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RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • ) was si ted in the north-east part of the field where there was a coïncidence of pre— medi eval and médiéval pottery. A test pi t (T37) was also dug in the south west , over a squar e wh i c h had produced n o t. a b 1 e qu ant i t i e s of pre- medi eval pottery and brick and tile
  • 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
  • charcoal (16) and smail 1 fragments of mudstone; this produced two smal 1 and abraded sherds of Iron-Age pottery (Fabric 86); the upper fill (15) had no finds. Another pit was also found in the north section (22: lm wide, 0.42m deep) whose fill (23) had no finds but more mudstone
  • the proximity of the Roman buildings. The si des and bottom of the trenches were cleaned manually. Ihe extent of the trenches was limited by the track and modem drainage pipes. T42 was eut from the north-west corner of T28 due west for a 1 distance of 9m; T43 was eut due north from
  • the same corner and was 4.5m long; T44 was eut north from the north-east corner of T28 for 4.4m (fig. 3). In T42 two ditches were located eut into the natural . One (24) was lm wide and about 0.2m deep and was fi lied with a loam (23) similar to the plough soil. The other (39) was much
  • probabil ity the same one, at the north end of both trenches. The ditch (27 in T43, 35 in T44) was 0.7m wide and 0.3m deep and was fill ed with a silty clay which produced no finds (28 in T43, 33 and 34 in T44) . This ditch appear s to have been a drainage ditch for the track which
  • marks the north b oun d ar y of t h e field. None of the trenches produced structural évidence though the plough soil contai ned large blocks of stone which were cl early derived from a building. It is qui te possible that the buildings were located right. on the ridge, and therefore
  • underneath the présent track. Trench 29 The plough soil s (3 and 4) were removed to the level that was reached at the end of the? 1986 season. A modem pit (7 and 8) was rel ocated aïs was ai ditch (5) in the north of the trench. A shallow and i rr egular modem trench was also found (18
  • and was destroyed or collap>sed in the second century, with no subséquent occupation of that parti cul ar site. A31/79 (Ru-ffiac ZN 119) A3 1/79 is situated 4 00m north of Petit Madou in Ruffiac; it stretches from the crest of a ridge on the 40m contour down the north-east slope of a small
  • ) . At a later stage two further trenches were eut mechanically 30m either side of T39 (T40 to the south, T41 to the north). The sides of the trenches were cleaned by hand and recorded; the lowest part of the plough soil and features were excavated by hand. In one case T39 was extended (T46
  • soil varied from 0.15m on the top of the ridge (the south-west end of T40) to 0.4m at the north-east, down-slope, end. The plough soil (57, 78) overlay the natural clay subsoil (79), into which features had been eut. The shallowness of the plough soil and regular ploughing probably
  • to run east-west and it had been reçut, for' ditch 3 had removed the north side. The reçut ditch had a similar profile, was 0.6m wide and 0.4m deep. It contained an A31/79 Roman poMery f f Brick and tile o o o o OOOO O o 00 o o O o o 00 00 TV o o o 000 00 000 00 00 o o
  • by plough soi 1 1, context 25 itself being similar to plough soi 1 2. No further ditches or pits were located beyond ditch 24, but 5rn to the north a layer of dark loarn was found i nterposed between the clay subsoil and the lower plough soi 1 (2). This layer (4) extended for about 25m
  • and reached a maximum depth of 0.35m: this point corresponded with the break in slope. No finds were recovered from layer 4. The only other feature located in T39 was 18m from the north end of the trench and was a shal 1 ow-si ded 'ditch' 0.15m deep (5). It had an irregular profile
  • of pasture north of H132, in order to investigate the farmer's report of large blocks of stone coming from the area. It had eighteenth- and ni netee^nth-centur y pottery in the ploughsoil, but neither structures nor features were revealed. The square was excavated in the same way as B409
  • : diameter lm, filled with 37) and a ditch, perhaps a drain, which ran diagonally across T32 (32: 0.8m wide, filled with 34); at its north-west end i t. was shallow and f 1 at-bottomed , but at the south east it had become deeper and had a 'V' shaped profile (fig. 6). Fi ve other post
  • , for the post holes were sealed by a 'buried soi 1 ' (20, 29) which in places in T38 had a corrugated surface; in parts of T38 this soi 1 was deeper and may have had two horizons, 45 below 29. In the north part of T32 a lityer of soil and quartz (18) was laid on the buried soil and on top
  • of the reniai ning courses of thèse walls contrasted strongly with that of wall 9/17 to the north. Extremely large blocks of quartz and altered schi ste (over 25kg each) formed the base; the remaining 348kg comprised 24% soft Brioverian shale, 39% altered 3L\ schi ste , 27% quartz, 67
