| |
|
METEREOLOGISTS............1 (0.000%)
|
| in "hard" lightning, taken over by metereologists now, | 34893 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 5 Electricity - |
| |
|
METEROID..................1 (0.000%)
|
| R. D. Associates, New Scientist). 28. Meteroid impacts (5 to 10 km diam.) | 102049 THE BURNING OF TROY: - - Chapter 1: THE QUANTAVOLUTIONARY SCAN - |
| |
|
METEROLOGICAL.............1 (0.000%)
|
| 8000 to B. C. (London: Royal Meterological Soc., | 33644 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 2 The Gaseous Complex : Notes (Chapter Two: The Gaseous Complex) |
| |
|
METERS....................93 (0.012%)
|
| large spare frame a full two meters, | 6644 COSMIC HERETICS: PART 1: - Chapter 2: THE PRODIGAL ARCHIVE - |
| at an apartment only a few meters away from the Jewish Synagogue and college where Hyam Maccoby works, | 9713 COSMIC HERETICS: PART 2: - Chapter 6: HOLOCAUST AND AMNESIA - |
| supposed to have been over 100 meters lower 20, | 22881 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : CORAL REEFS |
| can be from 1 to 12 meters per thousand years. | 22885 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : CORAL REEFS |
| or at depths of hundreds of meters elsewhere may have originated in the swamps and shallow seas of Pangea, | 22891 CHAOS AND CREATION: - - CHAPTER 03: COLLAPSING TESTS OF TIME : CORAL REEFS |
| depth is mostly less than 100 meters, | 29536 CHAOS AND CREATION: - - CHAPTER 10: VENUS AND MARS : GLOBAL RUINATION AND ITS PERPETRATOR |
| wind velocities of 10 to 100 meters per second are comparable to those of the jet stream that races through the upper atmosphere of the Earth 17 . | 33913 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| passed above him by a few meters. | 33938 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| passing through the Chinese countryside thirty meters below the houses and farms on the loess above. | 33980 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 3 Hurricanes and Cyclones - |
| thinnest film up to a few meters in which life forms take hold or dwell. | 35934 THE LATELY TORTURED EARTH: PART I: ATMOSPHERICS: Chapter 7 Fire and Ash - |
| below its path by hundreds of meters. | 37186 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 9 Gases, Poisons and Foods - |
| a depth of only 1.5 meters. | 37722 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| Earth to depths of a thousand meters and more. | 38063 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| oil slick of one to ten meters' depth all over the globe 26 . | 38139 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 10 Metals, Salt and Oil - |
| and great mountains are about 80 meters per million years, | 38768 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| land masses in tropical regions 225 meters per million years. | 38769 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| Circular ridges of less than 750 meters relief could be broken down in 5 million years, | 38769 THE LATELY TORTURED EARTH: PART II: EXOTERRESTRIAL DROPS: Chapter 11 Encounter and Collisions - |
| water depths of less than 300 meters and penetrated to depths of from 20 to 300 meters, | 39354 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| depths of from 20 to 300 meters, | 39355 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 12 Water - |
| explosions have raised waves of 85 meters, | 40193 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| which has buried 11 or 12 meters depth of occupation levels under the present flood plain." | 40332 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| been strewn in a level six meters below ground, | 40364 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| of species." Tortoises of over six meters, | 40377 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| have picked up bones hundreds of meters below ground. | 40474 THE LATELY TORTURED EARTH: PART III: HYDROLOGY: Chapter 14 Floods and Tides - |
| deep valley. It ascended, achieving 250 meters, | 41708 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| and the layering of ca 2 meters of alluvion talus atop the pumice bed. | 41711 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| and the algae Melobesia, at 3000 meters, | 41907 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 17 Volcanism - |
| Central Asia rose another 2,000 meters. | 42085 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| dredges or pierced by the few meters of core drills, | 42148 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| islands and Italy were found 3000 meters below sea level in the central Tyrrhenian Sea, | 42158 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| been lifted hundreds or thousands of meters higher than others. | 42807 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 18 Sinking and Rising Lands - |
