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RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • place between 21 March and 13 April in the communes of Ruffiac, Tréal , St-Nicol as-du-Tertre and Carentoir in the Morbihan in eastern Brittany. The aim of the study is to détermine when, how and why the exploitation of the environment changed direction within the historic period
  • 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
  • EAST BRITTANY SURVEY: QUST-VILAINE UATERSHED REPORT ON FIELDWORK IN MARCH-APRIL 1985 The fourth season in a programme of fieldwork, itself part of a larger, multi-discipl inary study of the rel ati onshi p between land-use and seulement during the last two thousand years, took
  • ; 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
  • 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
  • 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
  • contour in a flat area. In the early nineteenth century it 1 ay on a track and was part of a block of arable in the ' château landscape' associated with La Meule, 125m to the west (a landscape where seigneurial 1 and management introduced distinctive rectangular field shapes, greater
  • 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
  • in an area that was extensive 1 ande in the early nineteenth century. Previously, there was little to suggest that it was cultivated before the twentieth century and it is clearly in a zone that was marginal for most of the historic period: the nearest settlement (La Bridelaie) is 500m
  • part of the valley, is an area of permanent pasture in which there is a prominent bank and a possible platform (see fig. 2). The bank runs diagonally across the valley bottom. 130m to the west of this bank, at the bottom of the south-facing slope of the valley, is a pronounced
  • body of the lynchet and lay immediately below the modem plough soil. The loam and the plough soil produced 112 pièces of brick/tile and 92 sherds of pottery. Most of the pottery was of fabric 1 (64%), the most common médiéval type found in surface collections throughout the study
  • not look profitable to pursue this work in the near future. The preliminary stages of analysis of the pedology and sedimentol ogy of the soils have been initiated. Dr Marie-Agnès Courty and M. N. Fedoroff, with their assistant Anne Gebhardt, visited the study area during the season
  • in the area. Samples were taken from Trench 1 and Trench 2; more will be taken during the summer; and micromorphological analysis will begin in September. The samples taken from 'total' collection sites in 1984 for phosphate analysis have ail been processed and a study was made
  • from the fields of the study area, and to pursue the problem of surface scatter arising from middens, it was decided to investigate phosphate and magnetic susceptibil ity readings from this known settlement with its known pattern of rubbish disposai. In December 1984 soil samples
  • of the building, especially inside and immediately outside its walls, there were higher levels of 26-37 Si/kg and 200-300ppm. The experiment suggests that we might expect structures and middens in the study area to produce relatively high levels. Pottery from the 1984 season has been sorted
  • produced an archeomagnetic date of 895-945 AD. A survey of ail standing buildings has been in progress in the study area since October 1984, undertaken by Pete Addison, working as a fui 1 -time research assistant. To date, 4000 buildings have been recorded on standardised recording
  • and hal 1 . Local pronunci ation material collected while fieldwalking has again suggested that the influence of the vernacular language is évident in scattered parts of the study area; initial stress on Trignac and Kerhal , for example, are notable. Pi scussi on The 1985 season
  • of Trignac and on the western outskirts of Carentoir village, a striking contrast with that collected around Treal centre in 1984 (Astill and Davies 1984c: 56). In fact, the combination of material again suggests that modem settlements generate little scatter and that - in this study area
  • of the local schi stes. The problem is a simple one: because of outcrops and deep ploughing, fields more often than not have a surface scatter of freshly broken and/or abraded schi ste; schiste is also the most common building material in use in the study area between the seventeenth
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • EAST BRITTANY SURVEY 1987 PU EAST BRITTANY SURVEY - OUST/VILAINE WATERSHED EASTER 1987 The seventh season in a programme of fieldwork, itself part of a larger, mul ti -di sci pl i nary study of the relationship between 1 and-use and settlement during the last two thousand
  • years, took place from 20 March - 4 April in the communes surrounding Ruffiac, Treal , St-Ni col as-du-Tertre and Carentoir, in the departments of Morbihan and 1 1 1 e-et-Vi 1 ai ne in eastern Brittany. The aim of the study is to détermine when, how and why the exploitation
  • of the environment changed direction within the historic period, 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 core communes of Ruffiac, St-Ni col
  • 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
  • ) Sampling was organized in three 2km transects radiating from the core (P, M and R) and thèse were wal ked in the same way as Transects A to L within the core and Transect N outside it, in 1982-6. Transect P ran due west to the River Oust for 4.1km from the western boundary of Ruffiac
  • ' areas in which nothing - or virtually nothing - can be found on the surface. It looks as if thèse 'blanks' are fields on land not cultivated in the historic period until the twentieth century; sometimes they are in areas clearly utilized as woodland until very recently. In P
  • two groups of 'blank' fields south east and south west of Comblessac. Together thèse zones suggest that the settlement of Comblessac and its immediately dépendent arable may have been rather small, much smaller than the centres in the core communes: it is notable that a tile
