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Excerpt from On the Geology of the Delta, and the Mudlumps of the Passes of the Mississippi
I have shown that toward the close of the Drift period, the place of the present Mississippi was occupied by what, but for its stupendous prop/ortions, might be termed a torrent of fresh water, having, even as far south as the present coast line, a velocity sufficient to transport pebbles of five to six ounces weight, from localities not nearer than Tennessee and northern Arkansas; together with the smaller ones derived, doubtless.
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