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- W2107750723 abstract "Although the more immediate object of geologists in the actual state of their science is rather the collection of facts, and such an induction of conclusions from them as shall be, so far as possible, independent of theory; yet when theory confines itself to pointing out the influence of causes which we know to exist, in modifying the general condition of our globe, and enables us to estimate the extent of their action, it may be regarded as rendering a real service to science. It thus tends in some degree to diminish the complexity of the problems to be resolved, or at least to reduce them to their true difficulty, by showing what portion of them can and what cannot be accounted for on known principles, thereby narrowing the field of research, and directing the efforts of future speculators to the discovery of causes of another description.This consideration has induced me, not without some degree of hesitation, to offer to this Society, though in a very crude and imperfect state, some views which have occurred to me of a possible explanation of a portion, at least, of that great geological phaenomenon,—the difference between the actual climates now prevailing over extensive regions of the earth’s surface, and perhaps over its whole extent, and those which the organic remains discovered in its strata lead us to conclude have formerly subsisted during very long periods of time. The ingenious attempts which have been lately made to account for this remarkable fact" @default.
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- W2107750723 date "1832-01-01" @default.
- W2107750723 modified "2023-10-01" @default.
- W2107750723 title "XVII.—On the Astronomical Causes which may influence Geological Phænomena." @default.
- W2107750723 doi "https://doi.org/10.1144/transgslb.3.2.293" @default.
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