The Abyss of Time, Changing Conceptions of the Earth's Antiquity After the Sixteenth CenturyFreeman, Cooper, 1980 - 251페이지 |
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... continents are inactive or nearly so . At this juncture , sea level had stabilized at about its present posi- tion . The continents had emerged from the universal ocean , plas- tered with marine sediments molded into mountains and ...
... continents are inactive or nearly so . At this juncture , sea level had stabilized at about its present posi- tion . The continents had emerged from the universal ocean , plas- tered with marine sediments molded into mountains and ...
95 페이지
... continents , he reminds us , are formed from the waste of older continents . The present lands themselves are eroding away , and the sediments shed from them are being stored on the ocean floor as the foundations of continents that will ...
... continents , he reminds us , are formed from the waste of older continents . The present lands themselves are eroding away , and the sediments shed from them are being stored on the ocean floor as the foundations of continents that will ...
221 페이지
Claude C. Albritton. present continents away from the original continent . Slow - moving convection currents in the subcrustal region are commonly thought to be the agents that raft the plates about . Whatever the mechanism , the idea of ...
Claude C. Albritton. present continents away from the original continent . Slow - moving convection currents in the subcrustal region are commonly thought to be the agents that raft the plates about . Whatever the mechanism , the idea of ...
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Adam Sedgwick Agassiz animals appeared Arthur Holmes began beginning bodies bottom Buffon Burnet calculations Cambrian Carboniferous Carozzi catastrophists causes Cenozoic century changes CHAPTER continents cooling Cuvier Darwin deposits earth earth's crust energy erosion essay estimates evidence father figures fishes Floetz Flood formation fossiliferous fossils Geological Society geologists glaciation glaciers heat Holmes Hooke Hooke's Hutton idea Jura Mountains Kelvin kinds land later layers lectures living Lyell Maillet marine mathematics million minerals molten Murchison natural history neptunist ocean Ordovician organisms original Paleozoic particles period petrifactions physical plants Playfair present primitive mountains principle published radioactive radiometric radiometric dating rocks Royal Society Sacred Theory Scrope sea level Sedgwick sediment sedimentary shells Siccar Point Silurian Smith solid species Steno strata stratigraphic stratum studies substances succession superposition surface Telliamed temperature thickness Thomson tion tonguestones Triassic uniformitarians University volcanic Werner William