Journal of the Transactions of the Victoria Institute, Or Philosophical Society of Great Britain, Том 13Victoria Institute., 1880 |
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Стр. 19
... result of the cor- rections thus required will be practically to set aside the 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 ...
... result of the cor- rections thus required will be practically to set aside the 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 ...
Стр. 21
... resulting temperature 10 ° .3 . This is nearly the same as that of Canada , near Quebec , while the summer tempera- ture , by the previous estimate , would be almost 30 ° higher . This is wholly different from the conditions of a ...
... resulting temperature 10 ° .3 . This is nearly the same as that of Canada , near Quebec , while the summer tempera- ture , by the previous estimate , would be almost 30 ° higher . This is wholly different from the conditions of a ...
Стр. 23
... result , but shows at the most a limit towards which the temperature would tend , if the solar heat and radiation into space maintained the given proportions for an indefinite period of time . If the rule were sound , some very ...
... result , but shows at the most a limit towards which the temperature would tend , if the solar heat and radiation into space maintained the given proportions for an indefinite period of time . If the rule were sound , some very ...
Стр. 24
... result would be an increase of summer heat and winter cold , each about 28 ° at the most , but probably much ... resulting from the progression of the apsides alone . The change from precession for this same period , at the present rate ...
... result would be an increase of summer heat and winter cold , each about 28 ° at the most , but probably much ... resulting from the progression of the apsides alone . The change from precession for this same period , at the present rate ...
Стр. 26
... results for Great Britain . 88 • 0415 302 ° 47 ' ⚫01564 16 ° .18 48 ° • 41 87 * 0544 135 ° 7 ′ ! -'01572 - 17 ° 07 15 ° .16 86 • 0631 326 ° 0 ' 01679 18 ° .23 50 ° .46 85 * 0664 156 ° 22 ' -'00980 - 10 ° 64 21 ° .59 84 ⚫0622 346 ° 46 ...
... results for Great Britain . 88 • 0415 302 ° 47 ' ⚫01564 16 ° .18 48 ° • 41 87 * 0544 135 ° 7 ′ ! -'01572 - 17 ° 07 15 ° .16 86 • 0631 326 ° 0 ' 01679 18 ° .23 50 ° .46 85 * 0664 156 ° 22 ' -'00980 - 10 ° 64 21 ° .59 84 ⚫0622 346 ° 46 ...
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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