A palæolitliic flake has been found still farther east, at Stone,[1] between Exbury and Calshot Castle.
Assuming the existence of an ancient river Solent flowing at an elevation of upwards of 100 feet above the present level of the sea at Bournemouth, its western sources must have drained much the same basin as that of the rivers now discharging into Poole Harbour; but without at present entering into that question, I may mention the discovery of a palæolithic implement at Dewlish, about 3 miles N. of Piddletown, Dorsetshire, by Mr. James Brown, of Salisbury. It is very neatly chipped, but slightly unsymmetrical in form, one side being straight and the other curved; but in general character it resembles Fig. 430 from Thetford, having been made from a large flake, and showing the original crust of the flint at its base. It was found on the surface, at the top of a high hill, at no great distance from the branch of the Trent or Piddle, which flows past Dewlish. Elephant[2] remains have been found near the same place, which have, however, been assigned to Elephas meridionalis.
Fig. 477.—Broom Pit, Axminster. 12
