| |
|
SEDIMENTATION.............41 (0.005%)
|
| quantification quantity quantum quantum relativity quantum sedimentation quantum-mechanics, | 4891 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| secret word secularism sediment sedimentary meteorite sedimentation sedition science seed seismic discontinuity seismic sea wave seismism seismology Selene self awareness self control self destructiveness self fulfillment self-rule Selimiye Selye, | 5220 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| THREE: Collapsing Tests of Time Rapid Sedimentation Coral Reefs Radiodating Radiation Turbulence Potassium-Argon Dating The Radio-Halo Problem Radiocarbon (Carbon-14) Dating Tree-Ring Time Magnetism The Fossil Record and Mutating Time Cycles and Anniversaries 58 Tests in Dispute The Dissolution of Time Of Mammonths and Amber Schaeffer and Velikovsky CHAPTER FOUR: | 21239 CHAOS AND CREATION: - - - TABLE OF CONTENTS - |
| meets the eye of water erosion, sedimentation, | 21834 CHAOS AND CREATION: - - CHAPTER 01: COSMIC INSTABILITY : THE CLEAVAGE OF MARS: A PARTICULAR CASE |
| pursue time enough on Earth for sedimentation, | 21878 CHAOS AND CREATION: - - CHAPTER 01: COSMIC INSTABILITY : "ONE OR TWO CENTURIES" OF "ETERNAL ORDER" |
| be explained in Chapter 7. RAPID SEDIMENTATION Rates of sedimentation are usually estimated on the basis of contemporary rates. | 22776 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| Chapter 7. RAPID SEDIMENTATION Rates of sedimentation are usually estimated on the basis of contemporary rates. | 22778 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| be of holocene age 7 . Ocean sedimentation recently examined under conventional premises (with the "help" of potassium-argon techniques), | 22784 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| intervals between layers... Observed rated of sedimentation range from almost immeasureably small fractions of an inch per century to many feet per hour and make it almost impossible to estimate the average for my large deposit..." | 22842 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| In the case of several areas - sedimentation, | 23634 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : 58 TESTS IN DISPUTE |
| heavier silicate magnesium mixtures (sima). Great sedimentation had occurred. | 24830 CHAOS AND CREATION: - - CHAPTER 05: SOLARIA BINARIA : THE WORLD OF PANGEA |
| material from volcanic material in the sedimentation of the Earth is a large task that chemical geology is now assuming. | 25330 CHAOS AND CREATION: - - CHAPTER 06: THE URANIANS : THE DESTRUCTION OF PANGEA |
| their surroundings. Biological assemblages follow suit. Sedimentation rates are also a function of current velocity. | 33588 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 2 The Gaseous Complex - |
| are only occasionally found in it. Sedimentation from lakes and rivers seems to be an impossible explanation. | 33986 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| Magnetic reversals may be concealed because sedimentation is too slow to capture its duration, | 34342 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| a piping system for magma flow. Sedimentation on them is slight. | 43573 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| these areas where the abyss begins, sedimentation is thicker and can reach 1000 meters in exceptional areas. | 44129 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| ocean. The time required for such sedimentation is calculable in a couple of thousand years or less under quantavolutionary conditions. | 44135 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| Wind and water bring in the sedimentation layers. | 45014 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| bottoms, too much for long-term sedimentation to have occurred. | 46183 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| place is a long record of sedimentation with occasional gaps... | 46234 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| long gap with only very occasional sedimentation... | 46236 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| called the "onion skin theory" of sedimentation is untenable, | 46295 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| by many. The essential principle of sedimentation should probably be called "quantavolution." | 46296 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| now well understand. Specifically applied to sedimentation, | 46298 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| for even very special kinds of sedimentation and rocks to form. | 46327 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| numerous wide differences in rates of sedimentation: | 46336 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| he calls "the phenomenon of quantum sedimentation." | 46342 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| out? Or another case of rapid sedimentation? | 46350 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| sediment, including the famous Scandinavian varves. "Sedimentation goes on all the time, | 46387 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| one long gap with only occasional sedimentation." | 46414 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| of subsidence. "It is only when sedimentation and subsidence coincide that the conditions will be right for the preservation of the vast thicknesses that constitute the stratigraphic record." | 46426 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| of heavy deep volcanism and slow sedimentation. | 47696 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| A type of non-fossiliferous deep sedimentation discoverable over an area of 100 km diameter." | 49180 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| steep stairs of the canyon, no sedimentation, | 57026 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 16: VENUS AND MARS - |
| caves and rock shelters. Estimates of sedimentation rates of deposits into which artifacts were sandwiched, | 62060 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : TIME UNNEEDED FOR CULTURE |
| A. D. Repeated devastations and heavy sedimentation and sinkings have obliterated practically all traces of their villages and gardens, | 65617 HOMO SCHIZO I: - - Chapter 5: CULTURAL REVOLUTION : MAJOR DEVELOPMENTS EVERYWHERE CONTEMPORARY |
