Though terraces of gravel are found at various places along the course of the Waveney, and apparently of the same age as those of the Little Ouse valley, yet up to the present time no discoveries of implements in them have been recorded, although it seems improbable that it is at Hoxne alone that implements exist.
In the gravels of the valleys of the Gipping, and other small streams between the Waveney and the Stour, no works of man have as yet been discovered; but in a pit worked for ballast, near Melford Junction, on the Great Eastern Railway, and at no great distance from the Stour, the late Mr. Henry Trigg discovered one or two implements of flint, and a portion of a tooth of Elephas primigenius. Some worked flints have also been found in the gravel at Sudbury, Suffolk, and some palæolithic implements in the valley of the Stour, north of Colchester. In the cliff at Stutton, opposite Manningtree, is a freshwater deposit containing many shells of Corbicula fluminalis. Numbers of these washed out from the cliff are lying on the shore, and among them I found, in 1883, a broad flake about 3 inches long, which has all the appearance of being palæolithic. At Lexden Park,[1] near Colchester, Mr. Edward Laver has found a small ovate implement with a cutting edge all round, ogival in character. Some other specimens have been discovered to the north of Colchester. On the banks of the Ter, a tributary of the Chelmer, Mr. J. French[2] has found two palæolithic implements near Felstead; and in 1883, at North End Place, 112 miles south of Felstead, the Rev. A. L. Rowe, F.G.S., picked up a rudely chipped heavy oval implement of quartzite (6 inches) which he has kindly added to my collection.
The valleys of the small rivers between the Stour and the Thames, the Colne, the Blackwater, and the Crouch, have up to the present time produced no relics of human workmanship, though I have seen a rudely worked flint, apparently from gravel, which was found on the sea-shore by Mr. W. Whitaker, F.R.S., a little to the north of the mouth of the Colne.
Before proceeding to discuss the discoveries that have been made within the basin of the Thames and in the Southern counties, I must call attention to one that was made in 1890 in the Midland Counties, not far from Birmingham.
The old gravels of the river Rea at Saltley, Warwickshire, have for a long time been subjected to a careful examination by Mr. Joseph Landon, F.G.S., of Saltley College, in the hope of
