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RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • usters of other classes of material. 5 Excavations (EBS85 Tl and T2) Small -scale excavation of earthworks was undertaken in order to begin investigation of the soils and archaeology within field boundaries near sites identified in fieldwalking. As indicated previously, one
  • the large lynchet (Site Tl), and a lm-wide trench, 18m long, across the bank (Site T2). This was done using a JCB, a method that would allow a preview of the stratigraphy . lm-wide trenches were excavated to the side of the machine cuts, and thèse were divided into mètre squares
  • , and the effects of such changes on social groupings and labour patterns. The complète fieldwork programme consists of systematic fieldwalking of ail available ploughed fields within the four communes, together with sélective geophysical and geochemical surveys, and small excavation
  • ; in addition, environmental analysis and a survey of standing buildings is being undertaken. The larger study involves (amongst other éléments) analysis of documents, including the very detailed cadastral maps and records of the early nineteenth century (Asti 1 1 and Davies 1982a, 1982b
  • collection; phosphate analysis and soil magnetic susceptibil ity survey of the four selected areas; and excavation of part of a bank and lynchet near a field from which 'total' collection had previously been made. Three days (21-23 March) were spent in préparation by three people
  • to concentrate upon the excavation. Overall , 434 mandays were spent on this year's season, including travelling time and time off; 364 of thèse were working days. Two of the main team spent most of their time assisting in a survey of standing buildings already in hand when the season started
  • acing slopes. Upland concentrations were less notable than in 1984 (transects H, J, K) with only a quarter lying between the 50m and 75m contours; more than half 1 ay between 25m and 50m (59.9%), as in the other Carentoir transects. Only 35.3% of sites 1 ay within 250m of streams
  • were the subject of more intensive study: four fields (A107, D221, B216, B347) were gridded in 5m squares so that everything on the surface of the fields, including schiste, might be collected. A107 had been classified as a 'possible site', with comparable amounts of médiéval
  • , and rather more variation than did the other fields, with some tendency for lower readings in the area of the brick/tile/Roman cl ustering. A pl atf orm at the north-western edge of the field produced little material of any type; it is likely that this area has been ploughed down
  • useful information. After three days préparation, excavation took place over eight days with a team of nine people, making a total of 52 working days. The weather during this period was appalling, with torrential rain and high winds: one complète day was lost and extremely difficult
  • conditions prevailed on another three. Excavation therefore had to be more limited than was intended. The excavation strategy was similar to that used by Martin Bell to sample lynchets and valley bottoms in the south of England (Bell 1977; 1983). A 2m-wide trench, 14m long, was eut across
  • to facilitate excavation and recording. Soil was excavated using trowels and ail the finds, with the exception of schiste, were three-dimensional ly recorded. Because of the quantities recovered and the lack of time, the schi ste was collected in 5cm spits. The bad weather prevented total
  • excavation of the trenches. In Trench 1 work was concentrated in areas where features had been observed in the machine-cut trench: 64% (9 of the 14 mètre squares) was dug. As no features were seen in the machine trench, alternate squares were excavated in Trench 2 and hence 50% (9
  • and 40cm, as was also true of the other material. The pottery, brick, tile and also this schi ste were probably brought on to the field in the course of manuring. Trench 2. The remains of a bank, only 20cm high, were found lying on the natural, midway along the trench. The bank
  • %). As in Trench 1, there was no apparent zoning of particular fabrics. The quantities of the (non-local) schi ste progressi vely decreased with depth, and the small amount of brick and tile is in striking contrast to that in Trench 1. The excavations are important for demonstrating
  • and tile coul d indicate that this happened before brick and tile were in common use. Both trenches have shown that lynchets could have a complicated history, with their origins in other features. From the point of view of land-use history, the pottery suggests that this area of Ruffiac
