Faith and Thought, Том 13 |
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Стр. 6
The heat , generated by internal pressure , will partly escape through the opening , while the pressure also is lessened by the rupture of the crust . The approach must be constantly towards a limit , when the upward and expansive force ...
The heat , generated by internal pressure , will partly escape through the opening , while the pressure also is lessened by the rupture of the crust . The approach must be constantly towards a limit , when the upward and expansive force ...
Стр. 7
He calculates , from Fourier's theory of the rate of conduction , and the specific heat of rocks at Edinburgh and Greenock , that the consolidation of the earth's crust cannot have taken place less than 20 nor more than 400 millions of ...
He calculates , from Fourier's theory of the rate of conduction , and the specific heat of rocks at Edinburgh and Greenock , that the consolidation of the earth's crust cannot have taken place less than 20 nor more than 400 millions of ...
Стр. 8
The view , which Sir William rejects as more hypothetical , that the heat is generated by chemical change , seems to me less hypothetical and more natural than his own ; and needs only to be carried a step further and applied to the ...
The view , which Sir William rejects as more hypothetical , that the heat is generated by chemical change , seems to me less hypothetical and more natural than his own ; and needs only to be carried a step further and applied to the ...
Стр. 9
It had been shown by Sir W. Thomson and others , from physical considerations of the sun's heat and the secular cooling of our globe , that the history of the earth's crust must be limited to a period of something like a hundred ...
It had been shown by Sir W. Thomson and others , from physical considerations of the sun's heat and the secular cooling of our globe , that the history of the earth's crust must be limited to a period of something like a hundred ...
Стр. 10
If there be a difference , which is probable , I think it much more likely that it would be of an opposite kind , and that its heat has increased by condensation , more than it has lost by dissipation . In the " Theory of Helmholtz ...
If there be a difference , which is probable , I think it much more likely that it would be of an opposite kind , and that its heat has increased by condensation , more than it has lost by dissipation . In the " Theory of Helmholtz ...
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accept according ancient animals antiquity appear argument Associates bear believe Bishop body bones called cause cave cavern Christian conclusion connection considered Council deposit discussion divine doubt earth evidence existence extinct fact faith feet flint force geological give given glacial gravel ground hear heat human implements Institute interesting known late less lived mammoth matter means meeting Members mind nature objects observed opinion origin period Philosophical physical Pleistocene position present principle probably produced Prof Professor prove question reason recent referred regard religion remains remarks result river scientific seems Society South stalagmite stone Street supposed surface taken theory things thought true truth Tyndall University valley whole