 43242 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| be broken off serially from the continental mass. | 43249 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| 32-7. 5. "Topological Inconsistency of Continental Drift on the Present Size Earth," | 43283 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction : Notes (Chapter Nineteen: Expansion and Contraction) |
| originate which can raise and lower continental masses vertically? ... | 43350 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| the apparently interconnected Pacific Basin and continental movements I find a need for a more universal force. | 43380 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| pushed from behind by the moving continental mass. | 43396 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| swelling magma. Unlike the motorboat, the continental blocks as a whole would not then sink; | 43406 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| occurs rapidly as the cut-apart continental blocks scramble for position. | 43419 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| the vast inertial forces initiated in continental rafting. | 43478 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| to his mechanism would be rapid continental movement toward the south, | 43496 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| of it, unless, as we said, continental drifting is called thrusting. | 43545 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| a supposed situation in which the continental crust folds and thrusts and compresses into abundant mountains while the oceanic crust slides up and under and around without making mountains, | 43556 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| igneous ridges and seamounts. That no continental mountains are to be found imbedded in oceanic basalts is remarkable. | 43559 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| overthrusting has been several thousand miles (continental drift), | 43658 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| dumps by turbulent currents, and the continental slopes are the largest of fans. | 43709 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| channels; and the sediments, including the continental slopes. | 43718 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| 4 (Summer 1982), 8-25. 7. "Continental Drift," | 43784 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny : Notes (Chapter Twenty: Thrusting And Orogeny) |
| 5 percent of the surface into 'continental masses' and left only 15 to 20 percent of it as basins... " | 43824 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| basins, that is, distinct from the continental material as they are on Earth. | 43826 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| same time by the migration of continental land driven to the scene of the disaster. | 43834 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| of the Arctic Ocean floor is continental shelf, | 43932 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| seamounts. The three ridges enter the continental shelf of northeast Siberia. | 43937 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the Nansen Cordillera moves into the continental shelf in a great "Sadko Trough" and, | 43939 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| Throughout the Arctic ocean bed the continental mass rises abruptly above the abyssal plains. | 43943 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| The Arctic Hemisphere, indicating the largely continental (rather than basaltic ocean-type) bottom; | 43964 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| Ninety Degrees Ridge, and the largely continental rock platforms that underlie the vast Asia-Australia area. | 43972 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| main fractures occurred before the main continental shift, ( | 43986 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| shelves that then plunge down. The continental slopes, | 44052 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| hand, are water-covered moraines of continental debris laying on top of ocean abyssal basalt. | 44053 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| making nearly a right angle where continental block meets ocean floor; | 44054 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| More likely exponentially declining rates of continental debris and seabottom spread worked together to provide the profile. | 44059 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| told in the previous chapter, the continental slopes are free of continental mountains, | 44066 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the continental slopes are free of continental mountains, | 44066 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| why have none appeared on the continental slopes? | 44069 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| and poured off the miles-steep continental blocks into the ocean. | 44074 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| their waters crept up upon the continental blocks and shelves. | 44077 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| thin. They are denser than the continental sial. | 44099 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| have expanded and intruded upon the continental granites. | 44101 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| basic or less acid than the continental crust indicates that it separated from the primeval melt after the granitic crust; | 44108 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| floor does not cover a former continental surface, | 44114 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| case. Nevertheless the floor probably contains continental debris in small amounts. | 44116 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| expect ocean-bottom drills to collect continental material here and there. | 44117 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| most sinkings have occurred on the continental slopes or shelves. | 44119 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the