Journal of the Transactions of the Victoria Institute, Or Philosophical Society of Great Britain, Том 13Victoria Institute., 1880 |
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Стр. 4
... result to the ordinary operations of nature , combined with the element of unlimited time ; the other , appealing to agents that operated during the earlier epochs of the world with greater intensity , and over wider areas . The former ...
... result to the ordinary operations of nature , combined with the element of unlimited time ; the other , appealing to agents that operated during the earlier epochs of the world with greater intensity , and over wider areas . The former ...
Стр. 11
... results on the relative specific gravity of solid and melted rocks , are in perfect accordance with §§ 832-849 , on the present condition of the earth's interior ; that it is not , as commonly supposed , all liquid within a solid crust ...
... results on the relative specific gravity of solid and melted rocks , are in perfect accordance with §§ 832-849 , on the present condition of the earth's interior ; that it is not , as commonly supposed , all liquid within a solid crust ...
Стр. 14
... result , as Mr. Croll contends , from the latter combination , it must have done so from the other , and for the same reason . On the other hand , if a hotter summer undoes and reverses the effect of a colder winter with an increased ...
... result , as Mr. Croll contends , from the latter combination , it must have done so from the other , and for the same reason . On the other hand , if a hotter summer undoes and reverses the effect of a colder winter with an increased ...
Стр. 16
... result from increased excentricity does not seem to follow . 28. A second objection has some weight . The total heat received by the earth in a year from the sun is inversely as the minor axis , when the periodic time and the 16.
... result from increased excentricity does not seem to follow . 28. A second objection has some weight . The total heat received by the earth in a year from the sun is inversely as the minor axis , when the periodic time and the 16.
Стр. 18
... result cannot depend on a lessened total amount of solar heat incident on the earth at the eras in question , for ... results -6 ° 3 and + 1 ° 3 F. for the midwinter heat of our country at those two eras . With such a degree of cold ...
... result cannot depend on a lessened total amount of solar heat incident on the earth at the eras in question , for ... results -6 ° 3 and + 1 ° 3 F. for the midwinter heat of our country at those two eras . With such a degree of cold ...
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