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CRUSADES..................2 (0.000%)
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| As Anselm seeks proof, King Arthur crusades. | 98892 THE DEVINE SUCCESSION PART 1: THEOMACHY Chapter 8: INDISPENSABLE GODS - |
| judgments, as we see in the Crusades, | 99552 THE DEVINE SUCCESSION PART 2: THEOTROPY: Chapter 10: ETHICS AND THE SUPERNATURAL - |
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CRUSHED...................7 (0.001%)
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| are recognizable unless subsequently melted or crushed. | 23393 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : THE FOSSIL RECORD AND MUTATING TIME |
| the uniformitarian and gradual evolutionists and crushed in the same battles that saw the defeat of the creationists. | 32887 THE LATELY TORTURED EARTH: - - CHAPTER 1: Quantavolutions - |
| terrible bodies of the giants lay crushed beneath their own massive structures, | 37409 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 9 Gases, Poisons and Foods - |
| Flotation is employed to separate the crushed particles according to their density. | 37894 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| likely to see exoterrestrial intruders smashed, crushed and exhibiting metal here and there; | 37903 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| by the current, or from being crushed and broken up by the trampling of animals that came to drink. | 46830 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| in his writings were from the crushed cultures of -776 to the beginning of his own lifetime. | 79073 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 2: GODS, PLANETS, MADNESS Chapter 7: CRAZY HEROES OF DARK TIMES : THE CART BEFORE THE HORSE |
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CRUSHES...................1 (0.000%)
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| the Devil and by hostile humans, crushes his life-values: | 66554 HOMO SCHIZO I: - - Chapter 6: SCHIZOID INSTITUTIONS : GROUP VS. INDIVIDUAL |
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CRUSHING..................11 (0.001%)
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| rise to a peak swiftly, inflict crushing blows, | 22520 CHAOS AND CREATION: - - CHAPTER 02: HIGH ENERGY FROM SPACE : THE EXPONENTIAL PRINCIPLE |
| Antarctic find. It is extracted by crushing and leaching its host rock. | 37845 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| isolate ore are imitations of nature. Crushing is first, | 37890 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| sky-high came the sea-wall, crushing all things," | 40045 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| a murky and stagnant inferno under crushing pressures many times greater than those on Earth. | 56710 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 16: VENUS AND MARS - |
| expressions including spectres and pandemonium; of crushing and effacing effects that are prolonged and of high intensity; | 63811 HOMO SCHIZO I: - - Chapter 3: MECHANICS OF HUMANIZATION : SOCIAL IMPRINTING |
| crop failure, economic depression, or a crushing defeat by a hostile army. | 66818 HOMO SCHIZO I: - - Chapter 6: SCHIZOID INSTITUTIONS : AUTHORITY |
| Greek-speaking and Middle East areas, crushing damage to late Mycenaean and early Hellenic civilization occurred in the period -776 to -687. | 78350 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 2: GODS, PLANETS, MADNESS Chapter 6: THE RAPE OF HELEN : THE AGE OF MARS |
| resources, that he could evade a crushing preemptive suppression were effects of his workable scheme. | 91122 GODS FIRE: - - Chapter 6: THE CHARISMA OF MOSES : SCIENTIST AND INVENTOR |
| even though no event is as crushing as the withdrawal of love, | 109695 THE BURNING OF TROY: PART 4: POLEMICS AND PERSONAGES: Chapter 24: THE OUTLOOK OF SCIENTISTS : ALL SCIENCE IS SOCIAL SCIENCE |
| felt that he could score a crushing victory over his opponents. | 138120 THE VELIKOVSKY AFFAIR: PART 4: CUNEIFORM ASTRONOMICAL RECORDS AND CELESTIAL INSTABILITY - - - |
| |
|
CRUSHINGLY................1 (0.000%)
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| was the Deity who came down crushingly on Earth, | 52518 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 5: THE SAC AND ITS PLENUM : Notes on Chapter 5 |
| |
|
CRUSOE....................1 (0.000%)
|
| the Sun, of Defoe's Robinson Crusoe, | 77105 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 1: SACRED SCANDAL AND DISASTER Chapter 2: THE SONG OF LOVE : THE PHAEACIAN UTOPIA |
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CRUST.....................298 (0.037%)
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| Basin as the source of the crust that was wrenched from the Earth by an electrically attractive passing body, | 963 QUANTAVOLUTION AND CATASTROPHE: PART 3: A Comment on the Q-C Test and Its Individual Items - - - |
| 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 - - - |
| of metal Crozier, W. D. crucifiction crust, | 2385 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| crucifiction crust, displacement of Earth's crust, | 2386 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| earth charge earth chimney, hoodoos Earth crust Earth dilation Earth energy Earth expansion Earth figure Earth fracture Earth history Earth interior Earth magnetism Earth Mother Earth pole Earth radius Earth size Earth surface Earth's mantle Earth, | 2620 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| Pacific Ocean ca 11500 for much crust was lost as the larger element of outer planets (Uranus-Neptune, | 8037 COSMIC HERETICS: PART 1: - Chapter 3: CHEERS AND HISSES - |
