80 Proceedings of the Society, 1952-53. an Aisled

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80 Proceedings of the Society, 1952-53. an Aisled 80 PROCEEDINGS OF THE SOCIETY, 1952-53. V. AN AISLED FARMHOUS E ALLASDALETH T EA , ISLE OF BARRA. BY ALISON YOUNG, F.S.A., F.S.A.ScoT. During 1950 and 1951 Sir Lindsay Scott examined the farmhouse at the AUasdale heath f do Barran ei mose th , t southerle y sizth y islan n ean i f do Outer Hebrides; he planned to complete the excavation in 1952. In April of that yea became rh e seriously befor d ill ,an deats ehi Junn hi expressee eh d the wish that the examination of the site should be completed. Her t seemei s tributfittin y wors pa hi Scottisr o kgo fo t et h prehistory. His keen observation and wide outlook won for him a very special place in compane th Scottisf yo h archaeologists. Excavation at the AUasdale in 1953 was made possible by grants from the Society and from the Prehistoric Society. Thanks are due to The MacNeil, the owner of the site, for permission to excavate, and for presenting the finds to the National Museum of Antiquities.1 The site, described by Lindsay Scott as an aisled farmhouse, is built o nknola l of rocky outcro . abovft 0 ep40 sea-level, wher steeple eth y slabbed hil f Coro l a Bheinn characteristio s , e Hebrideath f o c n landscape, flattens int oseriea terracesf so , also typica terraie th f o l. n 1) (PI , V . The farmhouse entrance faces west across one of these terraces towards e nortClian th Be ho e sead T th shelter. e sitth se fro e worsmth f tho te north-westerly e south-wesgalesth o t , Martin Be t n rise abouo st ft. 0 , 80 t and the coastal plain at the foot of these hills is a wide stretch of machar bounded northwards by Greian Head, where there is deep water anchorage, shelvin e soute th th y ho b t gd reefan Seaf so l Bay. The site excavated consists of the farmhouse, with souterrain and kiln- hpuse and an outside working-place, as well as a steading, which included barn and byre, the whole standing in approximately 1^ acres of ground, enclosed by a wall (see fig. 1). The farmstead, known locally as Tigh Talamhanta ("The house under the ground"), was built with the entrance at the highest point of a rocky knoll steeply scarped on three sides. On the fourth, to the east, a gentler incline of gravelly soil overlies schistose rock (figs. 2, 3, 4). The wall footings were lai clay n havclay d o an y,ma e been use filo dt l 1 I am indebted to Miss K. M. Eichardson, P.S.A., and Mr B. Steel, who worked during the 1953 season; also to Mrs E. Steel for her drawing of the final plan of the site (fig. 3). Also to Mr H. H. Coghlan, P.S.A., and Mr A. D. Lacaille, P.S.A., for examining material. AISLED FARMHOUS E ALLASDALETH T EA , ISLE OF BARRA1 8 . TIGH TALAMHANTA, ALLASDALE , Farmhouse1 . PigNo , Souterrain 2 . 1 . , KilNo ;3 . n , OutsidhouseNo ;4 . No ;e working place; No. 5, Steading; No. 6, Later structure. Fig. 2. Conjectured reconstruction of farmhouse. VOL. LXXXVII. TIGH TALAMHANTA j~ Ash o Post holes Uprights FARM WALL HEIGHTENED TO FORM SIDE OF LEAN TO. STEADING Pig. 3. General Plan. AISLED FARMHOUS E ALLASDALETH T EA , ISL BARRAF EO 3 8 . in between stones; this was easily obtainable at various points in the banks nearbo otw f y streams. These burns, risin Corn gi a Bheinn, divergee on , flowing west, drainin fertile gth e Allasdale othee ,th r turning north, providing alike defenc thein ei r marshy margin easiln a d y san accessibl e water supply. The iron present in the soil colours the burns, and the rocky sides are stained wintee th re o dt r high-water mark. e enclosinth n i p g ga wal A •l e nortopenth goon o ho t s d pasture, also towards another farm site, one of a group noted by Lindsay Scott, in this instance lying at a distance of half a mile from Tigh Talamhanta above the steep nort e banth f hko flowing burn. ALLASDALE, BARRA FARM HOUSE TI MM nit mini HITTT HEARTHS DRAIN! BEAT enl .OCCUPATION GRAVEL OVEI CLAY FLOOR SCHISTOSE IS 20 SOUTERRAIN . FigCD . Section4 .d an B sA The Farmhouse. This structure diametern i . ft 6 3 ,s roughl i , y circulae th plann i rd an , souterrain and kilnhouse open from the main building. The paved entrance on the west leads inward from a sill of the natural rock, and the building at this point