The Atlantic Monthly, Volume 10, No. 62, December, 1862 by Various
page 53 of 280 (18%)
page 53 of 280 (18%)
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and depositing in the course of ages the regular layers of gravel, sand,
and marl, which now cover so large a part of Europe. This was still further followed by a period in which the temperature of the earth was lowered, and ice and glaciers had perhaps a part in forming the present surface of the northern hemisphere. During the first period, which may be called the "Quaternary Period,"[B] the mighty animals lived whose bones are now found in caverns, or under the slowly deposited sediment of the waters, or preserved in bog,--the mammoth, and rhinoceros, and elk, and bear, and elephant, as well as many others of extinct species. [Footnote B: We should bear in mind that the Quaternary or Diluvian Period, however ancient in point of time, has no clearly distinguishing line of separation from the present period. The great difference lies in the extinction of certain species of animals, which lived then, whose destruction may be due both to gradual changes of climate and to man.--PICTET.] We may suppose, that, if man did exist during these convulsions and inundations, his superior intelligence would enable him to escape the fate of the animals that were submerged,--or that, if his few burial-places were invaded by the waters, his remains are now completely covered by marine deposits under the ocean. If, however, in his barbarian condition, he had fashioned implements of any hard material, and especially if, as do the savages of the present family of man, he had accidentally deposited them, or had buried them with the dead in mighty mounds, the invading waters might well sweep them together from their place and deposit them almost in mass, in situations where the eddies should leave their gravel and sand.[C] [Footnote C: Sir C. Lyell, in his remarks before the British Association |
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