The Abyss of Time, Changing Conceptions of the Earth's Antiquity After the Sixteenth CenturyFreeman, Cooper, 1980 - 251페이지 |
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34 페이지
... strata existed " ( 4 ) . This is an early formulation of the principle of superposition of strata , upon which much of what we think we know concerning the history of the earth and the moon is based . A modern phrasing of this prin ...
... strata existed " ( 4 ) . This is an early formulation of the principle of superposition of strata , upon which much of what we think we know concerning the history of the earth and the moon is based . A modern phrasing of this prin ...
36 페이지
... strata must originally have formed a solid stack filling lowland areas between uplands formed of the harder strata , as shown in his Fig . 22. By application of these same principles , one must envision an original situation , prior to ...
... strata must originally have formed a solid stack filling lowland areas between uplands formed of the harder strata , as shown in his Fig . 22. By application of these same principles , one must envision an original situation , prior to ...
123 페이지
... strata as Floetz or Secondary , and the un- consolidated or weakly consolidated sediments of the lowland areas as Alluvial . Around the beginning of the nineteenth century , European geolo- gists became engaged in a systematic ...
... strata as Floetz or Secondary , and the un- consolidated or weakly consolidated sediments of the lowland areas as Alluvial . Around the beginning of the nineteenth century , European geolo- gists became engaged in a systematic ...
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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