The specimen engraved as Fig. 72 was found in the neighbourhood of Wareham, Dorsetshire, and is in my own collection. It is formed of syenite, and, unlike the instruments previously described, is narrower at the edge than in the middle of the blade; the section shows that the faces are nearly flat. I have another celt, in which these peculiarities are exaggerated, the |128| faces being flatter, the blade thinner, and also wider in the middle in proportion to the edge, it being 5 1∕2 inches long, 2 1∕4 inches wide in the middle, and 1 1∕2 inches at the edge, and rather less than an inch in thickness. The material is a _Serpula_ limestone, and the celt was no doubt formed from a travelled block, as it was found in a Boulder-clay district at Troston, near Bury St. Edmunds. I have a much heavier implement from the same locality, and formed of the same kind of stone. It is 10 inches long, and rather wider in proportion than Fig. 72. It does not narrow towards the edge, but in section and general form may be classed with the specimen there figured. A large celt, 10 inches long, of the same section, but thinner proportionally, and with straighter and more parallel sides, in outline more like Fig. 79, was found at Pilmoor, in the North Riding of Yorkshire, and forms part of the Greenwell Collection. It is of clay-slate. Another in the same collection, and from North Holme, in the same Riding (10 inches), is broader and flatter, with the sides somewhat more square, and the edge more curved. One face is somewhat hollowed towards one side, possibly to grind out the trace of a too deep chip. A third is from Barmston, in the East Riding (10 1∕2 inches), and a beautiful celt of hornblendic serpentine (10 5∕8 inches), oval in section and pointed at the butt, was found at Cunningsburgh,[412] Shetland, and another of diorite (10 1∕8 inches), rather broader in its proportions than Fig. 72, on Ambrisbeg Hill,[413] Island of Bute. An analogous form from Japan is in the museum at Leyden. [Illustration: Fig. 73.—Forfarshire. 1∕2] A long narrow chisel-like celt, with an oval section, is given in Fig. 73. The original is of dark greenstone, and was found in Forfarshire. It is in the National Museum at Edinburgh. I have a larger celt of the same form (5 1∕2 inches), formed of a close-grained grit, and found at Sherburn, Yorkshire. Messrs. Mortimer have another of schist (4 1∕2 inches), from Thixendale, Yorkshire. This form occurs, though rarely, in Ireland. A much larger celt, of metamorphic rock, 8 1∕2 inches long, 3 inches broad at the edge, and 1 3∕4 inches at the butt, 1 3∕8 inches thick, was found on Throckley Fell, Northumberland, and is in the Museum at Newcastle.