| that wrenched away half of the crust, | 12343 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| from the original precipitous outburst of crust. | 12352 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| years ago, balked at picturing the crust of the Earth exploding into space to form the Moon a few thousands years earlier. | 12387 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| of the modern skies and terrestrial crust were seeming to make a point. | 12511 COSMIC HERETICS: PART 3: - Chapter 10: ABC'S OF ASTROPHYSICS - |
| should in theory the earth's crust contain them? | 15382 COSMIC HERETICS: PART 4: - Chapter 12: THE THIRD WORLD OF SCIENCE - |
| says that the turbulence of the crust descends to greater depth. | 15383 COSMIC HERETICS: PART 4: - Chapter 12: THE THIRD WORLD OF SCIENCE - |
| had earlier caused the Earth's crust to erupt the moon. | 19127 COSMIC HERETICS: PART 5: - Chapter 16: PRECURSORS OF QUANTAVOLUTION - |
| The Preferred Altitiudes of Earths Crust 19. | 21375 CHAOS AND CREATION: - - - TABLE OF CONTENTS - |
| find memorials in the Earth's crust, | 21511 CHAOS AND CREATION: - - - INTRODUCTION : THE UNIFORMITIARIAN RESISTANCE |
| a fracture of the Earth's crust will reduce the energy of the braking and increase the time given to it. | 21753 CHAOS AND CREATION: - - CHAPTER 01: COSMIC INSTABILITY : IMPACTS ON EARTH |
| Earth could have acquired a hard crust in a thousand years (if radioactive internal heating is ignored) 7 . | 21779 CHAOS AND CREATION: - - CHAPTER 01: COSMIC INSTABILITY : IMPACTS ON EARTH |
| lava and great chunks of Martian crust, | 21820 CHAOS AND CREATION: - - CHAPTER 01: COSMIC INSTABILITY : THE CLEAVAGE OF MARS: A PARTICULAR CASE |
| be altered and even reversed. The crust or shell of the bodies, | 22092 CHAOS AND CREATION: - - CHAPTER 02: HIGH ENERGY FROM SPACE - |
| long distances. Different layers of the crust may move at different speeds and for some miles down. | 22247 CHAOS AND CREATION: - - CHAPTER 02: HIGH ENERGY FROM SPACE : SEISMISM AND VOLCANISM |
| preferred levels in the Earth's crust." | 22745 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| periods of time, have fluxed the crust of the Earth so thoroughly that a great many strata of false identity and false age have been created. | 22768 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| of Pangea, the wholly continental Earth-crust that we postulate in this book. | 22893 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : CORAL REEFS |
| be found in rocks of the crust of the Earth, | 22920 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RADIODATING |
| is that any magnetism of the crust is primordial except where the crust has suffered a melt or welled up as new crust from the interior magma. | 23382 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : MAGNETISM |
| crust is primordial except where the crust has suffered a melt or welled up as new crust from the interior magma. | 23383 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : MAGNETISM |
| melt or welled up as new crust from the interior magma. | 23383 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : MAGNETISM |
| or movement of the Earth's crust can form all of these features in short intervals of time. | 23538 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : 58 TESTS IN DISPUTE |
| term "Pangaea" to mean the continental crust, | 24349 CHAOS AND CREATION: - - CHAPTER 04: A CATASTROPHIC CALENDAR : Notes (Chapter Four: A Catastrophic Calendar) |
| was maintained, without abrupt interruption. The crust of Pangea was sial, | 24828 CHAOS AND CREATION: - - CHAPTER 05: SOLARIA BINARIA : THE WORLD OF PANGEA |
| and aluminum elements, as is the crust today. | 24828 CHAOS AND CREATION: - - CHAPTER 05: SOLARIA BINARIA : THE WORLD OF PANGEA |
| as much was on the original crust of Pangea. | 24831 CHAOS AND CREATION: - - CHAPTER 05: SOLARIA BINARIA : THE WORLD OF PANGEA |
| Pacific Rise are indicative of a crust that had been suddenly greatly thinned. | 26413 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| had been suddenly greatly thinned. The crust would not have been removed so deeply where land masses exist today. | 26415 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| of inertia of the earth's crust is about 200 times less than that of the planet as a whole." | 26422 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| direct ejection of fragments of the crust in explosions and of ash and gas during volcanic eruptions, | 26426 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| would slip past, beneath the surface crust, | 26443 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| between the inner Earth and its crust, | 26444 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| but a large part of its crust would be stripped off in a set of gigantic swirling typhoons. | 26451 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| heat from the explosions of the crust, | 26462 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| other portions of the Earth's crust, | 26465 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| 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 |
| molten Pacific basin, bereft of continental crust, | 26471 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| of a portion of the sial crust of the earth." | 26512 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| sial is deeply embedded in the crust. | 26515 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| 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 |
