| |
|
OCEANA....................1 (0.000%)
|
| William of occultism ocean ocean basin Oceana, | 4415 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| |
|
OCEANBED..................1 (0.000%)
|
| found in mountain sediments suggest catastrophic oceanbed lava extrusions buckling to form mountains. ( | 102041 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| |
|
OCEANIA...................7 (0.001%)
|
| the "New World" as well as Oceania had once their Uranian humans and will, | 25907 CHAOS AND CREATION: - - CHAPTER 06: THE URANIANS : OLD AND NEW WORLD CONCORDANCES |
| Cycle of the Moon-Bone," XIX Oceania (September), | 31202 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| Europe, Africa, and Asia, so for Oceania. | 42678 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| islands of South and East Asia. Oceania was born, | 45521 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| predecessors, diffused through Asia, Africa, and Oceania, | 70477 HOMO SCHIZO II: - - Chapter 1: THE NORMALLY INSANE : GENETICS: ARE THERE HOMINIDS AMONG US? |
| Cycle of the Moon-Bone," XIX Oceania (September, | 78075 THE DISASTROUS LOVE AFFAIR OF MOON AND MARS PART 1: SACRED SCANDAL AND DISASTER Chapter 5: HOLY DREAMTIME : Notes (Chapter 5: Holy Dreamtime) |
| although small populations in Africa and Oceania pursued such practices until this century, | 97841 THE DEVINE SUCCESSION PART 1: THEOMACHY Chapter 6: RITUAL AND SACRIFICE - |
| |
|
OCEANIC...................94 (0.012%)
|
| transform absolute zero absorption Abydos abyss, oceanic Acadian disturbance acanthode Acapulco Bay acceleration accelerator acclimatization accretion by comet accumulation, | 1333 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| ocean ocean basin Oceana, cultures of oceanic flood gravel Oceanic plate subduction oceanogrophy ocher October Odessa Odin Odysseus Odyssey Oedipus Oesel island Oestrus Ogden, | 4416 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| Oceana, cultures of oceanic flood gravel Oceanic plate subduction oceanogrophy ocher October Odessa Odin Odysseus Odyssey Oedipus Oesel island Oestrus Ogden, | 4417 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| from the Earth would cause the oceanic fracturing and rafting of continents, | 11826 COSMIC HERETICS: PART 3: - Chapter 9: NEW FASHIONS IN CATASTROPHISM - |
| elements are not found in expected oceanic and atmospheric abundances for a long time record. | 23554 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : 58 TESTS IN DISPUTE |
| of the ice into the new oceanic basins. | 25385 CHAOS AND CREATION: - - CHAPTER 06: THE URANIANS : THE ICE DUMPS |
| 41 miles thick taken off the oceanic areas would be sufficient," | 26481 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : CONTRIBUTING THEORIES AND ERUPTION DYNAMICS |
| 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 |
| Sea mounts reach up from the oceanic abyss by the tens of thousands. | 26713 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| Zealand became an island surrounded by oceanic deeps. | 26773 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE GLOBAL FRACTURE SYSTEM |
| the Atlantic ridge, and the new oceanic surface was paved by lava flows as the land retreated. | 26811 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : THE TETHYAN WELT |
| distinct continents, the ocean basins, great oceanic ridges; | 26841 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : GLOBAL EXPANSION |
| up greatly the spread of the oceanic depressions. | 26958 CHAOS AND CREATION: - - CHAPTER 07: EARTH PARTURITION AND MOON BIRTH : OCEAN DEVELOPMENT |
| in behavior. Civilizations, now separated by oceanic waters, | 28084 CHAOS AND CREATION: - - CHAPTER 08: SATURN'S CHILDREN : THE "GOLDEN AGE" |
| which threatens the prevailing theory that oceanic waters are regionally stable, | 33581 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 2 The Gaseous Complex - |
| bottom content. Eddies of the great oceanic currents such as the Gulf Stream occasionally break off from these gigantic oceanic flows and set up columnar rings of water that can reach 300 kilometers in diameter, | 33584 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 2 The Gaseous Complex - |
| occasionally break off from these gigantic oceanic flows and set up columnar rings of water that can reach 300 kilometers in diameter, | 33585 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 2 The Gaseous Complex - |
| show a dearth of discharges upon oceanic surfaces 5 . | 35352 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 6 Cosmic and Terrestrial Lightning - |
| north, which contains living species of oceanic type. | 36162 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| the eastern, which disappear into the oceanic abyssal bottom. | 38658 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| now, life seems to reject the oceanic abyss. | 39141 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| and Tanganyika, contain adapted or primordial oceanic animals like the seahorse and jelly fish. | 39307 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| question respecting the origin of the oceanic waters. | 39977 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| and plunged down into the new oceanic chasms, | 40876 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| or crust of the continental and oceanic bottoms? | 41260 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 16 Earthquakes - |
| off the East Asian continent. The oceanic volcanos string along with most of the fracture system. | 41610 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| and about 5 miles below the oceanic bottoms. | 41778 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| 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 - |
| that it was in a warm oceanic current, | 42233 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| over the oldest spot of the oceanic abyss, | 42271 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| Charles Darwin, believed that a single oceanic race had inhabited a great island in the Pacific Ocean which had then been sunk. | 42561 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| characteristic of continental crust, not of oceanic crust, | 42690 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| continent. One may expect to find oceanic basalt or sima beneath Easter Island, | 42697 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| We are inclined to view this oceanic marginal fault system as a possible stretching to accommodate expansion. | 43246 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| mountains as they plough through the oceanic crust. | 43377 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| are flat, save for the steep oceanic ridges, | 43546 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| compresses 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 - |
| 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 - |