  • ). There is subsequently clear évidence for the western extension of the building. A shallow cut (22 and 26) was made north of the main wall, which may have been to allow the original and extension walls to be bonded. The main wall was extended west , a trench being packed with shale as a bedding (52
  • , including whole siltstone slates ('spotted slate': K-OIM) and fragments of the weight of 35 whole slates - it might wel 1 represent roof collapse in situ. The area north of wall 7/51 was then (or already) spread with the residue of wall 9/17, making a layer of compact stone some 25cm
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • for walking. The season was therefore especially productive. Fieldwalking in Runs at 50m intervais (Transect Walking) Fieldwalking over large areas was organised within transects running south/north across the communes. L (in Ruffiac), the only transect not yet walked, was completed
  • and two adjacent transects in Carentoir (F and C), which had been inadequately covered in 1983 because of the height of the crop, were rewalked; F included the cadastral and modem village of Carentoir (see fig. 1). Except for a small area in the north of C, and for fields previously
  • , concentrations of surface material were most frequently found in the basin to the south of Ruffiac village (the centre of L) and in the nei ghbourhood of Trignac, in the north of Carentoir commune (F); however, sites were common throughout the southern halves of F and C, particularly
  • in the Coet Morel /Hôtel Orl and area (Carentoir). Surface material is markedly absent from fields on the northern and southern boundaries of L, on the east/west ridges (particularly on a band north west of Carentoir) and - as might be expected - on most steep slopes. There are again
  • was recorded, the field being the same size and shape as at présent but divided into bandes; an area of 1 ande lay to the north and the nearest settlement (La Boulardaie) lay 130m away. Pottery, building material and schi ste were collected from an area of 1 hectare, distributed ail over
  • ity readings did not vary much, but although médiéval and post-medieval pottery were gênerai ly distributed over the field, both Roman wares and brick and tile cl ustered in the north-west quarter. Although quantities of Roman pottery were small, those of brick and tile were
  • unusually large, and their distribution, together with the nature of the assemblage, suggests that the field once contained a Roman-period structure. Médiéval and post-medieval pottery, by contrast, probably arrived as a resuit of manuring. B216 lies on a slight north-west si ope at 65m
  • of brick and tile (50.82g). The assemblage included second-century Roman wares, fifteen fragments of tegul a and one of imbrex. Médiéval and post-medieval pottery were gênerai 1 y distributed over the field but both Roman pottery and brick and tile cl ustered in the north-eastern third
  • , 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
  • , at least during the médiéval period (Astill and Davies 1984a: 20). A116 lies to the north of Ruffiac, between Coetion and Le Vivier. It is located in a small damp valley bottom, on a north-facing si ope, at 70m. At least one platform can be seen. To the north of the field, in the lowest
  • farms) of La Touche Gourelle, Bas Coetion, Ruis, Gayon, and Le Vivier. The surroundings of the château seem to have been deliberately landscaped with long, straight, tree-lined approach roads, copses and a fish pond, and the farms are surrounded by the large rectangul ar blocks
  • of the 18 mètre squares) was dug. Soil samples for micromorphol ogical and pollen analysis were taken in columns from the sections, using purpose-made meta! containers. Small test holes were also eut by machine at every 15m to the north of Trench 1 (up the side of the south-facing valley
  • ) in order to record the depth of the subsoil (see fig. 2). Trench 1. A shallow ditch was located, eut into the subsoil and natural schi ste. It had a slightly sloping bottom (33cm wide) and was situated 5m north of the crest of the présent lynchet; the ditch was on approximatel y
  • ploughing of the field to the north, at least during the médiéval period (see fig. 3). The trial holes up the slope to the north of Trench 1 showed that the subsoil occurred at a shallow depth (about 30cm), in contrast to that recorded at the north end of Trench 1 (lm), and at the crest
RAP03864 (PORT-LOUIS (56). Citadelle-bastion Desmouriers. Rapport de diagnostic)
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • and also zones that tend to produce more or less of a surface scatter» Surface material is usually markedly absent from areas near the commune boundaries and is also difficult to find in the fields to the north of Qui 1 vain and around Le? Bois Faux; si gni f i cant 1 y , the more