| both marine and terrestrial, with confused sedimentation (Nature) 19. | 102020 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| clays? Clay is conventionally assigned to sedimentation or decomposed structural material, | 102920 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 2: THE BURNING OF TROY : A NEW INTERDISCIPLINARY METHOD |
| think in terms of extremely gradual sedimentation as creating the scene. | 106484 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| encasement, unless the long period of "sedimentation" were in fact the ash fall of a single day. " | 106494 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| |
|
SEDIMENTATIONS............1 (0.000%)
|
| from heaven" images as explanations of sedimentations, | 46399 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| |
|
SEDIMENTED................4 (0.000%)
|
| For the ocean bottoms are scarcely sedimented 4 . | 22743 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| shelves. The ocean basins are scarcely sedimented; | 44121 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| basins are young, thin, and scarcely sedimented. | 44319 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| s, that the trenches are scarcely sedimented.) " | 45699 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| |
|
SEDIMENTOLOGICAL..........1 (0.000%)
|
| always composed of herbivores? Are their sedimentological characteristics different from other bone layers? | 46880 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| |
|
SEDIMENTOLOGY.............1 (0.000%)
|
| and pervasive uniformitarian influence exists in sedimentology as in paleontology, | 46913 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| |
|
SEDIMENTS.................167 (0.021%)
|
| flood plain flood, catastrophic Florida Florida sediments flow of material fluvial pattern fluvial process flux flywheel Foehn wind fold morphology Folgheraiter, | 2888 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| boom Soos Springs, Czechoslovakia soot in sediments Sophist Sorenson, | 5375 QUANTAVOLUTION AND CATASTROPHE: PART 5: The Scope of Quantavolution - - - |
| up many thousands of feet. These sediments left behind them the basic shield rock 10 . | 22250 CHAOS AND CREATION: - - CHAPTER 02: HIGH ENERGY FROM SPACE : SEISMISM AND VOLCANISM |
| feet or 80 miles thick of sediments 3 . | 22741 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| Or perhaps someone has been burning sediments to make granites for the sial. | 22746 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| 40 of the globe and the sediments lay on the average only 4 miles thick upon the 20 mile thick sial, | 22757 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| per cent of the Earth's sediments have disappeared. | 22759 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| become 4. Then 96 of the sediments are missing. | 22764 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| land robbery. Half of the stolen sediments were never there. | 22767 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| created. The other half of the sediments was stolen by "Uranus Minor" and stashed away on the Moon: | 22769 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME - |
| than by former calculations 8 . The sediments were found to be astonishingly meager. | 22786 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| to this new dating, the ocean sediments could be provided readily from catastrophic sources in a thousand years after the basins formed, | 22787 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| under enormous pressure, contains only unconsolidated sediments, | 22790 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| the oceans, the oceans and their sediments have accumulated a supply representing less than 100, | 22794 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| ocean becomes holocene 10 . For most sediments would have been dropped or transported in the earliest years. | 22796 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| layer, he says "For the common sediments... | 22829 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| Again I quote Shelton: "Unfortunately most sediments do not contain reliable clues to how fast they were deposited --- or to the duration of intervals between layers... | 22840 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : RAPID SEDIMENTATION |
| to quantavolutional geologists, uniquely related to sediments, | 22854 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : CORAL REEFS |
| melted metamorphic rock, can be tested. Sediments cannot. | 23076 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : POTASSIUM-ARGON DATING |
| processes that devastate the atmosphere, build sediments and transport life forms quickly. | 23412 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : THE FOSSIL RECORD AND MUTATING TIME |
| have, since the sial and its sediments are lighter than the sima of the ocean floor. | 24836 CHAOS AND CREATION: - - CHAPTER 05: SOLARIA BINARIA : THE WORLD OF PANGEA |
| by the masking effect of younger sediments and metamorphism of older terranes." | 25351 CHAOS AND CREATION: - - CHAPTER 06: THE URANIANS : THE DESTRUCTION OF PANGEA |
| Aromatic Hydrocarbons in Soils and Recent Sediments," | 31225 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| Billy (1967), "Microtektites in Deep-sea Sediments," | 31593 CHAOS AND CREATION: - - - BIBLIOGRAPHY - |
| 24.Continental Tropism and Rafting 25.Sediments PART VI: | 32676 THE LATELY TORTURED EARTH: - - - TABLE OF CONTENTS - |
| evidence, especially by chemical examination of sediments, | 32827 THE LATELY TORTURED EARTH: - - CHAPTER 1: Quantavolutions - |
| up two thousand square kilometers of sediments and breaking down surface features, | 33748 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| once all around the world, many sediments would be displaced, | 33769 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| multiple meteoroidal instrusions. Finally, if the sediments of the world do not reflect adequately cyclonic effects, | 34032 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| and contamination affect samples, when the sediments are dumped or shifted, | 34344 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 4 Magnetism and Axial Tilts - |
