river to the terminal moraine. Its surface is about thirty-five feet above the flood-plain of the Tuscarawas; it consists of stratified material, containing many granitic pebbles and much granitic gravel. The deposit at Newcomerstown extends over many acres, having been protected from erosion in the recess at the
Fig. 6.
mouth of Buckhorn Creek. Through the middle of this deposit the railroad had cut its road-bed, and for years has been appropriating the gravel for ballast.
Mr. Mills is an educated business man, who had been a pupil in geology of Prof. Orton, of the State University, and had with him done considerable field-work in geology. Mr. Mills's character and reputation are entirely above suspicion. In addition to his business he took a laudable interest in the collection of Indian relics, and had in his office thousands of flint implements, collected by him and his associates in the vicinity, who had been organized into an archæological society. His office was but a short distance from the gravel pit from which I have said the
