The Geological Evidence of ManCosimo, Inc., 2005. 9. 1. - 432페이지 It's impossible to overstate the significance of this classic of scientific literature. A necessary companion to Darwin's The Origin of Species, it springs from the ingenious mind of one of his closest friends, geologist Charles Lyell, whose theories were a critical influence on Darwin's landmark work.First published in 1863, this exploration of the implications of Darwin's "natural selection" for humans remains one of the clearest, most concise explanations of a foundational branch of modern biology. Eminently insightful, the books sings with a scientific poeticism -- chapter sections have such titles as: . "Works of Art in Danish Peat-Mosses." "Curiosity awakened by the systematic Exploration of the Brixham Cave." "Two Species of Elephant and Hippopotamus coexisting with Man in France." "Extinct Mammalia in the Valley of the Oise"Readers in the sciences are sure to find this essential book a highly engaging one as well.Scottish geologist and natural philosopher SIR CHARLES LYELL (1797-1875) was one of the foremost popularizers of science of his time, and the fundamental scientific concepts he developed continue to shape geology and evolutionary biology today. He also wrote the multivolume Principles of Geology: An Attempt to Explain the Former Changes of the Earth's Surface by Reference to Causes Now in Operation. Craters on Mars and the Moon are named in his honor. |
목차
1 | |
7 | |
26 | |
CHAPTER IV | 46 |
CHAPTER V | 58 |
CHAPTER VI | 73 |
CHAPTER VII | 83 |
CHAPTER VIII | 95 |
CHAPTER XIV | 210 |
CHAPTER XVI | 256 |
CHAPTER XVII | 269 |
CHAPTER XVIII | 277 |
CHAPTER XIX | 292 |
CHAPTER XX | 301 |
CHAPTER XXI | 318 |
CHAPTER XXII | 331 |
CHAPTER IX | 118 |
CHAPTER X | 134 |
CHAPTER XI | 152 |
CHAPTER XIII | 181 |
CHAPTER XXIII | 354 |
Whether Man can be regarded as an Exception to the Rule if | 367 |
Notes | 395 |
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Abbeville Acheul alluded alluvial alluvium Alps Amiens ancient animals antiquity Aurignac basin beds boulder clay British bronze cave caverns century Chalk character cliffs coast containing Crag Cyrena Danish Darwin deposits depth drift elephant Elephas antiquus elevation Eocene erratic blocks Europe evidence existence extinct mammalia fauna feet thick flint implements flint tools flora fluviatile formation fossil fragments freshwater genera Geol geological geologists glacial period glaciers Glen Roy gravel hatchets height hippopotamus human bones hyæna islands lake land latitude Liège living species loam loess lower mammalia mammoth marine shells miles Miocene moraines mountains natural Neanderthal North observed occur origin peat plants Pleistocene Pleistocene period Pliocene posterior present Prestwich primigenius Professor quadrupeds race Recent region remains rhinoceros river rocks sand Schmerling seen skeleton skull Somme stone period strata stratified submergence supposed surface Switzerland Tertiary theory valley
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14 페이지 - ... the minimum of time required for the formation of so much peat must, according to the estimate of Steenstrup and other good authorities, have amounted to at least 4,000 years; and there is nothing in the observed rate of the growth of peat opposed to the conclusion that the number of centuries may not have been four times as great, even though the signs of man's existence have not yet been traced down to the lowest or amorphous stratum. As to the 'shell-mounds...