| reveal a general composition resembling the crust and upper mantle of the Earth 17 . | 26535 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| one get a 65-kilometer-thick crust that is 50 to 85 percent plagioclase without melting most of the moon? | 26538 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| the surface of the Earth. Its "crust" is igneous anorthosite to a great depth 20 . | 26558 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| be derived from the Earth's crust. | 26561 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| the Earth's crust. The Moon crust is ten to twenty times the crust of the Earth in thickness accounting for nearly half of the Earth's crust. | 26561 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| is ten to twenty times the crust of the Earth in thickness accounting for nearly half of the Earth's crust. | 26562 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| nearly half of the Earth's crust. | 26562 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| body forming from the Earth's crust, | 26618 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| 22. Anorthosite of the Moon's crust may be formed in only 1000 years 41 . | 26622 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| either more or less than the crust, | 26644 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| or less than the crust, the crust will be slung off. | 26644 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : LUNAR CONFORMITIES TO ERUPTION |
| continental shelves, and torques of the crust-that are conceptualized in the text. | 26712 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| the figure outlines the estimated devastated crust and expanded surface of the globe. | 26732 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| that had been created in the crust. | 26774 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| world the level at which the crust exploded and the crust slipped. | 26852 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : GLOBAL EXPANSION |
| which the crust exploded and the crust slipped. | 26852 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : GLOBAL EXPANSION |
| and by the substances of the crust. | 26893 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE MAGNETIC FIELD |
| Uranus Minor that ripped off the crust of the Pacific hemisphere. | 26910 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE MAGNETIC FIELD |
| 000 years. OCEAN DEVELOPMENT Earth's crust was half erupted into space upon the intrusion of Uranus Minor without Earth's losing its atmosphere; | 26948 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : OCEAN DEVELOPMENT |
| 1966) 3 who estimates Earth's crust might solidify in 1000 years. | 27698 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : Notes (Chapter Seven: Earth Parturition and Moon Birth) |
| basalt, volcanically transformed, placed where the crust had been removed and between the separating continents. | 28252 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN : THE DOWNFALL OF SATURN : NOVA AND DELUGE |
| to imagine so much of the crust skimming into space. | 30546 CHAOS AND CREATION: - - CHAPTER 11: THE DEVIL'S ADVOCATE - |
| force required to pull away the crust, | 30549 CHAOS AND CREATION: - - CHAPTER 11: THE DEVIL'S ADVOCATE - |
| the Moon was torn from the crust of the Earth in recent memory. | 30760 CHAOS AND CREATION: - - CHAPTER 12: VICTORY OF THE SUN - |
| somewhere else, too, when half the crust of the Earth exploded into space. | 30971 CHAOS AND CREATION: - - CHAPTER 12: VICTORY OF THE SUN : THE PROPENSITY TO SURVIVE |
| Evidence for Recent Rupture of Continental Crust," | 31364 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| R. A. (1923), "The Earth's Crust and its Stability: | 31401 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| 1881), Physics of the Earth's Crust, | 31525 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| years is accorded the Earth's crust, | 33750 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| of 62 Suns. Even if the crust of the Earth is shoved around independently of the underlaying layers, | 34265 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| shape would have been altered, the crust would have been half removed, | 34469 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| have tilted the globe, removed the crust, | 34471 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| slippage. The Earth's shell or crust, | 34487 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| the moment when over half the crust was being blasted into space, | 34500 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| be increased if B has a crust floating on a molten interior, | 35497 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 6 Cosmic and Terrestrial Lightning - |
| to be torn from the lunar crust in numbers sufficient to trigger an interplanetary discharge. | 35547 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 6 Cosmic and Terrestrial Lightning - |
| by hot spots in the deep crust or mantle, | 35793 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| on a couple of miles of crust; | 35919 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| 85 of the exposed Earth's crust which is of igneous rock is all nearly as young as the ash levels, | 36303 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| material akin to the Earth's crust, | 36665 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| the tektites to the protosialic upper crust of the primeval earth." | 36730 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| large body exploded the Earth's crust to make them or a meteoroid impact did the job. | 36741 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| considerable portion of the Earth's crust should be composed of gathered-in planetary dust, | 36790 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| 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 - |
