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  • It is reasonable to suppose that these rocks, 323 IO PRELIMINARY REPORT ON THE GEOLOGY OF including the coal, are a part of the Conglomerate forma- tion; and also that the Conglomerate, as a whole, is very much thickened in this direction, as it is known to have a thickness very much exceeding i,ooo feet along the Cum- berland and the Pine Mountain escarpments.
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