tastefully-decorated objects of bronze and gold, shows conclusively that stone remained in use for certain purposes, long after the knowledge of some of the metals had been acquired.
The hammer-heads of the next form to be noticed are of a simpler character, being made from ovoid pebbles, usually of quartzite, by boring shaft-holes through their centres. The specimen I have selected for illustration, Fig. 155, is in my own collection, and was found in
Fig. 155.—Redgrave Park. 12
Redgrave Park, Suffolk. It is said to have been exhumed ten feet below the surface, by men digging stone in Deer's Hill. The pebble is of quartzite, probably from one of the conglomerates of the Trias, but more immediately derived from the gravels of the Glacial Period, which abound in the Eastern Counties. The hole as usual tapers towards the middle of the stone. The pebble is battered at both ends, and slightly worn away by use. I have a rather smaller, and more kidney-shaped hammer, also slightly worn away at the ends, found at Willerby Carr, in the East Riding of Yorkshire, and one (4 inches), that is considerably worn at both ends, from Stanifield, Bury St. Edmunds. An example was found at Normandy,[1] near Wanborough, Surrey. I have seen one formed from a sandstone pebble (412 inches) found near Ware.
Fig. 156.—Redmore Fen. 12
In the Greenwell Collection is a large specimen, made from a flat pebble (712 inches) obtained at Salton, York, N.R.
Fig. 156 shows a smaller variety of the same type, but rather square in outline, and with the shaft-hole much more bell-mouthed. The original is in my own collection, and was found in Redmore Fen, near Littleport, Cambridgeshire. I have others from Icklingham (238 inches) and Harleston, Norfolk (314 inches). Hammers of this and the preceding type are by no means un-- ↑ Surr. Arch. Coll., vol. xi. p. 248-9.