| molten material exuding from the great oceanic ridge volcanos, | 43895 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| rate; like today, rarely would the oceanic surfaces be troubled by seabottom volcanism and spreading. | 44006 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| Tethyan waters. Men began navigating the oceanic surfaces now. | 44010 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| and swamps. The length of the oceanic fractures and their transverse fissures (transform faults) amounts to some 300, | 44024 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| in exceptional areas. All of these oceanic sediments come either from cataclysmic off-pourings from the flooded continents, | 44132 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| under quantavolutionary conditions. The character of oceanic sediments varies. | 44138 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| compresses into abundant mountains; but the oceanic crust, | 44165 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| body of land surrounded by an oceanic cleavage. | 44237 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| and Howard Baker had recognized the oceanic rifts and called them recent, | 44415 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| no well-defined boundary of the oceanic expansion to the west, | 44564 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 22 Fractures and Cleavages - |
| that bespeaks turbidity currents, including the oceanic sands and fossils. | 45176 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| the period of 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 - |
| is of varying chemical composition; the oceanic wall is purer basalt of the mantle. | 45210 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| as a pull-back of the oceanic basalt or the continent, | 45212 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| bridged 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 - |
| cells and subduction of continental and oceanic material. | 45222 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| total continental area is antipodal to oceanic area." | 45319 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| much land would be antipodal to oceanic area. | 45325 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the Pacific Basin and the other oceanic basins, | 45343 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| had to account for the counter-oceanic distribution of land, | 45468 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| of the volcanically and seismically active oceanic ridges, | 45583 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 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 the oldest portions of the oceanic rocks ), | 45598 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| rising 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 - |
| of upwelling magma along the great oceanic ridges; | 45633 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| ought perhaps to be full of oceanic sediments, | 45637 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the Glomar Challenger was drilling into oceanic sediments north of Barbados at an apparent plate boundary and discovered older Miocene sediments overlying younger Pliocene deposits. | 45657 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| of an underthrusting (subducting) sediment-loaded oceanic plate. | 45660 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| sediments 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 - |
| is almost totally deductive. If the oceanic plates and basins have been completely renewed every 160 my, | 45734 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the only source of these is oceanic sediments) nor does it appear in any large sedimentary masses distinct from the indigenous continental mass. | 45743 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| that exceptions are considered anomalies. If oceanic plates repeatedly dumped their "young" sedimentary contents at the base of the onshore sedimentary heaps, | 45756 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 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 - |
| under five kilometers thickness. Below the oceanic crust, | 45783 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| In cases where the plate is 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 - |
| low-pressure, hydrated factory produced the oceanic crustal basalts out of upper mantle material. | 45800 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| their "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 - |
| causally with faults, even before the oceanic ridge system was known. | 45829 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| than 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 - |
| the continents as contrasted with the oceanic crust, | 45849 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| suggests the continental rock in the oceanic sediments; | 46185 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| in a thousand years. In the oceanic abyss, | 46639 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| 50-foot winged dinosaur. If the oceanic salt seas carry few analogous niches for today's species, | 46650 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| are rare on the most recent oceanic ridges. | 46674 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| are rare on the most recent oceanic ridges, | 47577 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| the search for the sources of oceanic water, | 49188 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| Isaacs and Schmitt address themselves to oceanic energy sources; | 49513 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| required in order to achieve the oceanic levels that we estimate occurred in the Uranian Lunar periods. | 55534 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| continental shelves. Many seamounts (and present oceanic islands) were exposed and acquired biospheres in time. | 55578 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| recent collection of studies on trans-oceanic contacts summarize the situation for us: | 65939 HOMO SCHIZO I: - - Chapter 5: CULTURAL REVOLUTION : AMERICAN CULTURAL ORIGINS |
| Memphis 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 - |
| may have created various large basaltic oceanic plateaus. ( | 102049 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| Scablands barrier- bursting floods, or giant oceanic tsunamis or Biblical overturning of mountains. | 104913 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 8: THE OBLITERATION OF HUMAN SIGNS - |
| the great rifts of the world, oceanic and terrestrial, | 106444 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| them in their habitat. Or whether oceanic bio-culture might not be accompanied by developments in thermal control, | 110736 THE BURNING OF TROY: PART 5: COMMUNICATING A SCIENTIFIC MODEL: Chapter 27: A COSMIC DEBATE : VI |
| much nickel in clay of the oceanic bed that he inferred that at some time in the past there had been a prodigious fall of meteorites 39 . | 140566 THE VELIKOVSKY AFFAIR: PART 7: ADDITIONAL EXAMPLES OF CORRECT PROGNOSIS - - - |