used, but was either mounted in some manner, or else some means were adopted for protecting the hand against its asperities. I have already called attention to its resemblance to an implement from Kent's Cavern, Fig. 388a.
The second specimen, Fig. 415, still shows the natural crust of the flint at its truncated end, and is well adapted for being held in the hand when used.
Other specimens from the Biddenham Pit are engraved on the scale of one-half linear measure in Figs. 416 to 418.
The whole, with the exception of Fig. 417, were in the collection of the late Mr. Wyatt.
Fig. 416 is of ochreous cherty flint, symmetrically chipped, and showing a portion of the original crust of the flint at the base. Its angles are sharp, and not water-worn. In character it much resembles many of the implements from the valley of the Little Ouse, and from St. Acheul, near Amiens.
The original of Fig. 417 is in my own collection, having been kindly presented to me by Mr. Wyatt. As will be seen, it is remarkably thick at the butt, which is somewhat battered, almost as if the instrument had been used as a wedge. On a part of the butt is a portion of the white crust of the flint, which is somewhat striated, and suggestive of the block of flint from which the implement was fashioned having been derived from some Glacial deposit.
Fig. 418.—Biddenham, Bedford. 12
Fig. 418 represents a very curious form of implement made from a part of a sub-cylindrical nodule of flint, and chipped to a rounded point at one end, and truncated at the other, where the original fractured surface of the flint is left intact. The angles at the pointed end are but little worn.
Implements of various other forms and sizes have been found in the gravels near Bedford, but in character they so closely correspond with those found in other parts of England, and in France, that it seems needless to particularize them. One of them, however, in my own collection, 1014 inches long by 414 inches wide, tongue-like in character, but of a long ovate shape, deserves special mention. It was found at Biddenham. The flat ovate, or oval type, is there of extremely rare occurrence.
I have numerous other specimens from the Bedford gravels, principally from Kempston, and others exist in various public and private collections. Like the mammalian remains, they occur for the most part towards the base of the gravel, but occasionally at higher levels in the beds. Besides the more highly wrought instruments, knife-like flakes of flint have been found, some of them presenting