basins proper but on the continental shelves and slopes. | 44128 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| dropped back to form islands of continental crust in mid-ocean. | 44135 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| varies. It differs markedly from much continental sediment that is rock. | 44138 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the ridges rise higher than the continental Alps. | 44156 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| out in the last chapter. The continental mountains were shaped by horizontal forces, | 44158 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the Earth, with similar assistance; unlike continental mountains, | 44160 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| uniformitarian forces produce this contrast? The continental crust folds and thrusts and compresses into abundant mountains; | 44164 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| have the extensive piping systems of continental volcanos. | 44215 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| New Zealand and a few other continental areas are remnants of them. | 44434 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| at the full depth of the continental crust, | 44451 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| western Tethyan fracture cut through the continental mass then occupying the Gulf of Mexico and lost itself in the inchoate molten mass occupying the blasted crater of the fissioned Moon material. | 44466 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| rotation. The Antarctic continent (including the continental shelf of the Ross Sea) is steep- standing in its surrounding ocean. | 44505 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| the uniform half circle are the continental masses of the world. | 44509 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| America persuades us that the original continental land on the east of the fracture is still there. | 44561 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| for the recent rupture of the continental crust that would probably have erased most of the perplexities just evidenced 4 . | 44585 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| being remembered and because of its continental geography, | 44686 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| be a minor feature of the continental slopes of the ocean and a minor canyon among submarine canyons. | 45055 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| of kilometers, first cutting into the continental shelf, | 45057 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| shelf, and then extending down the continental slope to the abyssal plain of the ocean, | 45058 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| the glacial period. That all the continental margins both off stable and unstable coasts could have been subjected to such movements in comparatively recent times is scarcely credible. | 45081 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| It seems quite possible that the continental glaciers during some of the earlier glacial epochs may have been sufficiently thick and sufficiently extended to have allowed a lowering of 3, | 45088 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| allow rivers to cut valleys on continental slopes. | 45116 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| km hr; they account for anomalous continental sand and fossils found on the ocean floor. | 45172 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| question remains to perplex: if the continental blocks were meanwhile rafting over long distances, | 45178 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| achieved, with a slant toward the continental rock against which it is emplaced. | 45197 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| until the tectonic plate theory of continental drift went shopping for its mechanism. | 45199 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| great disruption. Their oceanic sides abut continental walls that are much taller and deeper; | 45208 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| in many or any trenches. The continental wall is of varying chemical composition; | 45210 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| of convection cells and subduction of continental and oceanic material. | 45222 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| Alfred de Grazia CHAPTER TWENTY-FOUR CONTINENTAL TROPISM AND RAFTING A Texas association proclaims the slogan "Stop Continental Drift," | 45285 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| Texas association proclaims the slogan "Stop Continental Drift," | 45287 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| and then, goes the theory of continental drift -that is, | 45296 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 82.6 percent of the total continental area is antipodal to oceanic area." | 45318 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| percentage would appear. He simplified the continental areas into circles and fed their numbered forms into a computer which then randomly placed them to see how much land would be antipodal to oceanic area. | 45323 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| is 68.0 percent of the continental area. | 45327 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| began, then all of the existing continental land would be antipodal to oceans. | 45340 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| basins, we have noted, indicate that continental material was blasted out of the former and pushed aside from the latter. | 45344 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| faster than Africa. But since the continental world was moving generally south as well as east, | 45367 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| down from the Plateau.) The low continental Pangean mass to the south and east ultimately was partly flooded by the waters of the sky, | 45384 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| decelerated