The Abyss of Time, Changing Conceptions of the Earth's Antiquity After the Sixteenth CenturyFreeman, Cooper, 1980 - 251페이지 |
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... existence about a thousand years before Volterra ; hence 2331 B.C. is a more probable date for the last emergence of the lands . This would leave only about 1,650 years for the interval between the earlier and later floodings , allowing ...
... existence about a thousand years before Volterra ; hence 2331 B.C. is a more probable date for the last emergence of the lands . This would leave only about 1,650 years for the interval between the earlier and later floodings , allowing ...
159 페이지
... the Jura Mountains , and spread over the site of the Alps , which according to Agassiz were not in existence at the onset of glaciation . Then , " as a result of the greatest catastrophe. A Plenitude of Events 159 Zermatt Glacier.
... the Jura Mountains , and spread over the site of the Alps , which according to Agassiz were not in existence at the onset of glaciation . Then , " as a result of the greatest catastrophe. A Plenitude of Events 159 Zermatt Glacier.
170 페이지
... existence inevitably follows from the high rate at which all organic beings tend to increase . . . . Hence , as more individuals are produced than can possibly survive , there must in every case be a strug- gle for existence , either ...
... existence inevitably follows from the high rate at which all organic beings tend to increase . . . . Hence , as more individuals are produced than can possibly survive , there must in every case be a strug- gle for existence , either ...
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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