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Show 1836- 1837] Fogg's Far West 147 stance would have been deemed an omen, and, as such, commemorated in the chronicles of the city. On the 15th of February, 1764, Colonel Auguste Chouteau, with a number of persons from Ste. Genevieve, Cahokia, and Fort Chartres, arrived at the spot, and commenced a settlement by felling a splendid grove of forest- trees which then reared itself upon the bank, and erecting a building where the bility, therefore, of their having been imparted by some individual of a race of men who were strangers to the art of tanning skins, and at a period much anterior to that to which any traditions of the present race of Indians reaches, derives additional weight from this peculiar shape of the feet. " In other respects, the impressions are strikingly natural, exhibiting the muscular marks of the foot with great precision and faithfulness to nature. This circumstance weakens very much the supposition that they may, possibly, be specimens of antique sculpture, executed by any former race of men inhabiting this continent. Neither history nor tradition has preserved the slightest traces of such a people. For it must be recollected that, as yet, we have no evidence that the people who erected our stupendous Western tumuli possessed any knowledge of masonry, far less of sculpture, or that they had even invented a chisel, a knife, or an axe other than those of porphyry, hornstone, or obsidian. " The average length of the human foot in the male subject may, perhaps, be assumed at ten inches. The length of each foot, in our subject, is ten and a quarter inches: the breadth, taken across the toes, at right angles to the former line, four inches; but the greatest spread of the toes is four and a half inches, which diminishes to two and a half at the heel. Directly before the prints, and approaching within a few inches of the left foot, is a well- impressed and deep mark, having some resemblance to a scroll, whose greatest length is two feet seven inches, and greatest breadth twelve and a half inches. " The rock containing these interesting impressions is a compact limestone of a grayish- bhie colour. It was originally quarried on the left bank of the Mississippi at St Louis, and is a part of the extensive range of calcareous rocks upon which that town is built. It contains very perfect remains of the encrinite, echinite, and some other fossil species. The rock is firm and well consolidated, as much so as any part of the stratum. A specimen of this rock, now before us, has a decidedly sparry texture, and embraces a mass of black blende. This rock is extensively used as a building material at St Louis. On parting with its carbonic add and water, it becomes beautifully white, yielding an excellent quick- lime. Foundations of private dwellings at St. Louis, and the military works erected by the French and Spaniards from this material sixty years ago, are still as solid and unbroken as when first laid. We cite these facts as evincing the compactness and durability of the stone- points which must essentially affect any conclusions, to be drawn from the prints we have mentioned, and upon which, therefore, we are solicitous to express our decided opinion."- FLAOO. |