| entirely of basaltic lava. Ocean abyssal sediments are thin and loose, | 35896 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| geo-chemists. Soils and young marine sediments of northeastern and offshore America reveal, | 35948 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| seems to have been covered with sediments immediately after its formation," | 35968 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| were mixed through a column of sediments several times the thickness of the original ash bed. | 36012 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| contained some oxygen" and that the sediments "probably represent no more than 100, | 36052 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| Aromatic Hydracarbons in Soils and Recent Sediments," | 36343 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash : Notes (Chapter Seven: Fire and Ash) |
| atmosphere. They are found in recent sediments and on the surface. | 36706 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| in time, we should have the sediments of the ocean receive their quota of nickel laid down in a few thousand years. | 36814 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone - |
| Singer, "Zodiacal Dust and Deep Sea Sediments," | 36996 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 8 Falling Dust and Stone : Notes (Chapter Eight: Falling Dust and Stone) |
| Aromatic Hydrocarbons is Soils and Recent Sediments," | 37515 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 9 Gases, Poisons and Foods - |
| for the PAH are in surficial sediments. | 37543 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 9 Gases, Poisons and Foods - |
| of men. Cores drilled from Antarctic sediments of pleistocene age contained iridium and gold in anomalously high proportions. " | 37837 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| ice from collapsing ice caps, and sediments pushed by these, | 38045 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| waters were squeezed out of insoluble sediments into their own cavity. | 38047 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| and laid in even layers of sediments rather than in intrusive pockets is unanswered. | 38060 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| Gulf of California are producing from sediments a petroleum that is close to commercial standards. | 38134 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| as to insure deep burial of sediments all along the coast and shelf of the Gulf of Mexico. | 38222 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| geochemistry... The fossil prophyrins of ancient sediments and of petroleum are chemical fossils; | 38350 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| in living organisms nor in recent sediments... | 38366 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| recent sediments... Also crude oil and sediments contain polymers (asphaltenos, | 38366 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| plain be the crater debris and sediments and let the Atlantic cleavage be abetted by the Bermuda impact. | 38640 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| of fossil craters, contained in stratified sediments, | 38874 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| myth hold that the most ancient sediments must rest on the ocean floors, | 39134 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| age of the water is lacking. Sediments are thin, | 39150 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| the rock that underlies the continental sediments, | 39181 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| object that lakes become filled with sediments must imply that such fossil lakes should exist by tens of thousands in the stratified rocks of the world. | 39326 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| that had been trapped in shelf sediments when the Pleistocene ice ages lowered the ocean waters, | 39361 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| Surely so; however, not only chalk sediments but also ice layers could be deposited in a short time if the wobblings of the axis were greater and more frequent, | 40938 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 15 Ice Fields of the Earth - |
| of the oceanic abyss, erasing its sediments and boiling it. | 42272 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| melting of piles of pre-existing sediments. | 42786 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| It is thus that the marine sediments occur in all regions. | 42794 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| meters higher than others. Shallow marine sediments would be raised. | 42807 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| marine sediments would be raised. Many sediments would be reworked in the heat, | 42808 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| would develop. The superpositioning of fossilized sediments according to age would be preserved, | 42814 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| 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 - |
| scraped of its biosphere and surficial sediments, | 43160 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| the discontinuity and absence of expected sediments in so many places is the underlying expansion by igneous intrusions that once occurred. | 43163 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| may add: "How can kilometer-high sediments be pushed over thousands of kilometers of the surface of the Earth?" | 43355 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| ice bulldozes the surfaces of all sediments and biosphere in many areas; | 43374 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| which are largely built from folded sediments. | 43549 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| undersea mountains have a covering of sediments in many places, | 43552 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| places, they are not made of sediments, | 43553 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| for the superficial Cambrian and 'younger' sediments over the continuous, | 43659 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| interpreted as crustal rocks denuded of sediments by thrusts of their original sediments from beneath the ice caps driven by the hydrostatic pressure and the friction of the ice flow" (quoting Cook). " | 43664 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| sediments by thrusts of their original sediments from beneath the ice caps driven by the hydrostatic pressure and the friction of the ice flow" (quoting Cook). " | 43664 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| rifts, canyons and channels; and the sediments, | 43718 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| that a gradual off-flow of sediments has created the sloping figure. | 44058 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| thick or less. The thickest ocean sediments are not on 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 - |
