The Evolution of Earth Structure with a Theory of Geomorphic Changes: By T. Mellard ReadeLongmans, Green, and Company, 1903 - 342 páginas |
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Página ix
... FORCES INVOLVED IN CONTINENTAL OSCILLATIONS . PAGES 1-40 CHAPTER II CONTINENTAL EVOLUTION AND ITS RELATION TO MOUN- TAIN BUILDING 41-46 CHAPTER III CONTINENTAL GROWTH AND GEOLOGICAL PERIODS 47-77 CHAPTER IV OCEANOGRAPHY SUB - OCEANIC ...
... FORCES INVOLVED IN CONTINENTAL OSCILLATIONS . PAGES 1-40 CHAPTER II CONTINENTAL EVOLUTION AND ITS RELATION TO MOUN- TAIN BUILDING 41-46 CHAPTER III CONTINENTAL GROWTH AND GEOLOGICAL PERIODS 47-77 CHAPTER IV OCEANOGRAPHY SUB - OCEANIC ...
Página 12
... force or agency at work in the earth's interior tending to produce such a movement ; but even if there were such an agency , its effect would be limited by the possible deformation the earth could stand and retain . I venture to think ...
... force or agency at work in the earth's interior tending to produce such a movement ; but even if there were such an agency , its effect would be limited by the possible deformation the earth could stand and retain . I venture to think ...
Página 14
... force exists within the earth to prevent the continued effects of this weighting and the natural removal of promi- nences above the sea - level to one uniform plane ? If no such force exists , or has existed , the earth would long have ...
... force exists within the earth to prevent the continued effects of this weighting and the natural removal of promi- nences above the sea - level to one uniform plane ? If no such force exists , or has existed , the earth would long have ...
Página 15
... force ceased . What , as philosophers , we have to find out is the probable nature of this active principle , which may , indeed , be reckoned as the vital force of our planet . That upheavals above the mean level of the spheroid are ...
... force ceased . What , as philosophers , we have to find out is the probable nature of this active principle , which may , indeed , be reckoned as the vital force of our planet . That upheavals above the mean level of the spheroid are ...
Página 22
... forces into play ; indeed it is difficult to see where action and reaction would cease . When we consider that even in minerals that crystallise out in two systems the specific gravities are seldom the same , though the chemical ...
... forces into play ; indeed it is difficult to see where action and reaction would cease . When we consider that even in minerals that crystallise out in two systems the specific gravities are seldom the same , though the chemical ...
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Amazons America anticlinal Atlantic Azores B.Sc basin beds bottom Carboniferous changes CHEMISTRY chlorite clay cleavage Clonakilty coast College compression continental continents County Cork Cretaceous Crown 8vo D.Sc deep deposits depression depth Diagrams differential dome earth's crust ELEMENTARY elevation Engineer evidence exist expansion Experiment fact fathoms feet fissile fold geological geologists Gulf of Mexico heated Illustrations inches islands Israel Russell land areas layers lithosphere mass material matter mica mineral Mississippi Mountain Ranges movements nature North numerous ocean Origin of Mountain photograph Phyllades physical plane Plate Pleistocene portion Professor published by Longmans quarry raised beaches result ridges river rocks Royal 8vo sand sandstones Science Scientific Works published sediment sedimentary shearing sheet shown sink slate slaty-cleavage solid soundings South specific gravity square miles strata strata-plate structure submarine submerged subsidence surface take place temperature terraces Tertiary theory thickness tion valleys vertical volcanic
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