The Recumbent Stone Circles of North-East Scotland
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The Recumbent Stone Circles of North-East Scotland . BurW . l A . byH recumbentA stone circle consists circlea of stones of graded tallestheight,in two the often quadrantSW inthe flanking prostratea block. Within circlethe there commonlyis ring-a cairn. SUMMARY recumbene Th a t stone circles (RSCs ScotlanE N f )o d (fi probabl) g1 y derived fro Clave mth a cairns of Inverness which have many features in common with them. The recumbent stone is an Aberdonian innovation. b Other features of RSCs appear to confirm this derivation. primare Th c y are f settlemeno a t lie e eass f Inscth jus o tsouthwardd o t t han s through Correen-Bennachie th towardp eGa s Alford. d Analysi f apparentlo s y early feature e circleth n s independentlsi i s y confirmee th y db archaeological find datede sb than .ca t e Later forms of RSCs are found around the primary areas, particularly to the west and north. The latest stone circles in the region retain only a few of the 'classical' features associated wit theshs i RSCst i e d forman , s that further sout Perthshirhn i e appea 4-Posters a r smald san l six- r eight-stono e circles. f locaa RSC e lar s developmen shod signan w t w f fe influenc o s e from more southerly sources. g Present archaeological evidence does not reveal any RSC much earlier than 1800 BC or later than about 1400 BC. INTRODUCTION Much of the data is derived from F R Coles (1900 to 1907 inclusive) whose detailed descrip- tion pland s an f circleScotlansE o N n si d remai startine nstudyth w ne gy . poinSoman r f fo teo his work was amplified by J Ritchie (1917-20 and 1923). Keiller (1934) published a short paper concerned mainly with RSCs in which he summarised his fieldwork but, regrettably, did not later enlarge this. Early excavations by Dalrymple and others were described by Stuart (1867). More recent investigations have bee Childy nb e (1934 Kilbride-Joned )an s (1935; 1936) onle Th .y other work deptn i RSCn Henshaly ho b s si l (1963, 32-39; 1972,273-76 discusses whicn )i ha e hsh d possible origins and dates. presene Th t pape examination bases i ra n do f seventy-founo r certain RSCs (Appendi) xA BURL RECUMBENE TH : T STONE CIRCLE NORTH-EASF SO T SCOTLAND 57 and eighteen other probable sites (Appendix B). The lists are not exhaustive. Coles and Ritchie proposed many other possible sites which have been lef 'nos a t t unlikelprovens i t i t ybu ' that their THE RECUMBENT STONE CIRCLES OF NORTH-EAST SCOTLAND Fiol inclusion would have advanced this particular stud l unexcavate al thes ya e yar eithed dan r very badly ruined or totally removed. CLAVA CAIRNS AND RSCs Clave Th a cairn f Invernes o sRSCe th f Aberdeed o s an s n shar common ei isolaten na d position around the north-east fringes of the Grampians; megalithic circles with stones graded in height; an interest in the south-west quadrant; ring-cairns; cupmarks; quartz pebbles; and cremation pitd san containing burnt material withi centrae nth l area. Bu differenceo t tw ther e ear s that mus e explaineb t positiva f di e relationshie b o t s pi proved. 58 PROCEEDINGS OF THE SOCIETY, 1969-70 . Positiona of sites Henshall (1963 ) point 20 t ,tha ou s t Clava cairn e low-lyingar s , eve slighn i n t hollows, often ignorin gsligha t knoll immediately adjacent t RSC Ye normalle . ar s stea r spun po yo r with wide views. Certain Clava cairns, however occupo d , y higher situation thesd san e appear centrae th t peripheran i bu lt no l areas where later versions migh expectede b t . Dalcross Mains (Henshall 1963, 374) on a hillock crest with wide views across the Moray Firth; Culduthel (ibid, 372) and Gask (ibid, 378) on slight rises; and Carn Daley (ibid, 367-8) on a hillcrest, are all in prominent positions, the last three being to the south of the main and probably primary Clava area, supportin suggestioe gth n tha choica t f higeo h positions might be a later development. To the north-east of Inverness one could expect to find sites intermediate between the classical Clava forms and the RSCs. Here Clava cairns also sometimes have the higher positions associated with RSCs wels DalcrosA s . a l s Mains ther Eastee ear r Clune (ibid, 387) at 500 ft OD with wide views to north and west; Moyness (ibid, 388) in a flat field but with gooa dnorthe vie th Littld wo t an ; e Urchan gentla n i yyD slopin(ibidO t f 0 ,g 388 45 field t )a . onle Thith ys si cupmarke d Clav aeastware sitth en o outsid e dli maie y eth nma t groui d pan route from Inverness to Aberdeenshire and the heavily cupmarked RSC at Rothiemay, Banff. (References for RSCs are given in the appendices). Even furtheease th t o that r Naire nth n site Uppee sar r Lagmore (ibid, 389-90; Coles 1907, 141-9) and Marionburgh (Henshall 1963, 391) in the Spey valley. The first is in a level position terraca secone th n sharpla buo d n s ei dti an abov y; riverslopine e OD th t f Th . 