| 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 - |
| quantavolutionary conditions. The character of oceanic sediments varies. | 44138 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| course produced gaps in dating of sediments by fossils of many millions of years, | 44251 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the fossil record are common. With sediments so thin, | 44256 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| steadily to perform most transport of sediments, | 44875 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| carving banks and valleys, and depositing sediments, | 44877 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| and lava. Thereupon the miles of sediments begin to pile up, | 45010 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| the region. The three miles of sediments, | 45042 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| sand and mud. Speaking of the sediments of hundreds of feet, " | 45044 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| years. They have not filled with sediments. | 45167 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| against which it is emplaced. Its sediments are shallow, | 45197 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| foundation of the island arc." 11 Sediments of the trenches are scanty. | 45217 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 23 Canyons and Channels - |
| the ocean bottoms have deposited their sediments periodically beneath the sea shores of continents, | 45302 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the last 160 million years of sediments. | 45304 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| yesterday's action. They have scanty sediments, | 45636 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| perhaps to be full of oceanic sediments, | 45637 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 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 - |
| plate boundary and discovered older Miocene sediments overlying younger Pliocene deposits. | 45658 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| the plate went down its older sediments were sheared off and ended up overlying its younger sediments. | 45661 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| and ended up overlying its younger sediments. | 45662 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| trenches are scarcely sedimented.) "As the sediments get caught between the subducting oceanic crust and either the island arc or the continental crust they are subjected to strong deformation, | 45699 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| heating and metamorphism... Some of the sediments may even be dragged to great depths, | 45702 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| enhance the text by showing some sediments being scraped off on the opposite side and other sediment being miscilated and conveyed below. | 45706 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| whole of a previous world of sediments should be dumped in such heaps or carried down into a mantle reluctant, | 45711 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| of course, no such masses. The sediments by the trenches, | 45714 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| The balance of new and old sediments, | 45718 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| have scraped off some of their sediments upon each other. | 45736 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| as islands around the globe. Such sediments scarcely exist. | 45738 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| they are unrecognizable as such. The sediments of the oceans are less than a kilometer deep on the average. | 45739 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| 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 - |
| 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 - |
| this time, picking up and delivering sediments. | 45752 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| subduction and perpetual plate renewal. Marine sediments are the majority of all organic facies; | 45760 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| built up of primordial granites and sediments or of trench debris folds, | 45791 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| Alfred de Grazia CHAPTER TWENTY-FIVE SEDIMENTS We have entertained the possibility that till might have originated from the tail of a comet or cyclonically (tempestites). | 46129 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| As with till, so with all sediments: | 46151 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| 10 or less of deep ocean sediments. | 46153 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| all crustal rock is composed of sediments that remain in something approaching their state after deposition. | 46159 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| the globe at over two kilometers. Sediments have been classified by priority of deposition and anywhere from ten to hundreds of major and minor strata have been allocated positions, | 46162 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| of limestone. The old problem of sediments missing from the geological column became more worrisome with the discovery that the ocean bottoms do not carry their proportionate burden of sediments, | 46169 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| not carry their proportionate burden of sediments, | 46171 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| are confined largely to occasional polar sediments. | 46182 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| common in the shelf and ooze sediments. | 46185 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| the continental rock in the oceanic sediments; | 46185 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| ten miles is