EVIDENCES OF PREHISTORIC MAN IN WEST KENT. 331
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, the
river origin of the gravel cannot be doubted, and I have had
FIG. 3.—POINTED EOLITHS, WELL HILL.
1. From summit, 610 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