| considerable part of the Earth's crust is exoterrestrial and has fallen as dust and stone not long ago. | 36869 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| and volume for the Earth's crust that a young age for the Earth or a very young age for the catastrophized Earth suggests itself. | 36894 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| nickel core, sima mantle, and sial crust. | 37770 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| highly dispersed, fine grains throughout the crust, | 37871 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| we include the entire earth's crust in our consideration." | 37873 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| several kilometers of the earth's crust rather than throughout the total 35 km thickness of the continents or the thicker upper mantle. | 37876 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| ores at great depths in the crust, | 37880 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| axial tilt, a slippage of the crust above the mantle, | 38665 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| in weight of the earth's crust. | 38680 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| occurred upon a newly formed Earth crust, | 38876 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| contributing to the loosening of the crust. | 38956 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| 16. Op. cit., 2. 17. " Deep Crust Hints at Meteoritic Impact," | 39054 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions : Notes (Chapter Eleven: Encounters and Collisions) |
| skies, and then fallen when a crust had formed and cooled below 212 . | 39161 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| If all the earth's present crust were a uniform level, | 39177 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| unsuspected natural trend of the continental crust to lose its water holdings, | 39301 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| and around, but also its very crust, | 39934 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| extensive tides of magma beneath the crust. | 39965 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| have occurred. Presumably, too, the "solid crust" would soon warp and flow to erase much of the change. | 40024 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| it is a wonder that the crust of the Earth is not a homogenous finely ground mixture of all past life and surfacing rocks. | 40512 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| The result would be a homogenized crust. | 40525 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| accumulating weight, bore down upon the crust so heavily as finally to cause a rupture of the rim of the crater. | 40751 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| of Super-Uranus. The Earth's crust burst. | 40859 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| and blow-off of the Pacific crust. | 40862 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| cleaved, lost most of its continental crust, | 40870 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| 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 - |
| the underlying rifted area of the crust. | 41211 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| shallow focus and originate within the crust, | 41247 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| line of catastrophic slippage of the crust on several past occasions; | 41249 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| disturbances in the overhanging rock or crust of the continental and oceanic bottoms? | 41260 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| are decaying in the mantle and crust. | 41263 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| circles the Pacific area of erupted crust, | 41364 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| down, because of a loss of crust and an expansion of crust, | 41642 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| of crust and an expansion of crust, | 41642 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| only possible if the earth's crust is stretched and fractured through tectonic forces. | 41764 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| sialic rocks within the earth's crust 13 . | 41772 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| a stretching and tearing of the crust, | 41775 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| over the globe, the still landed crust moved in reaction to the eruption of the Moon. | 41782 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| special fractures of the Earth's crust. | 41883 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| a gaseous fission, or a thin crust, | 41928 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| 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 - |
| has sunk or from which the crust has been removed should not halt the argument. | 42146 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| and a great amount of continental crust is missing. | 42367 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| lodge itself into Asia. Half the crust of the earth was gone and the earth was expanding somewhat so that there was plenty of room for maneuver and titanic forces to propel the rafts. | 42428 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| of the Pacific rests upon a crust 20 to 30 kilometers thick; | 42689 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| thick; this is characteristic of continental crust, | 42690 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| of continental crust, not of oceanic crust, | 42690 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| land, but that the stripping of crust by the moon eruption brought on lateral avalanching