0 g fiel60 t da positions of these sites are sufficiently similar to RSCs for one to hypothesise that the RSCs of Aberdee tracee b y d nma fro Clave mth a cairns. b. Recumbent stone (pi 7) Thi featura s si e that never appear Clavy an a n sthosi n cairni r e No .site thers si larg y ean e blocking stone of which the recumbent could be a copy. Its origin remains a problem and at presen possibls i t i t et forwar onlpu o yt d several different theories. Atkinson (1962,17-20) suggeste origin d a comparabl a n i e featur t Lyleea s Hill cairn. ,Co Antrim (Evans 1953 , pointin5) , t thagou t apparent Lyles Hill fluted war beed eha n fount a d both Loanhead of Daviot RSC and East Finnercy cairn, Aberdeen. The Lyles Hill cairn-kerb 'recumbent', however, has no close resemblance to the Aberdonian stone circle recumbents and mors ha e affinities wit 'false hth e portals cairnf o ' s like Argyl, KintraB d lan (SimpsowA n 1967); Temple Wood, Argyll (Craw 1930) Auchagallond an ; , Arran (Bryce 1910), cairns geographically close to Ireland and in which all the 'recumbents' are kerbstones unlike those in Aberdeen. These Scottish cairns, however, do appear to be culturally related to the Clava group (Ritchie and Maclaren 1973, 11; Burl 1973, 40) and the discovery of a kerb-cairn at Culcharron, Argyll (Peltenburg 1973) with false portals and a cupmarked prostrate stone at the SSW in a position similar to the supine stones at Kintraw A and at Croft Moraig, Perthshire, increases the possibility that the origin of recumbent stones may lie within the Clava tradition, one version developin Greae footh e f th to t t gGlea Argylln i othee th , Aberdeenshiren ri . Another possible origin may be found in the makers of AOC beakers who entered Aberdeen shortly after 2000 BC, using in particular the R. Don as a port of entry/From present data it appears that bot positioe date broadle hth th ear d nan y coincidental with thos r primarefo y RSCs s noteworthi t I . y thapositioe recumbene th t th f no t stona SSW-NN n eo E n axii s si keeping wit orientatioe hth n preferre thesy db e peopl r theiefo r burials (Clarke 1970 , 455)62 , . associatioe Th rituaa n i l circl recumbena f eo t S-SSe stonth t bees eWa ha n site o notetw s t da outside Scotland where AOC sherds were found, in both cases being added to an existing monu- BURL: THE RECUMBENT STONE CIRCLE NORTH-EASF SO T SCOTLAN9 5 | D ment. At the Sanctuary, Wilts, a concentric stone circle succeeded a free-standing timber structure (Musson 1971, 371). Just outsid innee eth r circle lonthera s (Cunningge wa stoneholW SS e th -t ea 1931n to , pi t n)WoodhengeA . , Wilts sarsea , n 'recumbent' ston addeo s t eS wa df o jus W t timber ring 'B' subsequent to the erection of posts B8 and B9 (Cunnington 1929, 14). At both these sites there were AOC sherds (Clarke 1970, nos 1064F and 1107F). It is notable that at Loanhea f Daviodo potterther C C alss RS eotwa AO conjunction yi n with flat-rimmed ware. An analagous mixture of AOC and Knockadoon II ware was found at the ritual circle of Cashel- bane, Co. Tyrone (Davies and Mullen 1940) with a loose cupmarked stone at the S. juss i t tI possible thamakere th t f thiso s beaker pottery sometimes place recumbenda t stone at the S-SSW within ritual enclosures, perhaps related to the axial orientations of their burials. Certainly the distribution of early RSCs and AOC beakers coincide along the middle reaches of the R. Don in the first quarter of the second millennium. A recumbent stone circle might thus be the result of a fusion of beliefs from different cultures, a hybrid monument, pre- dominantly Clava wit grades hit d stone circle, ring-cair buriald nan customs witt innovae ,bu h th - recumbentioa f no t stone.