Archaeologia Islandica - 01.01.2006, Qupperneq 34

Archaeologia Islandica - 01.01.2006, Qupperneq 34
Steffen Stummann Hansen and John Sheehan vertical face. At east-southeast an exter- nal veitir abuts the bank and continues down towards north for a distance of about 12 m, and this has resulted in a narrowing of the width of the bank here. A short stretch of well-preserved bank is extant at northeast, but it has been completely removed at north. This was caused when an area, measuring c. 10 m north-south by c.9 m east-west and up to 0.8 m in depth, which incorporated part of the enclosure at north, was dug away. This resulted in a low vertical edge to the site, averaging 0.6 m in height, at this point. No visible trace of the site’s enclosing element is apparent at north- west, though here the line of a curving veitir preserves its probable course. The building is centrally located, approximately, within the enclosure. It is a rectangular structure, with its long axis aligned east-west and with an entrance passageway at west. Internally, it meas- ures 3.6 m east-west by 2.7 m north- south, while externally it has dimensions of 11.4 m east-west by 7.6 m north-south. Its walls, earthen banks furnished with coursed stone-facing internally, stand up to 0.65 m in internal height. Externally, at west, the long sides of the building extend for a further 4.6 m to form its entrance passageway. This averages 1 m in width and there are some indications of stone facing evident on its northern side. There is a large boulder/outcrop of basalt located about 1 m southeast of the building’s corner. It measures 1.6 m by 1 m and features two bored holes. These latter are of recent origin. The North Atlantic context The essential characteristics of the Leir- vík site - a small rectangular structure, oriented east-west, set within a sub-circu- lar enclosure - suggest that it belongs to a group of sites interpreted as chapels. Other examples of sites of this type sur- vive in the Faroe Islands, including those at Bonhúsgarður (English: farm of the prayer-house) in Norðoyri, on the out- skirts of the town of Klaksvík (Hansen, 1980, 150-156; Trap 1968, 306), at B0n- húsgjógv (English: prayer-house ravine) in Famjin on Suðuroy4, at Prestb^toft (English: ruin in the field of the priest) in Oyndarfjorður on Eysturoy (Bruun, 1929, 166; Trap 1968, 294), at Bonhúsflotu (English: the prayer-house at the plain) in Hvalba on the island of Suðuroy5, and at a site in Velbastaður on Streymoy (Fig. 4)6. The bonhús place-name element occurs at approximately thirty other loca- tions in the Faroe Islands, and is always attached to settlements. At a number of these locations there are as yet no archaeo- logical indications to confirm the pres- ence of an ecclesiastical site, but there are no recorded examples of the place-name element being attached to other types of site (Stummann Hansen,forthcomingA). A rather well-preserved bonhús- site is located close to the settlement known as Heiman á, on the island of 4 Nothing is visible on this site today. An aerial photograph, taken in 1968, shows a dark structure which probably reflects half of the sub-circular churchyard wall. This area has a diameter of approximately 20 m. The other half of the enclosure has been eroded away by the sea. 5Pers. com., Oliver S. Thomsen, Tórshavn. According to Thomsen the ruins of the church site could still be seen here in the 1930s. 6 Archives of the National Museum of the Faroe Islands (Sverri Dahl). No local name exists for this site, despite the fact that it is very well preserved. 32
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Archaeologia Islandica

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