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Object type: Part of cross-shaft [1]
Measurements: H. 29 cm (11.5 in); W. 35 cm (13.75 in); D. 19 cm (7.5 in)
Stone type: Pale grey to yellowish grey (10YR 8/1–2) shelly oolitic limestone, a felted mass of small (around 3mm) worn shell fragments, many of them gastropods, with ooliths of a wide size range (0.3 to 0.6mm) and some irregular 1 to 2mm pellets, in a hard calcite ground mass. Upper Lincolnshire Limestone, Inferior Oolite Group, could be Barnack Rag type.
Plate numbers in printed volume: Ills. 376–8
Corpus volume reference: Vol 5 p. 267-268
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Part of a collared shaft of South Kesteven type.
A (broad): The one partially surviving broad face is decorated in low relief on the shaft with what is probably a closed pattern of interlinked oval loops or a run of four-strand interlace; the strands are enriched with an incised medial line and there is a broad plain border. This stops against a projecting collar of the type exemplified by Creeton 1 (Ills. 124–7), standing 1cm proud. It is decorated with a similar broad plain border and a panel filled with a closed-circuit pattern whose precise form is made uncertain by surface damage.
B (narrow): The shaft is decorated by a run of four-strand plait within broad plain borders, the right-hand of which has been largely cut away in recutting the stone for secondary use. The surface of the collar has been recut, thereby removing all decoration.
C (broad): Recut, and now concealed by modern stone.
D (narrow): Recut, but with traces of holes in a regular pattern above the level of the collar, showing the remains of interlace.
This piece has most of the characteristics associated with the South Kesteven group of shafts (Chapter V). It has a section like a grave-marker, i.e. it is about twice as broad as it is deep; it is made of light grey gritty ragstone, which looks like Barnack Rag; it has panels with undecorated rectangular borders, and it has a projecting collar. Its decoration, too, is typical of the group. Fine four-strand plait is found on many of the narrow faces, as at Creeton 1 (Ills. 125, 127); large versions of interlinked oval loops are deployed on Creeton 1 and the Elloe Stone at Moulton (Ills. 176, 178), and the closed-circuit pattern on the collar may be similar to that on the broad face of that cross's collar (Ills. 171–2). Insufficient of this piece survives to offer a closer assessment than the general date-range assigned to the group.
The modern iconic reuse of the stone, with Toft 2b, is especially remarkable (Stocker with Everson 1990, 98; see Ill. 382).