Page:The Ancient Stone Implements (1897).djvu/646

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624
RIVER-DRIFT IMPLEMENTS.
[CHAP. XXIII.

worn. The elevation of the ground, at the spot where it was found, is estimated to be 86 feet above the mean sea-level.[1]

In another small pit, at a rather higher level, and close to the N.E. corner of the cemetery, at a depth of 5 feet from the surface, an oval implement was found by Mr. Read, in situ, in the gravel, which here attains a thickness of about 8 feet. In this, as also in the preceding case, a bed of brick-earth or loess has been removed from above the gravel. The surface of this implement is ochreous and polished, and its angles are waterworn. The periphery is much twisted, like that of Fig. 434 from Santon Downham.

At the N.W. comer of the Common, fully half a mile from the first pit, and at a higher level still, where the surface of the ground is stated to be more than 160 feet above the mean sea-level, was the extensive excavation known as the Town Pit. The gravel here retains the same character, but is perhaps rather less coarse; and above it is a thin bed of marl, which separates it from the loess or brick-earth, which in most places has been removed for use. The gravel itself attains a thickness of from 8 to 15 feet, and from "a fall," at about 6 feet from the surface, was picked out an ovate implement 41/2 inches in length, and in form like Fig. 419 from Bury St. Edmunds. Its edges are sharp, and its surface lustrous and stained of an ochreous tint, though on one face the flint has become partially whitened.

Another and still more interesting specimen (51/2 inches), which, like that last described, is now, by the kindness of Mr. Read, in my own collection, has also been found in this pit. It is irregularly oval in form, being somewhat truncated at one end, but bearing a strong general resemblance to that from Hill Head, Fig. 466. Its surface is lustrous and deeply stained all over of a bright ochreous colour, and its angles and edges are much water worn. The significance of this fact, in the case of an implement found in gravel capping a gently sloping tongue of land, between two rivers, the levels of which are now 160 feet below it, will be considered hereafter. Numerous other implements have been found near Southampton, and extensive collections of them are in the possession of Mr. W. E. Darwin and Mr. W. Dale. There is also a series in the Hartley Institution at Southampton. Higher up the valleys of the Itchen or the Test, none of the more highly-wrought implements have as yet been found in the gravels, although it seems probable that they may eventually be discovered, especially if the drift-beds at some considerable height above the present river levels be excavated. I have, however, seen a flake with one face artificial, and with signs of use or wear at the edge, which was found in a gravel-pit near the Fleming Arms, Swathling, a few miles north of Southampton, by Mr. Spencer G. Perceval. In the gravel near this place a molar of Elephas primigenius is recorded to have been found.[2]

I have also a deeply-stained ovate implement from Redbridge, close to Southampton, found by Mr. Worthington G. Smith.

I have already, in 1864, described elsewhere[3] the discoveries which have been made in the gravels on the eastern shore of

  1. Codrington, Quar. Journ. Geol. Soc., vol. xxvi. p. 537.
  2. Geologist, vol. vi. pp. 110-154.
  3. Quar. Journ. Geol. Soc., vol. xx. p. 188. See also Lyell, "Prin. of Geol.," 10th ed., vol. ii. p. 560.