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| | Letters to "Nature" on the Age of the Earth, by Alfred Russel Wallace |
 | | And this implies that at every successive period, from the Laurentian to the Pliocene, the conditions of denudation and deposition were totally different from what they are now, since at the present time it is demonstrable that the area of deposition of continental debris is only a fraction of the whole continental area. |
 | | They are therefore necessarily very much thicker than the average thickness of the denuded layer, and the ratio of the area of denudation to the area of deposition, which I have estimated at 19 to 1, gives their proportionate thickness. |
 | | If, however, the area of deposition is very much less than the area of denudation, which is now admitted to be the fact, then the rate of deposition per foot of thickness will be many times greater than the rate of denudation. |
| www.wku.edu /~smithch/wallace/S458AND.htm (806 words) |
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