  • of évidence suggests intensive cultivation in the late middle âges that was limited in the early modem period with changes in the social status of the 1 andowner and in his method of 1 and management. 8 Envi ronmental , Pottery, Architectural and Language Work, 1984-85 In the course
  • of the last year pollen analysis has been carried out on samples taken during 1984, in particular from buried soils beneath banks in woods near Le Vivier (not far from the excavation site) and Le Rond Point (Carentoir), areas of extensive 1 ande in the early nineteenth century. Although
  • and proposed - as part of an investigation into the application of microscopic techniques to the identification of traces of agricultural and pastoral activities in the soils and sédiments a sustained programme of soil analysis in close association with other field and archive work
  • of phosphate concentrations at the deserted médiéval settlement at Kerlano. This site, partially excavated by M. Patrick André nearly twenty years ago, is located in the granité upland of the Landes de Lanvaux, 30km west of the study area, and is the nearest known surviving médiéval
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • to the cadastral settlement pattern. The excavation method was the same as that used on K446 in 1986 (Asti 11 and Davies 1987, 112-13). A lm-wide trench was eut by machine from the ridge down the slope so that it went through the tile concentration and sectioned the earthworks (T39
  • the second century, or even in the prehi stor i c period, since i t does not respect, any of the? demonstrâbly Roman ditches or pits (see fig. 4). It is, however, différent from other s that have been excavated: the 1 ynchet lacks a ditch or bank at its core, as did Tl , T2, and T35 (see
  • 5, an orange ware, was found in jug and bowl forms. The forms of cooking ware are similar to those found on médiéval sites excavated in the Landes de Lanvaux (André 1974). The most common type of rim (34 examples) is that of the gai etti er e; other open bowl forms were comparati
  • the four communes named above, and sampling of fields in the surrounding communes, together with sélective geophysical and geochemical survey, and smal 1 excavations to test results; compl ementa.ry envi r onmental analysis is al so being undertaken . The fieldwalking programme
  • was completed in 1987, and a survey of ail standing buildings in the core in 1986. The complète study involves (amongst other éléments) analysis of documents, including the very détail ed cadastral maps and records of the early ni neteenth century. Thèse latter analyses have been completed
  • ; the cadastral work allows total reconstruction of the early rà neteenth- century ] andscape and is of parti cul ar value for the fieldwork programme (Asti 11 and Davies 1982, 1983, 1984, 1985, 1986, 1987)." The 1988 season involved sample excavation of parts of seven fields (B409, A92, A31
  • /79, H 132, 874, L26, D153) from which 'total' collection had previously been made (fig. 1). Of thèse, A92 had been started in 1986 and remained to finish. The ai rn of thèse smal 1 excavations was the investigation of surf ace/'sub-surf ace rel at i onshi ps; fields were selected
  • that had provided a wide range of différent surface data so that excavation might produce results that would allow interprétation of the whole mass of surface mater i al. Three days (25 - 27 August) were spent in préparation for the main season by two people, in addition to two spécial
  • . The square T36 was excavated in the same way as H 145 and A92 in 1986: a 5% sample was taken for sieving to check recovery rates and l'iand tools were used (Asti 11 and Davies, 1987). The excavation took 85 working days, with a team of five. Trench 36 The plough soi 1 (1) was excavated
  • ) of introduced stone pink siltstone (K-01M) , Brioverian shale (B2-3) , sandstone (02) and many lumps of fine black siltstone (03-4), of a quality often used for roofing, material which occurs natural ]y about lkm, away (58kg, 317. of stone excavated ) . A layer of yel 1 owi sh-brown sandy
  • loam lay under the plough soil (2). It contai ned little stone by comparison with the plough soil (59kg, as against 188kg) and very little clearly introduced stone (including only 1kg o-f 03-4, 27. o-f stone excavated); there were large amounts o-f charcoal , usually flecks although
  • some pièces were 5mm across. This layer varied in thickness -from 0.75m on the eastern, up-slope, side o-f the trench to 0.38m on the west. At the east end the top sur-face o-f 2 curved as i -f the layer had been mounded up. This layer could not be total ly excavated over the whole