composed of melted sediments, | 46189 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| the location of the granites or sediments suggest that granitization has consumed sediments. | 46191 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| sediments suggest that granitization has consumed sediments. | 46192 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| is found below, and intrusively, among sediments, | 46193 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| special electrical or thermal force. Old sediments do not appear to be far less common than new sediments, | 46196 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| be far less common than new sediments, | 46196 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| the Earth. It lay under such sediments as have formed out of largely 'cool' fall-out and heavy erosion. | 46212 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| disarrangement and, indeed, chaos of the sediments. | 46227 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| only of a Pangea in which sediments and life forms might readily become worldwide but also, | 46324 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| they do not form on mountains, sediments, | 46332 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| Lancaster; but for the flow of sediments from rivers into the seas he quotes Holmes' measure of only one centimeter per millennium. | 46338 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| argues convincingly the origin of deep sediments. | 46425 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| of deep sediments. The production of sediments is independent of subsidence. " | 46425 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| his facts. Notes (Chapter Twenty-five: Sediments) 1. " | 46503 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments : Notes (Chapter Twenty-five: Sediments) |
| levels of many marine and terrestrial sediments. | 46736 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| when finally buried deeper by later sediments of the river valley they would be preserved as they are seen here, | 46833 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| paleontology, with, in the interpretation of sediments, | 46913 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| based upon material dredged from marine sediments, | 47001 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| not completely decomposed?" To what degree sediments are "rock fossil assemblages" is unknown. | 47035 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| area a second layer of fossilized sediments, | 47101 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| worms can be traced in the sediments, | 47316 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| artifacts lay also upon the fossil sediments. | 47749 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| of 1000 kilometers diameter from which sediments of the same age are patchy, | 49117 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| assembled heavy biotic dissemination in contemporaneous sediments taking the form of fusain and calcination and extending over an area of 500 km diameter." | 49140 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| or more fossil conglomerates of similar sediments anywhere in the world exhibiting 2 times the normal background radiation of modern age bones." | 49176 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| pattern of pollen deposits in lake sediments moving at the rate of a mile a year 10 . | 49482 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| each other out. Since the ocean sediments average one kilometer, | 49668 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| will reach the average depth of sediments in about 1350 years, | 49670 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| and the dating of its associated sediments. | 49820 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| sedimentary rock requires admitting that the sediments can never have been very deep, | 53159 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 8: THE EARTH'S PHYSICAL AND MAGNETIC HISTORY - |
| that a considerable fraction of earthy sediments (what amounts to about 3 x 10 18 tons) are estimated to be meteoritic in origin (Niemann). | 54716 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| plenum its present volume, less its sediments, | 54724 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| its sediments, in a millennium; its sediments could have been laid down in some generations of late binary times by extraterrestrial and turbulent surface events. | 54724 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| local thrusts and folds of the sediments. | 54746 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| we have shown, cause magnetically confused sediments to be laid down, | 55218 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 12: QUANTAVOLUTION OF THE BIOSPHERE: HOMO SAPIENS : Notes on Chapter 12 |
| Aromatic Hydrocarbons in Soils and Recent Sediments," | 59220 SOLARIA-BINARIA: - - - BIBILIOGRAPHY - |
| 1967), "Zodiacal Dust and Deep Sea Sediments," | 60084 SOLARIA-BINARIA: - - - BIBILIOGRAPHY - |
| tuff, clay, marl, Bonneville-like type 'sediments' and scanty soilroot elements, | 62177 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : OLDUVAI GORGE |
| 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 - |
| Aromatic Hydrocarbons in Soils and Recent Sediments," | 103192 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 2: THE BURNING OF TROY : Notes (Chapter 2: The Burning of Troy) |
| any event would slowly fill with sediments and broaden. | 106089 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 12: A FAILED EXCURSION TO THE CAVES OF AQUITAINE - |
| rock layers are laid down (or sediments) the argon in the atmosphere is escaping and therefore less and less proportionally absorbed, | 106402 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| thereby exposing the great series of sediments seen today." | 106477 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| petroleum is never found in recent sediments (J. | 140456 THE VELIKOVSKY AFFAIR: PART 7: ADDITIONAL EXAMPLES OF CORRECT PROGNOSIS - - - |
| evidenced by the shift of marine sediments (1955) 50 . | 140604 THE VELIKOVSKY AFFAIR: PART 7: ADDITIONAL EXAMPLES OF CORRECT PROGNOSIS - - - |