Salisbury,[1] but only a few have since been discovered, as the gravel is little, if at all, worked; and it is therefore only on the slope of the hill where the beds have been cut through by the deepening of the valley that they occur. That shown in Fig. 468 is preserved in the Blackmore Museum. It is stained of an ochreous tint, and is worn at its edges. Others of similar form, but white, have also been found, as well as some large broad flakes. It is needless to discuss the character of the gravel, as so many discoveries, of which the circumstances can be better ascertained, have been made in the same neighbourhood. In the valley of the Wiley, at South Newton, about 5 miles above Salisbury, an isolated specimen of a flat ovate implement has also been found.
Fig. 468.—Lake. 12
Nearer Salisbury, at Bemerton and Fisherton, the discoveries have been of more interest and importance. They have already, to some extent, been described by myself,[2] principally from information given me by Dr. Humphrey P. Blackmore. The beds of Drift at these two places are at different levels on the slope of the north side of the valley of the Wiley, and of different characters; that at Bemerton being at the higher level, and principally gravel, and that at Fisherton lower, and principally consisting of brick-earth, with a few gravelly seams.
The pit at Bemerton, in which most of the implements have been found, is about a mile west of Salisbury, nearly opposite the new church, and close to the lane connecting the roads to Wilton and Devizes, and nearly midway between them. The gravel consists mainly of subangular flints, with a few Upper Greensand pebbles and Tertiary sandstone blocks in a red clayey matrix. It is 10 to 12 feet