The Ancient Stone Implements, Weapons and Ornaments, of Great Britain: Second Edition, RevisedEvans, John
History
The Ancient Stone Implements, Weapons and Ornaments, of Great Britain: Second Edition, Revised
Evans, John
Great Britain -- Antiquities; Stone age -- Great Britain
Mr. J. W. Cursiter, of Kirkwall, has a beautiful, long, narrow celt of
oval section, from Lunnasting, Shetland. It is formed of spherulitic
felstone, and is 9 1∕4 inches long, but only 2 1∕8 inches wide at the
broadest part. Another, 12 inches long, from Trondra, is of felstone,
and slightly curved longitudinally, so that it was probably an adze.
Others[403] (14, 11, 10 1∕2, and 9 inches) have been figured.
In the Greenwell Collection is a celt of this kind formed of
porphyritic greenstone, 13 inches long, from Sandsting, Shetland.
A celt of greenstone (8 inches), in outline much resembling Fig. 72,
was found, in 1758, at Tresta, in the parish of Aithsting, Shetland,
and is now in the British Museum. It is flat on one face, the other
being convex, so that the section is an oval with a segment removed.
Such an instrument must, in all probability, have been mounted as an
adze, though the flat face may have originally been due to the cleavage
of the material, which is a porphyritic greenstone.
Another celt (6 1∕4 inches), flat on one face, so that the section
presents little more than half an oval, was found in the island of
Yell, and is now in the Newcastle Museum.
I have a large heavy celt less tapering at the butt than Fig. 67, 8 1∕2
inches long, 3 1∕2 inches wide, and 2 1∕4 inches thick, said to have
been found at Spalding, Lincolnshire. One of flint (7 inches) nearly
oval in section, and found at Northampton, is in the museum at that
town.
Celts of the same form and character as Fig. 67 are found both in
Ireland and in France.
Fig. 68 shows another variety of this type, which becomes almost
conical at the butt. The original was found near Bridlington, and is
|125| now in my own collection. The material is greenstone. Implements
of this form, but rarely expanding at the edge, are of common
occurrence in that part of Yorkshire. Some of them have been made of
a variety of greenstone liable to decomposition from atmospheric or
other causes, and the celts when found present a surface so excessively
eroded that their form can with difficulty be recognized. In the
Greenwell Collection are celts of the type of Fig. 68, from Willerby,
in the East Riding (6 1∕4 inches and 5 1∕2 inches), and Crambe, in
the North Riding of Yorkshire (6 1∕4 inches), as well as another
(5 3∕4 inches) from Sherburn, Durham. I have one nearly 8 inches long,
from Speeton, near Bridlington, and several (5 1∕2 to 6 inches) from
the Cambridge Fens. The surface of one of them is for the most part
decomposed, but along a vein of harder material the original polish is
preserved.
Mr. F. Spalding has found one (8 inches), with a sideways curve, on the
shore at Walton-on-the-Naze.
[Illustration: Fig. 69.—Lakenheath, Suffolk. 1∕2]
A greenstone celt of this form (8 1∕2 inches) was found at Minley
Manor,[404] Blackwater, Hants.
Public-domain text, read in full here on John Shaqi.
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