Cincinnati had, at this time, (1818,) the appearance of a rapidly growing city, which appeared to have, from some general causes, been suddenly checked in its growth. Whole rows of unfinished brick buildings had been left by the workmen. Banks, and the offices of corporate and manufacturing companies, were not unfrequently found shut. Nor did it require long looking or much inquiry to learn that it had seen more prosperous times. A branch bank of the U. S. then recently established there, was much and bitterly, but I know not how justly, spoken against. But if there was not the same life and air in all departments, that formerly existed, there was abundant evidence of the existence of resources in the city and country, which must revive and push it onward in its career and growth, to rank second to no city west of the Alleghanies. This city owes its origin, I believe, to John Cleves Symes, father-in-law of the late President Harrison, a Jerseyman by birth, who, in planning it, took Philadelphia as his model. This has imparted a regularity to its streets, and squares, that visitors will at once recognize, as characteristic of its parentage. It stands on a heavy diluvial formation of various layers of clay, loam, sand, and gravel, disposed in two great plateaux, or first and second banks, the lowest of which is some thirty or forty feet above the common summer level of the Ohio. Yet this river has sometimes, but rarely, been known to surmount this barrier and invade the lowermost streets of the city. These diluvial beds have yielded some curious antiquarian relics, which lead the mind farther back, for their origin, than the Indian race. The most curious of these, if the facts are correctly reported to me, was the discovery of a small antique-shaped iron horse-shoe, found twenty-five feet below the surface in grading one of the streets, and the blunt end, or stump of a tree, at another locality, at the depth of ninety-four feet, together with marks of the cut of an axe, and an iron wedge. I have had no means to verify these facts, but state them as credible, from the corroborative testimony afforded them by other discoveries in the great geological basin of the west, examined by me, which denote human occupancy in America prior to the deposition of the last of the unconsolidated and eocene series.