to the north and west and a sinking generally in this sector. | 42694 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| the active element, and the brittle crust on which we live is passively tiding on this very slow flow. | 42828 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| acting differentially on irregularities in the crust and its surface topography, | 42830 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| lower side of the comparatively passive crust. | 42840 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| pushing up and pulling down the crust, | 42948 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| of mass consists of half the crust and most of a dense atmosphere, | 42984 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| a part of the Earth's crust fifty miles in thickness were to have its temperature raised 200 F, | 43029 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| of over half the Earth's crust, | 43098 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| for a complete melting of the crust of the Earth. | 43116 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| The loosening of the Moon-making crust and the cleaving of the globe would take place quickly; | 43129 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| be less dense than the escaping crust but only that temporarily it be in a molten state, | 43142 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| reduces its melting point. The lower crust and mantle boundary might melt at as low a temperature as 500 C under water saturation. | 43148 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| rain, snow, and ice. The upper crust on which the biosphere and sediments rested would be shielded from the abyssal heat by thousands of volcanic vents penetrating its surface and by the cyclonic venting of heat into space over the immense flayed crater of the Moon. | 43153 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| discharging it, wholly or partially. The crust of the earth resembles a Leyden jar, | 43220 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| daily expansion and contraction of the crust. | 43223 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| 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 - |
| 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 - |
| Why have not forces in the crust long since reached an equilibrium? | 43351 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| as they plough through the oceanic crust. | 43377 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| to pull out over half the crust. | 43413 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| so well portrays proceed: the remaining crust fractures down to the mantle in an explosive network providing the globe-girdling rift and fault system. | 43417 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| a force gripping or pushing the crust of the Earth like a shell so that it moves independently of the mantle and core. | 43426 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| rotates out of step with the crust. | 43430 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| the crust. The contacts of the crust with the plasmas of space and with its atmosphere may set up a continuous drag and eccentricity on the mantle, | 43430 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| evidences a clockwise rotation of the crust in relation to the core of 70 . | 43439 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| of the basal movement of the crust, | 43497 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| 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 - |
| into abundant mountains while the oceanic crust slides up and under and around without making mountains, | 43557 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| its formations of the Earth's crust, | 43603 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| biosphere products. Still, if upon the crust of the Earth were laid the seeds of plants and the eggs of animals, | 43612 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| several thousand years would find the crust blanketed kilometers deep in biotic debris. | 43615 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| enough; the Earth's surface and crust are a complicated mixture, | 43623 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| and materials of the Earth's crust are but the work of a clumsy chef, | 43628 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| earthly blisse." While the Earth's crust is reforming into the Moon, | 43640 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| for whole continents over the ocean crust where overthrusting has been several thousand miles (continental drift), | 43657 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| plateaus caused by a heat-expanded crust that cooled in its expanded form at great heights. | 43681 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| Earth has lost most of its crust, | 43883 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| vol. II, fig. 17. The lithosphere (crust) is everywhere shallowest beneath the ridge lines. | 43957 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| flows. This is but the cooled crust of the exposed magma of the mantle. | 44045 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| in itself suggests that the ocean crust is the product of a melt, | 44106 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| or explosion. The fact that ocean crust is more 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 - |
