appearance, both {the faces and aides being almost flat and nearly parallel. This peculiarity of form is no doubt mainly due to the schistose character of the rock from which the implement is made; which, in the case of the original of Fig. 64, is a close-grained slate or hone-stone. It was found at Swinton, near Malton, Yorkshire, and was given to me by the late Mr. C. Monkman. The angles are slightly rounded, and the butt-end is tapered off as if to an edge, which, however, is now broken away.
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| Fig. 64.—Swinton, neax Malton.12 | Fig. 65.—Scamridge Dykes, Yorkshire.12 |
Long, narrow celts of this rectangular section are of very rare occurrence both in Britain and Ireland, and, so far as I am aware, have never been found of flint. In Denmark, on the contrary, they are common in flint, but generally of a larger size than the specimen here engraved . The faces also are usually rather more convex.
They are to be found among the North American[1] forms, sometimes with a hole towards the butt-end, as if for suspension.
Somewhat the same form occurs in Siam and in the Malay Peninsula.
The next specimen, shown in Fig. 65, is of the same material as the last, and was found in the same neighbourhood, at the Dykes, Scamridge, in the North Riding of Yorkshire. Owing to the irregular fissure of the stone, it is considerably thicker at one side than the other. The broader side is flat with the angles chamfered, and the narrower side is rounded. The faces taper at the butt-end, which is ground to a- ↑ Schoolcraft, "Ind. Tribes," vol. i., pl. xi. 3; xiv. 2.
