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Knickerbocker's history of New York, vol. 1 (of 2)

Note 27 — Chapter IV

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It is a matter long since established by certain of our philosophers,—that is to say, having been often advanced, and never contradicted, it has grown to be pretty nigh equal to a settled fact,—that the Hudson was originally a lake dammed up by the mountains of the Highlands. In process of time, however, becoming very mighty and obstreperous, and the mountains waxing pursy, dropsical, and weak in the back, by reason of their extreme old age, it suddenly rose upon them, and after a violent struggle effected its escape. This is said to have come to pass in very remote time, probably before rivers had lost the art of running uphill. The foregoing is a theory in which I do not pretend to be skilled, notwithstanding that I do fully give it my belief.

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