rate. The fjords mark sheared continental mass, | 45392 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the Arctic Sea (which is mostly continental) signal the former land mass under the ice cap load. | 45394 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| Mesozoic, and that there were two continental masses, | 45419 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| Thus report Heezen and Hollister. These continental blocks, | 45443 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| a "gravity slide," the creeping of continental masses toward rimming geosynclinal depressions. | 45451 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| time...," 8 he was thinking of continental drift but could better have been speaking for a continental trot, | 45458 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| better have been speaking for a continental trot, | 45459 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| or lunagenic tropism of the continents. Continental drift theory has invented convection currents to move the Earth's plates with whatever continental land may be aboard on long journeys over the Earth. | 45461 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the Earth's plates with whatever continental land may be aboard on long journeys over the Earth. | 45462 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| lunagenic tropism," the tendency of the continental land to move toward the crater of the Moon and to fabricate new crust in compensation for the excisions. | 45472 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| outlined at the edges of the continental shelves. | 45490 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| shelves. But they poorly match the continental shelf morphology across the Pacific Basin. | 45505 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the "drift" of the combined, inseparable continental-oceanic lithosphere. | 45585 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| of oceanic sediments, not to mention continental sial that would happen to be subducted. | 45637 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| either the island arc or the continental crust they are subjected to strong deformation, | 45701 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 70 kilometers, far exceeds the present continental sediments (if the only source of these is oceanic sediments) nor does it appear in any large sedimentary masses distinct from the indigenous continental mass. | 45742 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| sedimentary masses distinct from the indigenous continental mass. | 45744 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| should be unevenly blown, for the continental portion is 40 km and the oceanic crust is only 5 kilometers thick. | 45778 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| oceanic and encounters a plate carrying continental material, | 45790 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| at about 40 km below the continental rock. | 45793 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| temporally brief. The fact that the continental blocks move at a distinctively different, | 45819 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| by G. R. Morton, cannot accept continental drift, | 45914 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| under a force sufficient to cause continental drift should then have amounted to from hundreds to thousands of times more than witnessed in the recent uplifts. | 45937 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| remained intact throughout Earth history. The continental blocks would require much less energy to move into the large areas heretofore occupied by continental material but now unoccupied save by an erupting and boiling mantle material. | 45964 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the large areas heretofore occupied by continental material but now unoccupied save by an erupting and boiling mantle material. | 45966 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| to be ploughed through by the continental blocks heading toward the lunagenic basin. | 45968 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| as with Carey, the writers on continental drift ignore an obvious probability and even necessity, | 45972 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| until the present day. Wegener's continental drift theory is accepted but not its cause. | 46012 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| and the connection between lunagenesis and continental break-up and movement. | 46018 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the other hand, copes well with continental drift theory, | 46041 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| in cosmogony. Notes (Chapter Twenty-four: Continental Tropism and Rafting) 1. " | 46048 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting : Notes (Chapter Twenty-four: Continental Tropism and Rafting) |
| Continental Tropism and Rafting) 1. "The Continental Drift Affair," | 46050 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting : Notes (Chapter Twenty-four: Continental Tropism and Rafting) |
| Triassic Tetrapods from Antarctica: Evidence for Continental Drift," | 46055 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting : Notes (Chapter Twenty-four: Continental Tropism and Rafting) |
| 13 Sep. 1970), 1197-1200. 4. "Continental Drift," | 46058 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting : Notes (Chapter Twenty-four: Continental Tropism and Rafting) |
| 18. G. Robert Morton, "Creationism and Continental Drift," | 46091 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting : Notes (Chapter Twenty-four: Continental Tropism and Rafting) |
| Convection Currents," 1962, unpubl., cf. Cook, "Continental Drift: | 46095 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting : Notes (Chapter Twenty-four: Continental Tropism and Rafting) |
| 1964, Nov. 1964. 20. "Creationism and Continental Drift," | 46098 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting : Notes (Chapter Twenty-four: Continental Tropism and Rafting) |