  • possible to see zoning in the présence of thèse schi stes» hence, only black schi stes occurred throughout the ^Ruffiac basin (from Lodineu to Ville Robert and south to La Rivière) and also in a large zone in the north of Transects D and E (from Trelo to La Touche du Mur); in strong
  • 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
  • , transects within the core. Ail available fields Transect for we>re covered; tl 11s ran 10km slightly west of N of from the north-west Ruffiac, and passed north , boundary communes of Carc , Reminiac and Augan the and into the through south oi Zampefrieac, running just to the w est
  • of Augan commune centre, Here there was a marked change in topography - as the and in modem land management — as we moved also in the bedroc north 5 it was with steeper rnuch higher hi 1 1 s and some north/south valleys; but farms (and often fiel ds and houses) were biqger
  • Bonneraye/Le Printemps/Saint-Nicolas (Reminiac) area and in the area around ^the château of Touraille, stretching north from it over the? Campeneac commune boundary to La Tieulais; and there are a di sti net i ve number of 1 ow concentrations of post-medi eval material in the Les PI aci
  • eux to Ville Glâird area. There are large 'blank' zones from La Ravraie to Le Boulay and also north west of Augan, although such zones are not so character i st i c of the commune boundaries as they are in the core communes. Se h i stes in gênerai re-f lect the pinker colour
  • 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
  • . 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
  • of blocks of a similar character were noted in the machine trenches, widely dispersed over the field, they could be natural features» T7, a 13m~long, lm--wide, north-west extension to T3, located a shallow ditch eut into the natural. It had a sloping bottom (50 cm wide) and was fi lied
  • 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
  • of the settlement of Quoiqueneuc in Treal , in the area of a smal 1 n i nth-cent ury monastery. The field is bounded to the north by the main east-west road leading to Quoiqueneuc, and to the west by the road to Le Passai r. The ancien cadastre shows H145 to have been within an area of largely
  • not reveal were any f eat ures ., Trench 12 The trench was excavated by machine and -for most of its 28m length merely provided a record of the depth of plough soil» However in its extrême north end a section of stone walling was excavated- The wall, 30cm high, consisted of coursed
  • blocks of schi s te and conglomérats which were bonded with a thin yellow clay. it was 80— 90cm thick and was laid directly on to a compactée! plough soil (8). Butted on to the north face of the wall was a dense layer of smal I (15—20cm in diameter) pièces of shale and sandstone
  • presurnabl y some kind of hardstanding or floor (9) « The northern extent of the standing was established by augering and was found to peter out some three mètres north of the wall. The eastern extent. of the wall was similarly established and found to end 1 » 2m from T12, with no sign
  • , 11?/» quartzite and 6% qres) . The area appears ta have been devoted to rubbish disposai during the médiéval period; it is possible that the pit, or perhaps tree hole, was filled with mater i al from a building. Comment The results of thèse excavations are extremely usef ul
  • sel f . K446 (Ruffiac ZA106) Ruf f i ac K446 is si tuât ed on the eastern outskirts of Becul eu 1 n
  • of non-local qres and quartzite fragments. The fill was homogeneous and produced 3 médiéval and 7 Iron Age sherds. At the north end of T24, where the greatest depth of plough soil had sealed some shallow features eut into the natural, were located two small gulleys (49, 52/53), whose
  • by the time the macadam road surface had been laid over it. The ditch may have acted as a drain or boundary for the holloway. T26 was eut to the north west of T23 to check that thèse features constituted a road: the same séquence of levels was recorded. Comment The résulte of thèse limited
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
  • Mésolithique final, ce qui va à rencontre des modèles dominants en Europe où la recherche de bonne matière s'intensifie. Stéphane Blanchet présente le site de la Croix-Audran à Carnac, qui a fait l'objet d'un premier diagnostic en septembre 2000 et devrait être fouillé en sauvetage à l'été
  • travaille sur les processus de néolithisation en Europe de l'Ouest et notamment sur les changements dans la diète des populations révélés par l'analyse des isotopes stables d'ossements humains. Ses analyses ont porté sur Téviec et Hoëdic et doivent continuer, tant au Musée de Carnac qu'à
  • entend étudier les différences morphologiques et les caractères discrets non pathologiques, d'origine génétique. On peut signaler, comme complément d'information, que Laurent Courtois commence une thèse sur l'ADN des populations mésolithiques en Europe, avec évidemment une attention