  • at the base of context 2, eut into what looked like a buried soil (32). AI 1 had si mi 1 ar fills of yel 1 owi sh-brown sandy loam with charcoal flecks. On the north side of the trench part of a large pit was excavated (3: lm wide, 0.42m deep > . It had a lower fi II with sliqhtly more
  • fragments. Mear the east section was an oval pit (25: lm x 0.75m and 0.28m deep); the fill again produced no finds (27). Another pit in section (26: fill 28, no finds) had been eut into by a smal 1er pit (7: fill 8). Three intercutting pits were excavated in the centre of the trench
  • with a 2m-hi gh crop on the field meant that. the excavations could not establish the reasons for the médiéval di str i but i on . It is however now clear that in E409, like H80 and K446 before, the occurrence of small quanti ti es of prehistoric mater, i al on the surface of the field
  • was not présent in such quanti ti es. Although the area excavated was so small, it is sufficient to reveal that this zone is of exceptional importance as a long-used settlement area - Iron Age, Roman nearby to the south east, two seigneurial sites hardby (Le Bois Guillaume and La Touche au
  • ZK67) Excavation o-f Trenches 28 and 29, started in 1986, was completed. Thèse two 6m squares were located over a dense tile scatter located by -fieldwalking at 50m intervais in 1982 and rewalked in 5m squares for 'total' collection in 19B6. The fieldwalking data suggested a Roman
  • sett 1 ement . In 1986 the plough soil in T2B
  • material was obtained from T29 (as was reflected by the results D -f the total collection) but more Roman pottery was found. Time ran ont and the sites had to be backfilled at the point, when ditches were recognised (Asti 13. and Davies 1987, 118-21). In 1988 the excavation was resumed
  • and irnplied that p>lough damage was greater than anticipated. 4m of the 6m length of the exposed ditch was excavated: it was steep sided with a fiai, bottom (0.8m deep and 1.3m wide). The ditch sloped down towards the east. It was filied with a silty soil with rounded quartz pebbles
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • and two others, returned on 28 April for three days in order to complète the excavations. Overall, 317 mandays were spent on this year's Easter seasons (303 by the main team), including travelling time and time off 5 255 (244) of thèse were working days. The weather was dreadful
  • . The depth of the plough soil varied between 30 and 50cm and in some places overlay the natural clay subsoil and in others the natural bedrock. No archaeol ogi cal features were encountered ., Trench 11 The plough soil was excavated by hand and found to be between 35 and 45cm deep. It 1
  • days were spent on site, with an average team of 6. The majority of features excavated were sections of ditches. An account. of al 1 thèse would be repetitious; instead the détails are tabulated after a discussion, by trench, of the other contexts. Al I the ditches had been dug
  • reçut (35/50, 37/51). Trench 21 Four ditches were excavated (41, 42, 47, 49), détails of which are given below. The only other feature wais a modem tree hole (46) ". Trench 22 S by 4m was cleared of approx i matel y An irregular area Of plough soil and a deposit of hard stone
  • EAST BRITTANY SURVEY 1986 EAST BRITTANY SURVEY EAST BRITTANY SURVEY EASTER AND SEPTEMBER SEASONS 1986 Easter Season 2 Fi el dwal ki ng at 50m intervais 2 Fi g . A 3 Sampling outside the core 6 7 Fig. B Excavations Al 16 8 Fi g. C 10 September Season Fi g
  • and labour patterns» The complète fieldwork programme consists of systemaitic fieldwalking of ail available ploughed fields within the four core communes of Ruffiac, St-Nicolas, Tré'al and Carentoir, together with sélective geophysical and geochemical surveys, and smal 1 excavations
  • to test results5 complementary envi ronment al analysis is also being undertaken, as is a survey of ail standing buildings in the core. The complète study involves (amongst other éléments) analysis of documents, including the very détail ed cadastral maps and records of the early
  • involved fieldwalking over large areas at wide intervais, as in 1982 85, in the four core communes; sampling in the communes surrounding the core? and excavation of parts of a field from which 'total' collection had previously been made. Two days (21-22 March) were spent in préparation
  • for most of the main season, with considérable rai nf ail; fields were usually in idéal condition for walking and surface collection was not seriously impeded, but it made excavation al most impossible. Conditions for the return visit were much better, allowing the desired program