| not give up sand; sand is continental. | 46153 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| veneer about three-quarters of the continental surface to thicknesses ranging from the merely visible to a dozen kilometers in height, | 46161 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| gap in the geological column. The continental slopes are formed of shaken down, | 46172 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| carried off the shelves in the continental movements and orogeny following lunagenesis. | 46175 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| the foot of many present-day continental slopes." | 46180 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| present-day continental slopes." 5 The continental shelves and the abysses carry clay. | 46180 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| and ooze sediments. Little suggests the continental rock in the oceanic sediments; | 46185 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| of 406 square kilometers of the continental lands 9 . | 46244 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| one another periodically, episodically, spasmodically. "The continental plates, | 46436 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| is rotated topographically, significant summaries of continental and regional data would be generated. | 46489 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| are as much a proof of continental rafting as continental drift is proof of the reason why eels must be astonishing long-distance travelers. | 46617 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| a proof of continental rafting as continental drift is proof of the reason why eels must be astonishing long-distance travelers. | 46617 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| survivors could readily adapt to the continental shelves and slopes, | 46628 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| are more commonly found on the continental shelf with few mutations. | 46640 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| teeth are found far down the continental slopes of North America. | 46657 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| Asia. This fact not only indicates continental rafting, | 46683 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| indicates continental rafting, but also recent continental rafting; | 46683 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| can conceive how, let us say, continental tides of translation might sweep in and deposit a life zone upon one area; | 47098 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| species may guarantee a replenishment of continental scope within centuries. | 47791 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| outer planets as a group. D. Continental "drift" theory would need to permit a negatively exponential rate of movement from a very late breakup of the Pangean crust, | 49014 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| the seabottom as well as on continental land. | 49227 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| an Atlantean concept of great sunken continental areas, | 49237 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| macrochronic reckoning. When Wegener advanced his continental drift theory, | 50264 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| opportunity to join lunar outbursting and continental drift was lost because of vast differences in timing the two events. | 50266 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| events. Both theories, moon-eruption and continental drift, | 50267 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| paleontological ecumenicalism, the moon-eruption, and continental cleavage and rafting. | 50274 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| then the origins and behavior of continental drift are explained, | 50416 THE LATELY TORTURED EARTH: - - - EPILOGUE - |
| s magnetic dip poles across the continental surfaces indicates the complex nature of the causal current through the material making up the Earth's bulk. | 53267 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 8: THE EARTH'S PHYSICAL AND MAGNETIC HISTORY - |
| formations at widely separated locations in continental North America and elsewhere (Saul). | 54513 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| this time the Earth had a continental crust everywhere. | 55414 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| geophysical and paleontological findings of the continental-drift school of thought 88 . | 55418 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| as half of the Earth's continental material rises into the sky, | 55432 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| the Earth. The remainder of the continental mass that had covered the Earth fractured into the complex ocean-ridge and land-rift system viewed today (see Figure 29). | 55498 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| of a number of plates carrying continental crust. | 55508 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| fill the basins up to the continental slopes, | 55538 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| passing Uranus Minor, the surviving broken continental crust of the Earth shattered and rapidly scattered, | 55547 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| the Earth's volume increased. The continental blocks fractured and sometimes folded as they conformed to the underlying shape of the Earth's body, | 55562 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| roughly to the base of the continental shelves. | 55578 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| old and new waters traversed the continental masses in the gorges of the major fractures, | 55584 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| into rivers that poured over the continental shelves and into the abysses, | 55585 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| broad-sheeted run-offs from the continental blocks. | 55588 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| abysses into the atmosphere above the continental blocks. | 55592 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| kilometers into the abyss from the continental shelves was known to the ancients. | 55597 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| basins were filled up to the continental margins, | 55614 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| de Grazia, 1981, 1984b) posits a continental rapid rafting of a thousand years or so, | 55775 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON : Notes on Chapter 13 |
