in thickness, and attains a height of at least 100 feet above the river, though in this particular pit it is only about 80 feet above it. The gravel caps the hill, instead of lying merely in a trough along its side, so that in this particular, the section I have elsewhere given is incorrect. The chalk comes nearly to the surface, lower down the slope, and divides the gravel from a brick-earth deposit continuous with that of Fisherton, farther down the valley.
Fig. 469.—Bemerton. 12
The implements found at Bemerton are principally oval, ovate, and ovate-lanceolate. They are for the most part considerably altered in texture at the surface, and many of them are much rolled and waterworn. A few flakes and spalls of flint have also been found. The original of Fig. 469 is in the Blackmore Museum, and is of grey flint, not waterworn. It shows some marks of use on the edge, towards the point, and a portion of the natural crust of the flint remains at the base. In all, upwards of twenty specimens have been found in this gravel, one of them as high as the cemetery. Several others have also been found between that place and Highfield, which is about a quarter of a mile nearer Salisbury than the Bemerton Pit; and in gravel which there caps the hill between the Wiley and the Avon, implements have also been found.
Fig. 470.—Highfield. 12
A remarkably small specimen from this place is shown in Fig. 470. It is of grey flint, slightly ochreous, and with its angles somewhat worn. The original is in the Blackmore Museum.