is much wrecked. Rough steps in the rock lead down the knoll, which is an outcrop of Hebridean gneiss stretching westward from the entrance ove irregulan ra r are morf ao e . thaft Wher 0 n2 e wallin lais dgwa on the natural rock it has greatly collapsed. There were indications of a working platform outsid entrancee eth mera w e no ,rickl f stoneseo a t bu , series of bowl forms recovered from this area suggest a dairy. Pilin againsp gu e a eassofe gneis th s th i t t n schistoso s e rock with 84 PROCEEDINGS OF THE SOCIETY, 1952-53. gravelly covering thin e greateo sth d an ,re farmhous parth f o t builts i e . The surviving wall stands at highest six courses and is built with no apparent sign of batter, well laid and of massive stonework. The outer and inner wall faces, filled with smaller material, have long stones lying athwart, bonding the whole. The choice of building-stone in this locality is poor, nevertheless skil shows li 1 n bot selection hi layinn i d stone gnth an e walling. Phase I. The horizo e Phasth f neo I leve blaca s i l k layer. Thiascribes swa d by Lindsay collapsScote th burnto a t f eo roof covered an , centrae dth l area. It was of varying depth from 4 ins. to a mere powdering of ash over the beaten clay floor of the bays, excepting in Bay 6, where the ash deepened and contained numerous sherds of pottery. At the lowest level many of these cam rathea s e ha fror h t leasma large as e on t e Th storag . 1) r (fig , eja 5 . different characte thihavn y ri sma ebay beed rusan ,f no other ho r material whicn i h storage jars were set. Charcoal from twig willof so wrecordes i d at this point, and suggests that baskets were also used. Cobbling alternates with rough pavine centrath n gi l area, where th e fire was made on the gravelly soil which was reddened and burnt to a depth of 2 ins. The Phase I hearth, roughly oval, was defined on the west by slab paving. This feature was also noted on the west of the barn hearth (PL VI, 2) would an d provid elevea l cooking place r baking r potsth fo efo o r o T , . southeaa y stonelesf pho la s clay, unburnt. Roughl t stoneyse s limie th t hearth on the east. Large charred fragments identified as spruce, presumably from a log of drift timber,2 were recovered from and around a post-hole. Two smaller post-holes on either side of the original hearth indicate a wooden structure firse th t n phasei . Stone-built piers, set radially, formed the foundations of roof supports. Of these, seven remain; originally there must have been nine survivine th , g piers, also lai clayn do , showing sign rebuild.f so baye Th s 3forme thesy db e radials were fenced toward centrae sth l are kerbingy a b slippe e On .d corbel- stone originally joinin outee gth e rth radiae wallins th wa d l6 g piean . rno sole remaining evidence of the method of roofing employed, with the excep- tion of heather charcoal identified in samples from the black level overlying the earnest occupation. Lindsay Scott was of the opinion that the roofing techniqu similas ewa thao rt t indicate t Clettraval,da wherd wallan e eth s are built free-standing as in the 4 AUasdale farmhouse, this is the simplest method of roofing where timber is scarce. He also postulated an overall 1 See plan (fig. 3). "Drift Timber in the West," Antiquity, XXV (1951), 151-3. 2 scraA 3 metalf po , perhap fragmene sth broocha f o e tbasfouns th f Pie wa ,eo t da (ser4 , e 1 fig , 9 . Appendid an . xB) ' P.P.S., xiv (1948), 53. AISLED FARMHOUS E ALLASDALETH T EA , ISL BARRAF EO 5 8 . 43 86 PROCEEDING E SOCIETYTH F O S , 1952-53. roof of thatch or turf to carry rain-water down to the outer walling, and from the charcoal identified as heather twigs we may deduce thatching. The skin tent roofing recently suggested by Mr T. C. Lethbridge for his Kilpheder site,1 wher walle eth s wer t free-standineno t backegbu d against the sand, would be impracticable on an exposed site such as Tigh Talamhanta, where howeve e outeth r r wallin s capablgwa f carryineo e weighgth a f o t roof. A recess r walo , l chamber, opening fro interioe mth s Phasn i r wa eI entered by a doorstep 21 ins. in length, which indicates that the original floor-level of this feature was higher than the interior of the main building.
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