A continent ten times the size of Europe elevated two miles would do little more than bring London to the latitude of Edinburgh, or Edinburgh to the latitude of London. He must be a sanguine geologist indeed who can expect to account for the glaciation... Geological Magazine - Página 389editado por - 1878Visualização integral - Acerca deste livro
| 1878 - 550 páginas
...deflection of 3° 17' (a deflection which would hardly sensibly affect climate), no less than one-tenth of the entire surface would require to be elevated...geography of the earth sufficient to deflect the pole half a dozen of miles, far less half a dozen of degrees. It does not help the matter much to assume... | |
| 1878 - 556 páginas
...require to be elevated to that height. A continent ten times the size of Europe elevated two miles wonld do little more than bring London to the latitude of...geography of the earth sufficient to deflect the pole half a dozen of miles, far less half a dozen of degrees. It does not help the matter much to assume... | |
| Sir Henry Hoyle Howorth - 1893 - 416 páginas
...one-tenth of the entire surface of the earth would require to be elevated to the height of 10,000 feet. A continent ten times the size of Europe elevated...geography of the earth sufficient to deflect the pole half a dozen miles, far less half a dozen degrees. It does not help the matter much to assume a distortion... | |
| 1878 - 1060 páginas
...deflection of 3° 17' (a deflection which would hardly sensibly affect climate), no less than one-tenth of the entire surface would require to be elevated...geography of the earth sufficient to deflect the pole half a dozen of miles, far less half a dozen of degrees. It does not help the matter much to assume... | |
| 1894 - 488 páginas
...climate) no less than ^ of the entire surface would require to be elevated to that height (10,000 feet). A continent ten times the size of Europe elevated...half-a-dozen miles, far less half-a-dozen degrees." 1. Darwin : Proc. Royal Soc. vol. 25, p. 328. 2. Darwin: Trans. Roy. Soc. vol. 167 (part. i). 3. Kelvin... | |
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