wich.[1] In the lower beds of sand, at a height of but a few feet above the sea, he found freshwater shells (including the Corbicula fluminalis), mammalian remains, and valves of the marine shell Balanus, as well as Entomostraca and Foraminifera, characteristic of brackish water conditions. It would appear that we have here another instance of the occurrence of beds with the Corbicula, at no great distance from those productive of flint implements, but at a lower level. From a pit of the same character, on the opposite side of the road, I have seen elephant remains in the possession of Mr. Slater, of Grays, near Chislet.
Fig. 464a.—Canterbury. 12
Another palæolithic implement of ovate form was discovered in 1865, on a heap of stones, about 3 miles north of Folkestone, by Mr. W. Topley, F.R.S., of the Geological Survey. It is of course impossible to say from what source it was derived; but it may be mentioned that at Folkestone itself, at the top of the West Cliff, near the Battery, at the height of 110 feet above low-water mark, are some beds of Drift of much the same character as those in which flint implements have occurred in other localities, containing remains of Elephas primigenius, Hippopotamus major, and other mammals, and shells of Helix.
Since this passage was written, a remarkably well-shaped ovate implement has been found in St. John's Road (Radnor Park end), Folkestone, by Mr. Richard Kerr, F.G.S., in August, 1893. It lay in brick-earth at a comparatively low level, and is of flint partially whitened. With it was found a molar tooth of Rhinoceros tichorhinus. It is now, through Mr. Kerr's kindness, in my collection, and is represented in Fig. 464b.
- ↑ Quar. Journ. Geol. Soc., vol. xi. p. 110.