  • particulière aux individus de Téviec et Hoëdic. Anne Tresset étudie l'arrivée des taxons domestiques de mammifères en Europe occidentale. Elle propose un panorama de cette question, de la Bretagne à l'Irlande aux 6 ème et 5 ème millénaires avant J.-C. Ses travaux sur Beg-er-Vil et Beg
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
  • les contours d’un site désormais considéré en Europe comme une référence pour comprendre les sociétés de la fin du 7ème millénaire avant notre ère. Il a fait l’objet de fouilles entre 2012 et 2018 sous la direction de Grégor Marchand et Catherine Dupont. Des fosses, des foyers de
  • , interprétation que les analyses fauniques ou les structures domestiques corroborent sans peine. La monotonie des types d’armature et l’intervalle de datation étroit font de Beg-er-Vil une référence exceptionnelle pour le second Mésolithique en Europe atlantique. L’habitat de Beg-er-Vil est
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)
RAP03185.pdf ((22)(29)(35)(56). Les premiers peuplements de l'ouest de la France : dépôts pléistocènes et occupations paléolithiques de la région Bretagne. Rapport de PCR)
  • of the Palaeolithic landscape at the western most tip of continental Europe: The shoreline seen by the Menez-Dregan dwellers. Environmental Archaeology, sous presse. MONNIER J.-L., RAVON A.-L., 2015 - Terra Amata et Menez-Dregan. Des industries du Paléolithique inférieur à rares bifaces et riches
  • , Quaternary International, RAVON A.-L., GAILLARD C., MONNIER J.-L., 2015 - Menez-Dregan (Plouhinec, Far Western Europe): the lithic industry from layer 7 and its Acheulian components, Quaternary International, sous presse. 5.2
  • /03/2015 : RAVON A.-L. & LAFORGE M., “Presentation of a new regional project: The first human settlements in North-Western France: pleistocene deposits and palaeolithic occupations in the Brittany region”, Jersey Research Meeting, Institute of Archaeology, Londres. 02/04/2015
  • of the La Manche region”, Workshop Pathways to Ancient Britain, Queen Mary University, Londres. 24-26/06/2015 : NAUDINOT N., LE GOFFIC M., BEYRIES S., BELLOT-GURLET L., BOURDIER C., JACQUIER J. et LAFORGE M. - Du nouveau à l'Ouest : l'abri sous roche du Rocher de l'Impératrice
  • de glace » du musée de Jersey Le Musée de Jersey organise une exposition intitulée « Jersey : Ice Age Island » à St Helier du 25 octobre 2015 au 31 décembre 2016. Cette exposition s’inscrit dans la lignée de celle organisée au Museum d’Histoire Naturelle à Londres, « Britain : One
Les premier peuplements de l’ouest de la France : dépôts pléistocènes et occupations paléolithiques de la région Bretagne (2018) (Les premier peuplements de l’ouest de la France : dépôts pléistocènes et occupations paléolithiques de la région Bretagne. Rapport de PCR 2018)
  • Plouhinec, Finistère - L'AMARAI – Association Manche-Atlantique pour la Recherche Archéologique dans les Îles - La Fondation Fyssen - The British Museum, Department Britain, Europe & Prehistory 3 Rapport final d’opération 2018 – PCR Paléo Bretagne 4 Rapport final d’opération 2018
  • contactent tout au long de l’année, mais nous n’avons pour l’instant pas entamé de collaboration avec tous. 19 Rapport final d’opération 2018 – PCR Paléo Bretagne Nom RAVON Anne-Lyse Spécialité Archéologie Rattachement paléolithique, étude The British Museum, Department Britain
  • , Europe & Prehistory lithique UMR 6566 CReAAH – Laboratoire Archéosciences Rennes LAFORGE Marine Géoarchéologie ÉVEHA – UMR 6566 CReAAH AOUSTIN David Palynologie UMR 6566 CReAAH – Laboratoire Archéosciences Rennes BAHAIN Jean-Jacques Datation ESR-U/Th BATES Martin
RAP01858.pdf (les sites mésolithiques en Bretagne. rapport de 1re année de projet collectif de recherche)
RAP01557.pdf (PLOULEC'H (22). le Yaudet. rapport final de synthèse de fouille programmée 1996-1998)
RAP03364.pdf (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport de FP 2014-2016)
  • are also essential at a greater scale since Early Azilian art is extremely rare in Europe. This discovery allows developing our research to another part of the Early Azilian socio-economic system. By their thematic and their formal codes, these engravings are firmly in the tradition
  • and symbolic changes during the Azilian. The Rocher de l’Impératrice rock shelter is an unavoidable site for the understanding of Northwestern Europe Lateglacial societies. Because of the diversity of the archaeological evidences this site allows to develop a global thought about the nature
RAP02521.pdf (MOLÈNE (29). beg ar loued : un habitat en pierres sèches campaniformes, âge du bronze ancien. rapport final de fouille programmée 2007-2009)
RAP03231.pdf (CAUDAN (56). ZAC de Lenn Sec'h, lot 1 : une succession d'édifices circulaires ; un hameau du Bronze final. Rapport de fouille)
RAP02397.pdf (PLOUHINEC (29). Menez-Dregan I. rapport final de fp 2006-2008)