| This would amount to 10 6 meters in a billion years, | 43061 THE LATELY TORTURED EARTH: PART IV: CRUSTAL TURBULENCE: Chapter 19 Expansion and Contraction - |
| mountain uplifts amounting to thousands of meters have occurred, | 43472 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| Could sea levels have been 400 meters and more lower than today, | 43575 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 20 Thrusting and Orogeny - |
| differences in depth; the upper 170 meters is normally magnetized, | 43901 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| is normally magnetized, the next 310 meters is reversed: | 43902 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| is reversed: and the following 40 meters is again normal 3 . | 43902 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| is continental shelf, less than 300 meters below sea level. | 43932 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| abyssal plains with depths from 2700 meters to 5000 meters. | 43933 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| depths from 2700 meters to 5000 meters. | 43933 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| plains. Sheer cliffs of over 2000 meters are the rule. | 43944 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| the circumglobal ridges. They are 20 meters thick or less. | 44127 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| is thicker and can reach 1000 meters in exceptional areas. | 44130 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 21 Ocean Basins - |
| project 30,000 or 40,000 meters into the 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 - |
| 00015 kilometer or 1.5 cubic meters of the Earth's surface per year. | 45612 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| submersible, DVS Turtle, at around 1600 meters of depth. | 45640 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 24 Continental Tropism and Rafting - |
| water cut many channels of many meters of depth through hundreds of kilometers of basalt plains, | 46217 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| depth of up to 20,000 meters, | 46333 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| at Flims, Switzerland; 40 million cubic meters of mountains fell into Lituya Bay, | 46418 THE LATELY TORTURED EARTH: PART V: RIFTS, RAFTS AND BASINS: Chapter 25 Sediments - |
| to a thickness of 2,000 meters, | 47026 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| not unusual that they are 10 meters thick, | 47030 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 26 Fossil Deposits - |
| Hollister 19 . At 1000 to 4000 meters of depth, | 47577 THE LATELY TORTURED EARTH: PART VI: BIOSPHERICS: Chapter 27 Genesis and Extinction - |
| may propose "Tidal waves attaining 100 meters in amplitude at 10 land points not less than 400 kilometers apart. | 49204 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| be "An absolute rise of 300 meters over an area of 100 km diameter." | 49226 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 30 Intensity, Scope and Suddenness - |
| amount to a column of 730 meters in 1000 years, | 49667 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| a single core drilled at 4805 meters of ocean depth off Africa into a fan of a submarine canyon cut into the Walvis Ridge; | 49829 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| the Walvis Ridge; at about 205 meters below the bottom the C T boundary was ascertained and its materials analyzed. | 49830 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| fossils above the boundary for two meters led to an unresolved question as to whether bioturbation or a prolonged extinction process was proceeding after the extincting event. | 49839 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| below which it alternates to 340 meters with volcanoclastics, | 49844 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| of ash is found at -200 meters just above the C T boundary transition and another at -60 meters. | 49847 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| boundary transition and another at -60 meters. | 49848 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| If, for instance, in the 280 meters of postbasalt deposits, | 49852 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| meters of postbasalt deposits, some 7 meters consist of ashes, | 49853 THE LATELY TORTURED EARTH: PART VII: DIMENSIONS OF QUANTAVOLUTION: Chapter 31 The Recency of the Surface - |
| METRIC UNITS Distances are measured in meters Multiples of the meter, | 50808 SOLARIA-BINARIA: - - - TABLE OF CONTENTS - |
