Redhill and Bromehill than that of either Santon Downham or of Gravel Hill, Brandon.
The Little Ouse joins the main river about 4 miles N.W. of Shrub Hill; and 5 miles N. of the junction the Ouse receives another affluent—the Wissey or Stoke River, draining 243 square miles—along the course of which, however, no palæolithic implements have as yet been found. The same is the case with the valley of the Nar or Setchy, a river which joins the Ouse just above King's Lynn, a few miles before it discharges into the Wash, and which drains an area of 131 square miles.
Along a great portion of its lower course the Ouse runs through a Fen country, where, of course, no gravel is to be seen; but at Ash Wicken and Leziate, a few miles E. of King's Lynn, and at South Wootton, about 2 miles to its N., the late Rev. John Gunn, F.G.S., found Drift-beds of apparently fluviatile character. In the gravels in a side valley leading into the marshes, near the School at South Wootton, Mr. W. H. Houghton, having been set upon the search for flint instruments by Mr. Gunn, found, in 1884, a tongue-shaped specimen, 514 inches long, in form much like that from Shrub Hill (Fig. 447), but having the whole surface worked, and having the flatter face slightly concave longitudinally. It is stained all over of an ochreous colour, and shows signs of use near the point, a part of which has been broken off. The angles, though not sharp, are not waterworn. The late Mr. James Wyatt, F.G.S., of Bedford, also found, in the year 1870, in gravel in a pit near Lynn—the base of which is seldom reached on account of its lying below the level of the water—an oval flint implement, well formed and deeply stained, and another of rude workmanship.
Many miles to the east, but still in Norfolk, there is seen in the cliff at West Runton,[1] near Cromer, what appears to be the channel of an old river, filled up with gravelly deposits. In these, at a depth of 12 feet from the surface, and above a black freshwater bed, Mr. A. C. Savin, of Cromer, in 1878, found in situ a fine well-wrought ovate implement of flint 434 inches long. A few years later I found on the sea-shore below, a large ochreous flake, apparently palæolithic, which I gave to Mr. Savin.
About 3 miles S.W. of Runton, near Gallows or Gibbet Corner, in Aylmerton parish, Mr. F. C. J. Spurrell found, in 1882, an ochreous implement from the gravels capping the hill, not far from Sherringham Heath. At East Runton,[2] in the pre-glacial "Forest Bed," Mr. W. J. Lewis Abbott thinks that he has found worked flints. I fail, however, to see any distinct marks of human workmanship upon his specimens.
With these discoveries in Norfolk and those near the mouth of the river, my account of the basin of the Ouse ceases, but before proceeding southwards I must record some others of the same kind.
Yorkshire lies far away from the usual scenes of palæolithic discoveries, but I have seen a pointed implement (334 inches), in form like Fig. 419, that was found on the surface at Huntow, near Bridlington. There is no record of its having been associated with any remains of the Quaternary fauna.
In the first edition of this book I recorded my finding an implement in form like Fig. 434, on a heap of stones near King's Langley, within
