MAN AND THE GLACIAL PERIOD. 



643 



gravel at Loveland, led me, on the 11th and 12th of No- 

 vember, 1887, to visit the localities and see their relation to 

 the glacial deposits of the region. The situation is as fol- 

 lows : 



Fig. 167.— Map showing glacial boundary, channels, and terraces near Cincinnati. 



Madisonville is situated eleven miles northeast of Cincin- 

 nati, in a singular depression connecting the Little Miami 

 Kiver with Mill Creek, about five miles back from the Ohio 

 (see Fig. 167). The Little Miami joins the Ohio some miles 

 above Cincinnati, while Mill Creek joins it just below the 