| megajoules of energy within a few meters of surviving observers. | 51540 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 3: THE SUN'S GALACTIC JOURNEY AND ABSOLUTE TIME - |
| is said to be 10 26 meters in radius; | 51913 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 3: THE SUN'S GALACTIC JOURNEY AND ABSOLUTE TIME : Notes on Chapter 3 |
| has a radius of 10 -10 meters. | 51914 SOLARIA-BINARIA: PART 1: ORIGIN AND DEVELOPMENT OF THE BINARY SYSTEM: Chapter 3: THE SUN'S GALACTIC JOURNEY AND ABSOLUTE TIME : Notes on Chapter 3 |
| rainfall of two-and-a-half meters (not uncommon in coastal areas today) would dump over one million cubic kilometers of water onto the Earth's surface. | 54748 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| present oceans. Cherrapunji (India) receives 11 meters of rain in 159 days, | 54751 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| mean daily intensity) would yield 26 meters of rainfall annually. | 54752 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 11: ASTROBLEMES OF THE EARTH - |
| an annual rainfall of 1.2 meters depth would have descended upon the Earth's surface, | 55536 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| new paved basins located five thousand meters below the surviving land masses. | 55593 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 13: NOVA OF SUPER URANUS AND EJECTION OF THE MOON - |
| per square kilometer- second, 1.5 meters of rain each hour. | 56128 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 14: THE GOLDEN AGE AND NOVA OF SUPER SATURN - |
| 500 km. wide, and 6,100 meters deep, | 57012 SOLARIA-BINARIA: PART 2: DESTRUCTION OF THE SOLAR BINARY: Chapter 16: VENUS AND MARS - |
| METRIC UNITS Distances are measured in meters Multiples of the meter, | 58461 SOLARIA-BINARIA: - - - LIST OF ABBREVIATIONS IN TEXT - |
| bones in the thousands of cubic meters of debris examined. | 61782 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : PEKING MAN |
| turtles, with diameters around 1.5 meters, | 61874 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : AMEGHINO'S ARGENTINE HOMINIDS |
| were found throughout the whole fifty meters' depth of a filled fissure of breccia, | 62302 HOMO SCHIZO I: - - Chapter 2: HOMINIDS IN HOLOGENESIS : CHARDIN'S ORTHOGENETICS |
| highest in mammals. It is 25 meters per second at 20 deg C in myelinated (sheathed) frog nerves to 100 meters in mammals. | 71973 HOMO SCHIZO II: - - Chapter 3: BRAINWORK : THE LOCATION OF INSTINCT DELAY |
| myelinated (sheathed) frog nerves to 100 meters in mammals. | 71974 HOMO SCHIZO II: - - Chapter 3: BRAINWORK : THE LOCATION OF INSTINCT DELAY |
| of burden or one wagon, three meters apart, | 92061 GODS FIRE: - - Chapter 7: THE LEVITES AND THE REVOLTS : NUMBERS LEAVING EGYPT |
| line of nine hundred toises (1754 meters), | 92779 GODS FIRE: - - Chapter 7: THE LEVITES AND THE REVOLTS : KORAH'S REBELLION |
| of debris "from 7 to 10 meters, | 102319 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 2: THE BURNING OF TROY : THE "BURNT CITY" OF TROY |
| of clay more than 0.50 meters thick, | 102690 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 2: THE BURNING OF TROY : THE "BURNT CITY" OF TROY |
| subsoil to a depth of 20 meters in 228 locations for the purpose of planning subway construction. | 102890 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 2: THE BURNING OF TROY : A NEW INTERDISCIPLINARY METHOD |
| distance of all 24 stadi (4440 meters) and comes upon a herd of pigs on a hill. | 103480 THE BURNING OF TROY: PART 1: HISTORICAL DISTURBANCES: Chapter 3: THE FOUNDING OF ROME - |
| at depths between 1300 and 1700 meters. | 105373 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 11: ICE CORES OF GREENLAND - |
| accumulation conditions" 12 . The 800 top meters of the Camp Century core count off 4000 years with uniform temperatures. | 105502 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 11: ICE CORES OF GREENLAND - |
| The Greenland core ends in many meters of debris, | 105523 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 11: ICE CORES OF GREENLAND - |
| out. In the Antarctic, the lowest meters constitute a shallow lake, | 105526 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 11: ICE CORES OF GREENLAND - |
| of peat in Ireland. Over 10 meters of peat formed in the Holocene and is found below the river valley of Eau Claire. | 106033 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 12: A FAILED EXCURSION TO THE CAVES OF AQUITAINE - |
| found on Floor I and 4 meters away with "a worked bone tool." | 106489 THE BURNING OF TROY: PART 2: GEOLOGICAL ISSUES: Chapter 13: THE LATECOMING OLDUVAI GORGE - |
| Office space of 5 x 10 meters for individual conferences, | 111677 THE BURNING OF TROY: PART 5: COMMUNICATING A SCIENTIFIC MODEL: Chapter 29: I.Q.: A UNIVERSITY PROGRAM : SUPPORT OF IQ |