  • to be completed on the excavation site» Fieldwalking in Runs at 50m intervais (Transect Walking) A. Within the core Fieldwalking over large areas within the four core communes was organised within transects running south/north across them» Transects A (Ruffiac), D, E, 6 (Carentoir), B
  • marked patterns» Such schi stes were présent on most fields (largely as a resuit of manuring), with the exception of some areas of 1 an de in the northern part of Transect B and of some isolated, scattered fields (D6 and 7, E267) with no other surface material. However , it was again
  • contrast black and pink/purple roofing fragments occurred together in zones immediately north of the Ruffiac basin and west of the Trelo zone. It was also possible, in some cases, to distinguish a range of other schi stes that were imported from nearby local sources, probably as walling
  • in the core, and more are on south- (32.7), north(18.47.) and west--facing (12.27.) slopes - again reflecting the h i g h er t op og r ap h y „ Excavations. Al 16 Excavation was designed to sample the medieva\l settlement. of Al 16, located by fieldwalking and classified as a "site
  • features, Work on the excavation was eventually abandoned in the main season because of the rising water table; however, the smal I team that returned in late April was able to complète the trial. Altogether excavationtook place on 8 days, with an average of 6 people per day, thereby
  • absorbing 42 working days. Two 6m squares were excavated (see fig. G), One, T3, was located on the highest part of the field, where surface prospection had identified both large amounts of pottery and concentrations of phosphates (Asti 11 and Davies 1983s 16, 18). The second, T4
  • because of the weather. Quadrats with 6m si des were chosen since a smal 1er cutting could fall within a structure, failing to reveal its existence. However, in the later stages of the excavation a machine (JCB) was used to eut three 1m wide trenches to extend the investigation
  • . The first (T7) ran north west from T3 across a slight break in si ope, and the other two (T5 and T6) were eut in order to section the platform near T4 (see fig. C) . The-? sections were cleaned and drawn and features in the bottom of the trenches recorded. The two 6m squares were mai ni
  • y excavated by hand. The plough soi 1 was removed in 10-20cm spits by shovel s the spoi 1 was searched for finds (including schi ste) on the si de of the excavation. As a control a randomly chosen 60cm square (57. of the main cutting), was removed separately and wet sieved
  • actor which may explain the relatively large amount. of pottery found on the surface by comparison with that recovered by excavation. Quartz and conglomerate blocks °\ EBS 85-86 0 20 40 60m were -found embedded in the sur-face of the naturel schi ste; since several groups
  • from the north-west corner of T4 and eut the edge of the earthwork platform at right angles; the other (T6) was 23m long and ran from the south-east corner of T4 to the southern end of the platform. A section of the whole earthwork was thus obt ai ned . The earliest évidence came
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
RAP02332.pdf (PAIMPONT (35). le Bois Jacob. rapport de fouille programmée annuelle)
  • , des couches, lors d'un rebouchage des excavations minières. 14 2.2. SONDAGE S105 Les premiers niveaux de cette extension vers l'est du sondage sont faits d'un sédiment orange-rouille à marron, légèrement granuleux, la plupart du temps meuble. Côté ouest et à une profondeur
  • (ZR) sous l'humus, et niveau intermédiaire de fouille à 90 cm de profondeur en moyenne. 2. niveaux moyens et comblements des excavations minières. Le comblement montre l'existence de poches ou couches différentiées (fig.10). L'unité stratigraphique principale présente par
  • la datation de ces excavations minières, qui reste pour le moment inconnue. Les questions posées par l'aspect des excavations observées et les interprétations envisagées sont abordées dans la synthèse concernant ces problématiques minières exposées en 4ème partie du rapport. 18
  • ferrugineux et des excavations minières -0.20 -0.30 -0.40 -0.50 -0.60 -0.70 -0.80 -0.90 -2.00 -1.00 -1.10 -1.20 -1.30 -3.00 -1.40 -1.50 4.00-1 -5.001 4.00 -3.00 -2.00 -1.00 0.00 1.00 2.00 Fig. 14: excavation M l - topographie de la partie supérieure de l'ouverture (moitié
  • est). Fig. 15 : excavation M1 - vue 3D de la partie supérieur de l'ouverture (moitié est). Fig. 16 : excavation M1 - coupe stratigraphique N-S. du niveau de creusement vertical. I IL Fig. 18 : Excavation M1 - courbes de niveau à partir du niveau de creusement vertical
