CORNELL UNIVERSITY LIBRARY Cornell University Library E 74.03C59 Pre-historic remains which were found on 3 1924 028 714 776 Cornell University Library The original of tiiis book is in the Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/cletails/cu31924028714776 THE CIl^TCIIsTNATI TABLET. ^ ^' 1 'I li' * ', M Mil';! 1^: \ Ji iW^t* V. *v J, liiitiiiiiiiiiiiiiiiiiiiiiiiijiiiiiilii THE PRE-HISTORIC REMAINS WHICH WERE FOUND On the Site of the City of Cincinnati, Ohio VINDICATION "CINCINNATI TABLET" By ROBERT CLARKE CINCINNATI 1876 CPre-hisioric (Remains at Cincinnati. face of the earth, with the head toward the setting sun, and at the southwest side of, or about fifteen feet from, an extensive mound of earth, raised probably for the purpose of a burial-ground, upon the margin of the second bank of the Ohio river (suddenly rising fifty feet above the first), and now elevated, in the extreme, eight feet from the general level of the same, with a gradual slope in the various directions, and a base of about one hundred and twenty feet by sixty. One of the main streets of the town passes through the western part of this grave, and in the frequent repairs of the acclivity, human bones have often been found. ... I should not omit to mention to you, that upon this mound are stumps of oak trees seven feet in diameter." This mound was, however, merely an appendage to the general works on the upper plain, mentioned by Colonel Sargent, but not described. The first descrip- tion of them is given by Dr. Daniel Drake in his Picture of Cincinnati, published in 1815. This I will use freely in endeavoring to give an idea of the character of the works. Cincinnati is built on two levels or benches of an alluvial plain, surrounded on the east, north, and west by hills of the lower silurian limestone — on the south is the Ohio river. On the lower level, or " bottom," no works of the mound-builders existed. Of this, how- ever, we have only negative evidence ; if any works existed on it, they may have gradually been obliterated by the overflow of the Ohio river, to which th^ bottom is subject. The "hill," as it was called in early days, rose from fifty to seventy feet above the bottom, and in its natural state was quite abrupt, but is now, of course, graded down to suit the exigencies of a city. It com- menced near Deer Creek, in the eastern part of the city, about two hundred feet distant from the Ohio. Thence