Select a site alphabetically from the choices shown in the box below. Alternatively, browse sculptural examples using the Forward/Back buttons.
Chapters for this volume, along with copies of original in-text images, are available here.
Object type: Fragment
Measurements: L. 36 cm (14.25 in) W. 24 cm (9.5 in) D. Built in
Stone type: Pale pinkish brown (5YR 7–8/3 to 7.5YR 7/4) medium-grained quartzose sandstone, very evenly graded, consisting of closely packed clear quartz grains of 0.3 to 0.4mm diameter, some rounded or subrounded, others angular (with euhedral overgrowth faces?); very porous, but with some pale grey argillaceous material in interstices between quartz grains. (Dr J. Senior confirms as 'Typical reddened Millstone Grit from the junction between the Upper Carboniferous and the overlying Permian strata. Such material was obtained from the River Nidd section near Knaresborough'; as Crowle 1 and Holton le Clay 1.)
Plate numbers in printed volume: Ills. 372–3
Corpus volume reference: Vol 5 p. 265
(There may be more views or larger images available for this item. Click on the thumbnail image to view.)
The stone is decorated in low relief on its only visible face with an interlacing pattern that can now be read with less confidence than when seen and interpreted by Butler (1963–4, fig. 2, no. 8; see Ill. 373). It appears to comprise at one end of the stone a four-strand plait, truncated by the stone's broken end, that is at the point of being transformed into a three- or two-strand plait, and at the other end a fragment of narrower, apparently two-strand plait. In both sections the strands are elaborated with a medial incised line. Between the two sections, four drilled holes may be the bases of the interstices in interlace linking the two, but the pattern itself cannot be made out. Along either edge there seems to be a broad border with no sign of decoration.
In its present worn state, it is not easy to offer a useful interpretation of the form of monument or parallels for its decoration. It might, as hitherto supposed, be the edge of a cross-shaft or alternatively part of a panel of interlace around a plain cross on a flat grave-cover. Its most significant aspect is its stone type, which is alien to Lincolnshire and paralleled in the county only by the shaft, Crowle 1 (Ills. 144–50), and the cover, Holton le Clay 1 (Ill. 203). Like them it originated petrologically near Knaresborough in the West Riding of Yorkshire, but also like them its immediate origin was probably reused Roman masonry from the city of York (cf. Morris 1988; Buckland 1988), perhaps redistributed as finished funerary sculpture. It may indeed be that the breakdown of the interlace from four strands to two within the stone is more akin to the work on the York group of grave-covers (Pattison 1973, pls. XLVIII–XLIX; Lang 1991, 39–40) than to anything comparably accessible to northern Lincolnshire.