  • h e d in de-ionized water, r e m o v i n g associated organic s e d i m e n t s and debris (where present). T h e aterial w a s then crushed/dispersed and repeatedly subjected to H C I etches to eliminate s e c o n d a r y carbonate components. In t h e case of hick shells, the s
  • of pitch/tar contamination, c o n s e r v e d materials. I I l a b o r a t o r y pretreatments w e r e applied. Special requests and p r e - l a b o r a t o r y p r e t r e a t m e n t usually a c c o u n t s for this. I Consistent Accuracy ... Delivered On Time. Beta Analytic Inc
  • 12,000 BP is still being researched and provides somewhat less precise correlation. Beyond that, up to about 20,000 BP, correlation using a modeled curve determined from U/Th measurements on corals is used. This data is still highly subjective. Calibrations are provided up to about
  • taken from the outer portion of a tree that was cut down to produce the sample in the feature dated). For other materials, the maximum and minimum calibrated age ranges given by the computer program are uncertain. The possibility of an "old wood effect" must also be considered
  • (containing balance/credit information and the number of samples submitted within the yearly discount period), and peripheral items to use with future submittals. The final report includes the individual analysis method, the delivery basis, the material type and the individual
  • pretreatments applied. The final report has been sent by mail and e-mail (where available). Pretreatment Pretreatment methods are reported along with each result. All necessary chemical and mechanical pretreatments of the submitted material were applied at the laboratory to isolate
  • the carbon which may best represent the time event of interest. When interpreting the results, it is important to consider the pretreatments. Some samples cannot be fully pretreated, making their 14C ages more subjective than samples which can be fully pretreated. Some materials receive
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
  • Barnenez’s term is associated to the cairn, excavated and restored during the 50-60’s by PierreRoland Giot. It seems isolated now but other adjacent buildings are known and specially a second long tumulus next to the cairn at its north. This work wants to bring to light this monuments
  • Archaeology, 0, 0. Consultable à http://www.jna.unikiel.de/index.php/jna/article/view/34. Laporte L. 2010b : Restauración, reconstrucción y apropiación : evolución de las arquitecturas megalíticas en el oeste de Francia, entre pasado y presente. Restauration, reconstruction, ap- ARPI
  • : Long monument de Barnenez en Plouézoc’h, in Ses- Mounds and Megalithic Origins in Western sion B27 Uispp: Megalithic Biographies: Cycles France: Recent Excavations at Prissé-la- Of Use And Closure, Charrière., Proceedings of the Prehistoric Socie- Laporte L., Joussaume R
RAP01557.pdf (PLOULEC'H (22). le Yaudet. rapport final de synthèse de fouille programmée 1996-1998)
  • CENTRE DE RECHERCHE BRETONNE ET CELTIQUE Université de Bretagne Occidentale INSTITUTE OF ARCHAEOLOGY University of Oxford LE YAUDET EN PLOULEC'H (22) Site muiti-pérlodes Fouille programmée RAPPORT 1996-1998 Patrick GALLIOU, Barry CUNLIFFE Brest, 1998 IS59- FICHE
  • de l'Université de Bretagne Occidentale à Brest, et Barry Cunliffe, de l'Institute of Archaeology de l'Université d'Oxford (GrandeBretagne). Nous avons reçu le soutien financier du Ministère de la Culture, du Conseil Général des Côtes-d'Armor, de la British Academy et de
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
  • , l'établissement de fouilles de grande ampleur sur un site mésolithique du Finistère aurait un effet dynamisant pour la recherche sur cette période, en suscitant de nouvelles problématiques, dans un constant allerretour entre prospections et excavations. 3. Mise en place d'une base de données
  • : grès lustré, 9-11 microquartzite FL). PCR - Le Mésolithique en Bretagne - Rapport 2001 5. Bilan de la campagne 2001 et projets des campagnes 2002-2003 5.1. UN BILAN DES METHODES DE FOUILLE L'exploration d'un site du Mésolithique en un temps limité est perpétuellement confrontée
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • as, Treal and Carentoir, together with sélective geophysical and geochemical surveys, and small excavations to test results; compl ementary envi ronmental analysis is also being undert aken , as is a sùrvey of ail standing buildings in the core. The complète study involves (amongst other
