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" We may not merely admit," he says, " but assert as highly probable, that the axis of maximum inertia and axis of rotation, always very near one another, may have been in ancient times very far from their present geographical position, and may have gradually... "
Geological Magazine - Página 165
editado por - 1877
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Geological Magazine, Volumen2;Volumen4;Volumen14

Henry Woodward - 1877 - 642 páginas
...regard to the thickness of the crust at the present time, he did not despair of astronomers at hist conceding a less thickness than that assigned by the...effect of such changes as possibly cumulative. Mr. Evana felt that the Society was much indebted to Mr. Twisden for having likewise investigated the question,...
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Report of the Annual Meeting

British Association for the Advancement of Science - 1877 - 826 páginas
...; and we may not merely admit, but assert as highly probable, that the axis of maximum inertia and axis of rotation, always very near one another, may...perceptible sudden disturbance of either land or water. Lastly, as to variations in the earth's rotational period. You all no doubt know how, in 1853, Adams...
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Good Words, Volumen19

1878 - 926 páginas
...been in ancient times very differently situated to what it is at present, and, indeed, that " it might have gradually shifted through 10, 20, 30, 40. or...perceptible sudden disturbance of either land or water."* Thus it appears that nature prevents catastrophes by the very hugeness of the scale on which she works....
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Eclectic Magazine: Foreign Literature, Volumen28;Volumen91

John Holmes Agnew, Walter Hilliard Bidwell, Henry T. Steele - 1878 - 832 páginas
...situated to what it is at present, and, indeed, that " it might have gradually shifted through IQ, 20, 30, 40, or more degrees, without at any time any perceptible sudden disturbance of either land or wa1878. THE EARTH'S PLACE IN NATURE. ter."* Thus it appears that nature prevents catastrophes by the...
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Geological Magazine, Volumen2;Volumen5;Volumen15

Henry Woodward - 1878 - 642 páginas
...their present geographical position, and may have gradually shifted through ten, twenty, thirty, forty, or more degrees without at any time any perceptible sudden disturbance of either land or water." I am glad to think that this question, to which I to some extent assisted to direct attention, has...
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The Journal of Science, and Annals of Astronomy, Biology, Geology ..., Volumen15

James Samuelson, Sir William Crookes - 1878 - 606 páginas
...their present geographical position, and may have gradually shifted through ten, twenty, thirty, forty, or more degrees without at any time any perceptible sudden disturbance of either land or water." The President was glad to think that this question, to which he had to some extent assisted to direct...
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The Year-book of Facts in Science and Art

Charles W. Vincent, James Mason - 1879 - 264 páginas
...69 miles, and Sir W. Thomson has not only admitted but asserted as highly probable, that the poles may have been in ancient times ' very far from their...perceptible sudden disturbance of either land or water.' " I am glad to think that the question, to which I to some extent assisted to direct attention, has...
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The American Journal of Science, Volúmenes121-130

1885 - 524 páginas
...and cau•tion. Professor William Thomson indeed has stated that "the axis of maximum inertia, and axis of rotation — always very near one another...perceptible sudden disturbance of either land or water."* George Darwin also has admitted that if the earth be not solid, " As in successive periods the continents...
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Textbook of Geology

Archibald Geikie - 1882 - 996 páginas
...may not merely admit," he says, " but assert as highly probable, that the axis of maximum inertia and axis of rotation, always very near one another, may...perceptible sudden disturbance of either land" or water." 1 But though, in the earlier ages of the planet's history, stupendous deformations may have occurred,...
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Science, Volumen1

John Michels (Journalist) - 1895 - 758 páginas
...present geographical position, and may have gradually shifted through ten, twenty, thirty or forty or more degrees without at any time any perceptible sudden disturbance of either land or water." Sir William Thomson gave no account of the calculations made by him as the basis of these conclusions....
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