The Abyss of Time, Changing Conceptions of the Earth's Antiquity After the Sixteenth CenturyFreeman, Cooper, 1980 - 251페이지 |
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Claude C. Albritton. head into the solid rock that encloses them . Or in more general terms how has one solid body come to be inside another solid body ? Steno begins his argument by stating what is known , from obser- vation and not ...
Claude C. Albritton. head into the solid rock that encloses them . Or in more general terms how has one solid body come to be inside another solid body ? Steno begins his argument by stating what is known , from obser- vation and not ...
32 페이지
... solids . These principles provide answers to three basic questions . Given a solid body enclosed on all sides by another solid body , which of the two first became hard ? How is the manner of ori- gin of some specific solid body to be ...
... solids . These principles provide answers to three basic questions . Given a solid body enclosed on all sides by another solid body , which of the two first became hard ? How is the manner of ori- gin of some specific solid body to be ...
183 페이지
... solid body . Again using 22 seconds per century as the rate of retardation in spin , he calculated that 7.2 billion years ago the centrifugal force at the equator would have been four times its present amount . If a solid crust were ...
... solid body . Again using 22 seconds per century as the rate of retardation in spin , he calculated that 7.2 billion years ago the centrifugal force at the equator would have been four times its present amount . If a solid crust were ...
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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 evolution father figures fishes Floetz Flood formation fossils geologic time scale 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 origin Paleozoic particles period petrifactions physical plants Playfair present primitive mountains principle published radioactive radiometric radiometric dating rocks 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