| or less acid than the continental crust indicates that it separated from the primeval melt after the granitic crust; | 44109 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the primeval melt after the granitic crust; | 44109 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| 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 - |
| no thickening of the ocean basin crust beneath the ridges, | 44154 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| 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 - |
| into abundant mountains; but the oceanic crust, | 44165 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| volume than solidified basalt; wherever the crust was boiling, | 44203 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| a plate of the earth's crust carrying the landmass of India collided with the plate carrying Asia some 45 million years ago, | 44243 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| cut its swath from the Pacific crust and staggered the Earth to a momentary pause, | 44447 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| the full depth of the continental crust, | 44451 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| was the limit of the exploded crust. | 44514 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| understandable if the Rise had no crust, | 44535 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| the recent rupture of the continental crust that would probably have erased most of the perplexities just evidenced 4 . | 44586 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| of a sudden unloading of the crust followed by a normal relaxation." | 44591 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| splitting and rafting of the Arctic crust in order to completely remove this magnetic anomaly." | 44613 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| into the mounting temperature of the crust and mantle, | 44620 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| crack radially. In addition the weakened crust beneath the cap would give way. | 44657 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| flayed the Earth of half its crust, | 44674 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| the northeast. Thus a swath of crust was removed that began narrowly in the North, | 44681 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| balance the world by redistributing the crust and by expansion and to vent gases and heat during the process. | 44782 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| and often long slits in the crust are found in various regions but are especially prominent around the Pacific. | 45190 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| the transition from the thin oceanic crust to the thick foundation of the island arc." | 45215 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| to believe that the Earth's crust has been, | 45288 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| been, and is, in motion. The crust is thin below the ocean bottoms and thick beneath the continents. | 45288 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the movements of the Earth's crust recently, | 45316 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| of over half the Earth's crust in what is mostly now southern hemispheric ocean. | 45346 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| preferred levels in the Earth's crust." | 45438 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| earth's mantle while the ocean crust is but a thin 5000-meter- thick film frozen over the earth's massive mantle." | 45441 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| between the mantle below and the crust above; | 45463 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the Moon and to fabricate new crust in compensation for the excisions. | 45473 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| West. It met little resistance. The crust had been vaporized, | 45513 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| from the east while the oceanic crust of its west is being subducted into the long western trench. | 45617 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| get caught between the subducting oceanic crust and either the island arc or the continental crust they are subjected to strong deformation, | 45700 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 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 - |
| It is about 5 of the crust. | 45747 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| The thickness of the Earth's crust, | 45776 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 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 - |
| Mohorovicic Discontinuity as the boundary between crust and mantle. | 45779 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 3.3, the mean for the crust being 2. | 45781 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| five kilometers thickness. Below the oceanic crust, | 45783 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| visualizes the conveyor belts of ocean crust moving along between ridges and trenches just above the Moho Discontinuity. | 45788 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| ocean, the level above which new crust had to be created from the uppermost magma of the mantle with atmospheric chemical participation. | 45798 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| was born as the boundary between crust and mantle. | 45803 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| greater weight" (relative to the oceanic crust) than with the historical fact of their quite different genesis. | 45820 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the disturbance of the Earth's crust and mantle would form a large area of surface directed as a narrowing cone into the mantle until it reached a point below which seismism could not be energized. | 45841 