EVIDENCES OF PREHISTORIC MAN IN WEST KENT. 33-1 



some little doubt as to the true character of the plateau drift on 

 the Downs, and the opponents of Eoliths have not been slow in' 

 casting doubts as to its antiquity. At Well Hill, however, tlie- 

 river origin of the gravel cannot be doubted, and I have had 



FIG. 3. — POINTED EOLITHS, WELL HILL. 



1. From summit, 6to feet. 



2. From trailed material, 450 feet O.D. 



satisfaction in finding in this ancient deposit some interesting 

 implements, now placed on the table for inspection. (Figs. 2 

 and 3.) 



I do not think I can better illustrate the antiquity of this 



