Page:The Ancient Stone Implements (1897).djvu/138

116 its faces present a series of diverging cracks, of slight depth, apparently- resulting from the dissolution of calcareous veins in the stone. It was found at Nunnington, Yorkshire, and now forms part of the Greenwell Collection.

The original of Fig. 58 was discovered at Burradon, Northumberland, where also the fine flint celt, Fig. 47, was found. This likewise is in the Greenwell Collection. It is of porphyritic stone, and has the angles of the flat sides slightly rounded. Another, in the same collection, 4 inches long, from Doddington, in the same county, is of similar character. Celts of much the same shape and size have been found in the Shetland Isles; one of these, 5 inches long, from West Burrafirth, is in the British Museum. A similar form is found in Japan.

Fig. 59 shows a celt of much the same kind, found at Livermere, near Bury St. Edmunds. It is formed of a close-grained greenstone, and is in my own collection. The angles at the sides are slightly rounded. I have others of nearly the same size and of similar material, found near Cirencester, and at Soham and Bottisham, Cambs. Greenstone celts of about this size, and with the sides more or less flat, so as to range between Figs. 48 and 58, are of not uncommon occurrence in the Fen country. Mr. Fisher, of Ely, has one, found near Manea, and several from Bottisham. I have one, of felstone, 3 inches long, found at Coton, Cambs., one side of which presents a flat surface inch wide, while the other is but slightly flattened. One (4 inches) was found near Torquay, Devon.

A still more triangular form, more convex on the faces, and having