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| upon the sima of the oceanic crust has surely to do with the greater depth of the continents as contrasted with the oceanic crust, | 45848 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| continents as contrasted with the oceanic crust, | 45849 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| as the average viscosity of the crust and upper mantle, | 45902 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| key to the movement of the crust. | 45959 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| into cold space with the exploded crust. | 45961 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| to the movement of the remaining crust would be much less than if the crust of the Earth had remained intact throughout Earth history. | 45963 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| be much less than if the crust of the Earth had remained intact throughout Earth history. | 45964 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| else admit some expansion of the crust. | 45982 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| The immense typhoon that conveyed the crust of the Earth into space would have carried away with it most of the heat generated in the transaction, | 46025 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| of melted sediments, making the original crust out to be a thin basalt covering where the upper mantle has cooled. | 46189 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| of a melt of an earlier crust by an exoterrestrial encounter. | 46207 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| was coated with a rougher opaque crust of partially fused sand. | 46783 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| of the Earth's poles and crust could produce the requisite shortening of the tempo of evolution. | 47451 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| the capacity of forces within the crust of the Earth to produce global catastrophe on this time scale;" | 47611 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| much rarer in the Earth's crust than in presumably exploded and space-affected meteorites. | 47689 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| stripping of half the Earth's crust and an associated expansion and cleavage of the Earth, | 47771 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| factors active in the earth's crust." | 48841 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| very late breakup of the Pangean crust, | 49015 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| the active element, and the brittle crust on which we live is passively riding on this very slow flow. | 49072 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| acting differentially on irregularities in the crust and its surface topography, | 49075 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| would have destroyed the Earth's crust entirely, | 49560 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| belief that electric charges within the crust and their magnetic fields are either constant or do not affect rates of radioactive decay of the elements whose decay is used as a measuring rod. | 49884 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| secondary transmutations in the earth's crust each year. | 49921 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| natural" radioactivity is concentrated within the crust of the Earth. | 49927 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| missing half of the Earth's crust by removing it, | 50078 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| hemisphere. They can place the removed crust on the Moon and in planetary space. | 50079 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| conductive nature. By contrast, the superficial crust of the Earth consists of more poorly conducting species. | 53148 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 8: THE EARTH'S PHYSICAL AND MAGNETIC HISTORY - |
| 425 K since the Earth's crust separated (Miller and Urey). | 53663 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 9: RADIANT GENESIS - |
| struck. The assault would crack the crust in many places (Norman et al., | 54638 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| 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 - |
| Uranus Minor reaches a maximum. The crust on the side closest to the intruder cracks and fragments. | 55431 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| Minor peeled a deep swath of crust (and some upper mantle material) from the Central Pacific and to lesser depth from the great seamount area west of the Americas. | 55437 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| by a complete shell of granitic crust. | 55444 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| the Earth encountered Uranus Minor. That crust which remains was once clustered around the ancient North rotational pole, | 55445 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| so that one point on the crust (magnetic south) was always leading on the orbit (see above) and the point on the opposite side (magnetic north) was always trailing (see over page). | 55457 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| compare with Figure 18), tearing away crust and creating the Moon Basin where shown. | 55464 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| Southern Hemisphere of the Earth's crust, | 55478 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| Earth entirely. Here, over half the crust was ejected, | 55483 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| was concentrated at the interface of crust and mantle and at the bottom of the moon basin. | 55492 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| 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 - |
