which characterizes the Tuscarawas River everywhere below the glacial boundary. Additional interest is given to this discovery by the fact that it is from one of the valleys to which I had directed attention several years before as likely to yield such discoveries.
The other most important facts bearing on the antiquity of man come from the Pacific coast, and perhaps have only an indirect connection with the Glacial period; but as their connection
Fig. 1.—The Smaller is the Palæolith from Newcomerstown, the Larger from Amiens (face view).
with the period must stand or fall with the facts collected some years ago by Prof. Whitney, I will allude to them here.
In the autumn of 1889, Mr. Charles Francis Adams, then President of the Union Pacific Railroad, brought to my notice a small clay image, an inch and a half in length, which had been found by Mr. M. A. Kurtz while boring an artesian well at Nampa, Ada County, Idaho. The image was of slightly baked clay, incrusted in part with a coating of red oxide of iron, which indicated considerable age, and came up in the sand-pump from a depth of three
