Journal of the Transactions of the Victoria Institute, Or Philosophical Society of Great Britain, Том 13Victoria Institute., 1880 |
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Стр. 12
... whole distance in 100,000 years . And since we cannot tell whether the earlier motion may not have varied so far in its direction , we can have no assurance that all the elements of our system may not have been altered by the proximity ...
... whole distance in 100,000 years . And since we cannot tell whether the earlier motion may not have varied so far in its direction , we can have no assurance that all the elements of our system may not have been altered by the proximity ...
Стр. 13
... whole surface , is the arrangement most favourable to a mitigation of fierce . extremes , and to fit our world for human habitation . At the same time , since the glacial epoch belongs to a stage of geology when the outlines of land and ...
... whole surface , is the arrangement most favourable to a mitigation of fierce . extremes , and to fit our world for human habitation . At the same time , since the glacial epoch belongs to a stage of geology when the outlines of land and ...
Стр. 17
... whole , it suffers the most from extreme cold . With an excentricity of 0575 , or 10 millions excess of aphe- lion over perihelion distance , the excess above the present would be three - twentieths per cent . , or 1 part in a thousand ...
... whole , it suffers the most from extreme cold . With an excentricity of 0575 , or 10 millions excess of aphe- lion over perihelion distance , the excess above the present would be three - twentieths per cent . , or 1 part in a thousand ...
Стр. 18
5 4 as 7 to 3 , and for the whole half - year as 5 to 3. There is an excess or defect of about one - fourth of the mean value . Hence of 10 + 2 of 8 18.5 , will be the total heat for the northern , and of 10 + 5 of 8 of 10 of 8 = 17.5 ...
5 4 as 7 to 3 , and for the whole half - year as 5 to 3. There is an excess or defect of about one - fourth of the mean value . Hence of 10 + 2 of 8 18.5 , will be the total heat for the northern , and of 10 + 5 of 8 of 10 of 8 = 17.5 ...
Стр. 19
... whole theory . 32. First , the excentricity is calculated by M. Leverrier's formulæ . It might seem beforehand very doubtful whether these can be relied on for a date three millions of years ago , or even for 850,000 , or 210,000 years ...
... whole theory . 32. First , the excentricity is calculated by M. Leverrier's formulæ . It might seem beforehand very doubtful whether these can be relied on for a date three millions of years ago , or even for 850,000 , or 210,000 years ...
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Agni Ahuramazda ancient animals antiquity appear argument Aryaman Aryan associated Asura Avesta believe Bishop bones breccia Brixham Callard cause cave cave-earth Christian conclusion Daksha Dawkins deposit Devas Ditto divine doctrine earth Europe evidence existence extinct mammalia fact feet flint force Gathas geological geologists glacial epoch gravel heat heaven human Hume hyæna implements inch intelligence Kent's Cavern lived Lyell mammoth meeting Members mind Mithra monotheism nature neolithic objects observed paleolithic Paley paper Pengelly period phenomena philosophical physical polished stone age pottery present Prof question reason referred regard reindeer religion remains remarks rhinoceros Rig-Veda river scientific Scripture seems Society Somme soul stalagmite stone age supposed Teleology Terrace theory things thought tion traces truth Tyndall valley Varuna Vedic VICTORIA INSTITUTE Vide whilst woolly rhinoceros Yama Yasna Zoroaster Zoroastrian