| were quite habitable, even tropical. The continental shelves and slopes had become livable. | 56023 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 14: THE GOLDEN AGE AND NOVA OF SUPER SATURN - |
| continents on what are now the continental shelves and slopes. | 56117 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 14: THE GOLDEN AGE AND NOVA OF SUPER SATURN - |
| river canyons that course down the continental slopes to the abyss were in existence before the Deluge and were now inundated and probably greatly eroded, | 56119 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 14: THE GOLDEN AGE AND NOVA OF SUPER SATURN - |
| basins of the globe, covering the continental margins left dry after the Uranian deluges. | 56123 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 14: THE GOLDEN AGE AND NOVA OF SUPER SATURN - |
| Meservey, R. (1969), "Topological Inconsistency of Continental Drift on the Present-Sized Earth," | 59844 SOLARIA-BINARIA: - - - BIBILIOGRAPHY - |
| would have welcomed the theory of continental drift in vogue today, | 61882 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : AMEGHINO'S ARGENTINE HOMINIDS |
| had moved North and East across continental connections. | 61886 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : AMEGHINO'S ARGENTINE HOMINIDS |
| understood in terms of a catastrophic continental drift with great global overthrusts and subsequent catastrophic read-justments that have really been the facts that have shaped the region... | 62205 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : OLDUVAI GORGE |
| defined, the occurrences of catastrophes of continental, | 62655 HOMO SCHIZO I: - - Chapter 3: MECHANICS OF HUMANIZATION : ANCIENT CATASTROPHES |
| which cut off peoples by splitting continental blocks, | 65935 HOMO SCHIZO I: - - Chapter 5: CULTURAL REVOLUTION : AMERICAN CULTURAL ORIGINS |
| raised, scoured and ploughed on a continental scale. | 77545 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 1: SACRED SCANDAL AND DISASTER Chapter 4: CATASTROPHE AND SUBLIMATION : THE GENERAL THEORY OF CATASTROPHE |
| sky changes, orientations change. (Nature) 4. "Continental crust found 450 miles west of Gibraltar." | 101923 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| at Cretaceous- Tertiary boundaries. Cf. galloping continental drift in Chaos and Creation. | 101952 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| Controversy over evidence of "plate tectonic" continental drift without continents on Venus (Venera 14 findings) (BBC, | 101999 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| cover depositional chemical environments ranging from continental and coastal soils to marsh and subtidalmarine deposits" of recent ages had disclosed complex polycyclic aromatic hydrocarbon assemblages (PAH) with "a high degree of similarity in the molecular weight distribution of the many series of alkyl homologs" 42 . | 102909 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 2: THE BURNING OF TROY : A NEW INTERDISCIPLINARY METHOD |
| Nature magazine upon the evidence of continental crust that lies foundered beneath the Tyrrhenian Sea. | 104047 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 5: THE CATASTROPHIC FINALE OF THE MIDDLE BRONZE AGE - |
| of Africa were destroyed that the continental population noticeably blackened after the event. | 104636 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 7: NINE SPHERES OF VENUSIAN EFFECTS - |
| out from the atmosphere, including airborne continental dust and biological material, | 105323 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 11: ICE CORES OF GREENLAND - |
| Flow Models, Isotopes, Volcanic Debris, and Continental Dust," | 105712 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 11: ICE CORES OF GREENLAND : Notes (Chapter 11) |
| movements over many millions of years - continental drift, | 110382 THE BURNING OF TROY: PART 5: COMMUNICATING A SCIENTIFIC MODEL: Chapter 27: A COSMIC DEBATE : EVOLUTIONARY AND REVOLUTIONARY PRINCIPLES |
| Potassium40 - Argon40 Radiochronometry;" "Migrating Eels and Continental Drift;" | 111417 THE BURNING OF TROY: PART 5: COMMUNICATING A SCIENTIFIC MODEL: Chapter 28: SYLLABI FOR QUANTAVOLUTION - |
| Problems of Quantavolution. Ice Ages theory. continental drift and plate tectonics, | 111567 THE BURNING OF TROY: PART 5: COMMUNICATING A SCIENTIFIC MODEL: Chapter 29: I.Q.: A UNIVERSITY PROGRAM : CURRICULUM |
| eruption from planets," "solar uncertainty"), geology (" continental drift" and "catastrophic end of the Ice Age"), | 112158 THE BURNING OF TROY: PART 5: COMMUNICATING A SCIENTIFIC MODEL: Chapter 30: PAST, PRESENT, AND FUTURE : THE POLITICS OF UNIFORMITARIANISM |
| meteorite. The patient described that large continental mass above as a sheet of ice. | 125890 RECOLLECTIONS OF A FALLEN SKY - VELIKOVSKY AND CULTURAL AMNESIA : - - - |
| forms that he observed. On the continental scale he observed that life forms, | 126695 RECOLLECTIONS OF A FALLEN SKY - VELIKOVSKY AND CULTURAL AMNESIA : Chapter 1: CULTURAL AMNESIA : SUPPRESSION AND REGRESSION |
| meteorite. The patient described that large continental mass above as a sheet of ice. | 128291 RECOLLECTIONS OF A FALLEN SKY - VELIKOVSKY AND CULTURAL AMNESIA : Chapter 3: PSYCHOLOGICAL ASPECTS OF THE WORK OF IMMANUEL VELIKOVSKY - |
| making, like floods, earthquakes, and sudden continental shifts. ' | 137398 THE VELIKOVSKY AFFAIR: PART 3: THE INCONSTANT HEAVENS - - - |