  • predomi nanti y médiéval or predomi nanti y post-medi eval sherds, others more than the necessary minimum proportions of médiéval and post-medi eval sherds, and others had a prédominance of man-made building material. The proportions of such concentrations are as follows, by transect
  • Roman settlements in Missiriac (P) and Comblessac (R) . In Missiriac the scatter associated with the excavated bath-house at Bermagouet continuée! to the west of the excavation for at least 250m (Gallia 1977: 346-7). In Comblessac, a field (R9) , adjacent to the field near Le Mur
  • st i es of the former, was separated from the Ruf f i ac/Carentoir core by the great Bruc 'blank'. Work outside the main season. 19B6—B7 During the past year work has continuée) on other aspects of the project, both field and archivai. Mi cromorphol ogi cal analysis of soi 1
  • samples from the 198é> excavations has been undertaken by Anne Gebhardt, under the supervision of Marie-Agnès Courty. Analysis of pottery fabrics has continuée), the sorting and classification of fabrics from the three 19B6 seasons now being half completed. Further work on local
  • . Future work A team of four will return to the core communes in October-November 1987 to do one final month of 'total collection'. In August and September 1988 we plan an extended season of small-scale excavation in the core, to continue to investigate the relationship between surface
  • provided financial support. G. G. Astill Department of Archaeology University of Reading Whi tekni ghts Reading RG6 2AA Wendy Davies Department of History University Collège London Gower Street London WC1E 6BT 9 July 1987 REFERENCES Astill, G. and Davies, W. 1982 'Un nouveau programme
RAP03312.pdf (CHARTRES-DE-BRETAGNE (35). ZAC des Portes de la Seiche, tranche 1B1. Rapport de fouille)
  • en lien avec les dernières productions potières du début du XXe siècle à Chartres-de-Bretagne. 4 ABSTRACT The excavation located in Chartres-de-Bretagne, ZAC des Portes de la Seiche, have revealed remains from medieval, modern and contemporary period. The main layout is dated
  • century. After their abandonment, the kilns and the entire space were subjected to several phases of fillings between modern and contemporary period. A quarry for extracting clay, located into an ancient pond was partially revealed. It would mesured about 4 000 m². The extraction
  • archéologiques. Il est à noter que l'exploitation des argiles éocènes est mentionnée dans la notice de la carte géologique. En effet, le sous-sol de Chartres-de-Bretagne fut largement exploité dans de nombreuses excavations atteignant ces argiles lourdes et kaoliniques, en vue de leur
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
RAP03187.pdf (QUIBERON (56). Beg er Vil : un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP 2015)
  • Hoedic, également célèbre, est à 22 km pour le même oiseau vers le sud-est, mais un être humain devra prendre une embarcation pour rejoindre ce campement insulaire, aujourd’hui comme au 7ème millénaire avant notre ère. Excavations L’occupation mésolithique de Beg-er-Vil a été
RAP03284.pdf (éléments pour une nouvelle approche de l'âge du Bronze en Bretagne ; le cadre chronologique et les formes de l'habitat. Rapport de PCR 2015)
RAP02769.pdf (ÎLE-DE-MOLÈNE (29). programme archéologique molenais, rapport n°17, beg ar loued : un habitat en pierres s7ches du campaniforme/âge du bronze ancien. rapport de fouille programmée 2011)
  • METHODES ET STRATEGIE DE FOUILLE............................................................. 20 1 – Méthodes mises en oeuvre ......................................................................................... 20 2 – Protocole de tamisage et gestion des refus de tamis
  • Molène à la fin du IIIe millénaire et au début du IIe millénaire avant notre ère, les fouilles cherchent à mettre en évidence aussi bien la chronologie du site, que l'organisation et les phases de construction du bâti. B – METHODES ET STRATEGIE DE FOUILLE 1 – Méthodes mises en oeuvre
RAP01858.pdf (les sites mésolithiques en Bretagne. rapport de 1re année de projet collectif de recherche)
  • l'occupation humaine était limitée à un secteur circonscrit, aujourd'hui détruit. Le tamisage des sédiments de la rive a en revanche permis de rassembler de nombreuses armatures et d'envisager ainsi des études typologiques étendues aux Monts d'Arrée. Les excavations de Kerliézoc ont
  • basées essentiellement sur la robustesse et restent donc, à cause de la variabilité inter et intra populationelles, assez subjectives. Nous utiliserons donc des méthodes plus récentes, apportant des réponses peut-être un peu moins catégoriques mais plus objectives (données métriques