| part by subsequent torques of the crust, | 55516 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| water carried away with the lost crust, | 55525 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| 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 - |
| ridges and faults of the current crust were sculptured as the Moon was torn from the Earth and as the Earth recoiled and recovered from that devastating encounter with Uranus Minor. | 55550 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| discontinuity, which is found beneath the crust throughout the world, | 55570 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| the level at which the ancient crust was served from the underlying solid. | 55571 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| close by the Earth (E), tearing crust away and forming the Moon in the process. | 55660 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| removed half of the Earth's crust when it departed. | 55669 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| origin and the Earth's missing crust. | 55708 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| Its sixty-five kilometers of anorthosite crust reveals that it was melted or, | 55726 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| lava and great chunks of Martian crust; | 57022 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 16: VENUS AND MARS - |
| al.). The carbonate rocks of the crust have locked away most of the potential supply of this gas. | 57048 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 16: VENUS AND MARS : Notes on Chapter 16 |
| junction which separates the Earth's crust and mantle. | 58820 SOLARIA-BINARIA: - - - GLOSSARY - |
| Leakage of rare gases from the crust is too great to permit any reliable dating. | 62223 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : OLDUVAI GORGE |
| the atmosphere, cleaved and ravaged the crust of the earth, | 62682 HOMO SCHIZO I: - - Chapter 3: MECHANICS OF HUMANIZATION : ANCIENT CATASTROPHES |
| to build more than a narrow crust of trust, | 68796 HOMO SCHIZO I: - - Chapter 7: PSYCHOPATHOLOGY OF HISTORY : SCHIZOTYPICALITY AND HOMO SAPIENS |
| The moon is enveloped by a crust of igneous anorthosite to the depth of 35 kilometers, | 80423 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 2: GODS, PLANETS, MADNESS Chapter 9: THE RUINED FACE OF A CLASSIC BEAUTY : THE INNOCENT ASTRONAUTS |
| surface of Mars, ripping off the crust in a swirling motion beginning at the eastern end of the canyon called Coprates." | 81760 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 2: GODS, PLANETS, MADNESS Chapter 11: THE BLASTED CAREER OF THE MIGHTY SWORDSMAN : THE FATAL WOUND |
| shearing friction. New levels of surface crust are developed on all of the bodies, | 82850 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 2: GODS, PLANETS, MADNESS Chapter 13: HOW THE GODS FLY : ELECTRO-MECHANICS OF THE GODS |
| number of possible movements of the crust resulting from combinations of decelerating and tilting forces; | 85907 GODS FIRE: - - Chapter 1: PLAGUES AND COMETS : THE DESTRUCTION OF EGYPT |
| or all of the Earth's crust, | 87683 GODS FIRE: - - Chapter 3: CATASTROPHE AND DIVINE FIRES : YAHWEH'S ELECTRICAL FIRE CONGLOMERATE |
| widely dispersed over the Earth's crust, | 87693 GODS FIRE: - - Chapter 3: CATASTROPHE AND DIVINE FIRES : YAHWEH'S ELECTRICAL FIRE CONGLOMERATE |
| of the depth of the surface crust of the Earth to the radius of the whole globe, | 96259 THE DEVINE SUCCESSION PART 1: THEOMACHY Chapter 1: THE GENESIS OF RELIGION - |
| And as the thickness of the crust varies beneath oceans and continents, | 96260 THE DEVINE SUCCESSION PART 1: THEOMACHY Chapter 1: THE GENESIS OF RELIGION - |
| changes, orientations change. (Nature) 4. "Continental crust found 450 miles west of Gibraltar." | 101923 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| Commercial Appeal). 25. Ophiolites (from oceanic crust) found in mountain sediments suggest catastrophic oceanbed lava extrusions buckling to form mountains. ( | 102040 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| wrench around so much of the crust of the Earth at a single moment of time? | 102709 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 2: THE BURNING OF TROY : THE "BURNT CITY" OF TROY |
| magazine upon the evidence of continental crust that lies foundered beneath the Tyrrhenian Sea. | 104048 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 5: THE CATASTROPHIC FINALE OF THE MIDDLE BRONZE AGE - |
| the Earth - the depth of the crust, | 105533 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 11: ICE CORES OF GREENLAND - |
| the top of the Earth's crust, | 106424 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| Ocean cleavage that moved the African crust eastwards and from an accompanying expansion of the Earth. | 106527 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| globe of the world "cleaved," the crust of the earth "convulsed," | 107796 THE BURNING OF TROY: PART 3: WORKING OF THE MIND: Chapter 19: THE 'UNCONSCIOUS' AS A LITERARY REVOLT AGAINST SCIENCE - |
| the axis with respect to the crust of the earth has gained the acceptance of science. | 135005 THE VELIKOVSKY AFFAIR: PART 1: MINDS IN CHAOS - - - |
| of Charles Hapgood (Earth's Shifting Crust), | 136202 THE VELIKOVSKY AFFAIR: PART 2: AFTERMATH TO EXPOSURE - - - |
| deep canyon, or 'crack in the crust that runs nearly twice around the earth. ' | 140598 THE VELIKOVSKY AFFAIR: PART 7: ADDITIONAL EXAMPLES OF CORRECT PROGNOSIS - - - |
| sudden and total shift in the crust only 26 and 32 centuries ago, | 140603 THE VELIKOVSKY AFFAIR: PART 7: ADDITIONAL EXAMPLES OF CORRECT PROGNOSIS - - - |