  • . Thereafter, although there are a few 'blank' fields in the nei ghbourhood of Pipriac it is again marked that there are very few from Pipriac east to the Vilaine. The contrast between this area and that to the west of it is very striking. The distribution of material in relation
  • . In P concentrations tended to lie on south-, south-eastor south-west—f aci ng slopes (48.17.) or on those facing west. (11.17.) - south-west especially; i n M they tended to lie on north-, north-east-or north-west-f aci ng slopes (36.97.) or, southand sDuth-west-f aci ng slopes
  • significant. In Transect P there are none of thèse materials on the high ground west of Ruffiac boundary, precisely in those areas which produced no surface pottery either; there are also no pink schi stes in and around Malestroit and close to the River Oust. In Transect M there are none
  • Emailleries. It seems highly likely that most of this transect, beyond its western parts, lay beyond the normal area of distribution of this material, whose source we have recently localized to quarries immediately south west of Guer. In Transect R there were no 'roofing' schi stes
  • 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
  • at the heart of the study area lie in a discrète zone of settlement and exploitation that does not occupy the whole of the Oust/Vilaine watershed. This zone did not extend to the Vilaine; a comparable zone, which did run to the Vilaine, and which shared many though not ail of the characteri
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • (Carentoir YK5) Fig. 9 Fig. 10 General Comment Acknowl edgements Références SEASQN 1988 EAST BRITTANY SURVEY - OUST/ VILAINE WATERSHED SEPTEMBER 1988 The eighth and 1 ast season in a programme of fieldwork, itself part of a larger, mul ti -di sci pl i nary study
  • of the relationship between land-use and settlement during the 1 ast two thousand years, took place from 25 August - 1 October in the communes of Ruffiac, Tréal , St-Ni col as-du-Tertre and Carentoir, in the department of Morbihan in eastern Brittany. The ai m of the study is to détermine when
  • , how and why the exploitation of the environment changed direction within the historic period, 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
  • 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
  • , and only two days were lost because of rain; however , the gênerai dryness meant that the ground was hard and made for very heavy working. EBS 88 B409 (Carentoir Zft 161) B409 lies on a west-facing si ope near the settlement of Le Eiois Guillaume, documentée! from the eighteenth
  • ) 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
  • 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
  • 2 and to the présent ground surface, that is it occurred at a higher level in the west end of T36 and sloped down to the east. It was on this surface that a spindle whorl of soft brown-yellow mudstone was found. Trench 37 The plough soil (13) was removed in three 0.1m spits
  • of charcoal would suggest a quick and deliberate backfill of this ditch. There was, however, a patch of charcoal (20) in the upper part of 16 at the west end of the ditch. No pottery was recovered from the upper fill but in context 17 were a near-compl ete terra-ni qra bowl with a foot
  • 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
  • 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
  • -west end of the trench) there was a collection of ditches and a pit, ail of which were filled with loam similar to the plough soil (2). The trench eut a ditch very obliquely: it was 0.5m deep and at least 0.6m wide and had a 'U' shaped profile (64: filled with 63). It appeared
  • 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
  • of the plough soi 1 (47, 48) varied -from 0.15m at its south-west end to 0.46m at the bottom of the slope. As with the other trenches, ail -features were eut into the natural clay subsoil (28) and had fills that seemed to be derived -from the pl ough soi 1 . The southern part o-f the trench
  • in the opposite direction, farther west along the ridge; in that case the pits would lie in a zone between the residential area and the fields. The sherd of glass and that of (?) amphora might suggest a settlement with wealthy occupants. Ail this suggests that much of field A31 /79
  • the cluster of squares with much médiéval pottery and the stone scatter. When it became clear that structural évidence survived, the area was extended as far as the eut maize would allow to the south and south west (T38) . A test pit (T31) was also dug 15m east of the château in a field
  • : 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
  • ). 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
  • , 28), and the upper courses of the main wall were also removed leaving some remains of the rubble core (6, 13). The whole area south of wall 7/51 was then spread with debr i s-packed layers - 11/25 in the west and 5 in the east; context 5 had a high proportion of roofing material
  • that has only rarely been found in our study area, was found in a destruction deposit (10), in a twelfthor thi rteenth-century rim form. Comment This small area, within 100m of the standing château, was clearly the site of several earlier structures. The séquence involved at least one
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • Chapelle Gaceline, Caro, Reminiac, Augan and Campélieac in the Morbihan in eastern E
  • of fieldwork, itself part of a larger, mul t i -di sci pl i nary study of the relationship between land-u.se and settlement during the last two thousand years, took place from 21 March - 5 April and 6 -- 27 September in the communes of Ruffiac, Treal, St~Ni col as-du-Tertre , Carentoir, La
  • 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
  • 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
  • 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
  • and fairly even distribution of médiéval and post-medi eval pottery. Although there were areas of slightly higher concentration, the scatter looked like a manuring scatter.. H145 is a flat field that is located near the crest of an exposed south-facing ridge on the south--west edge
  • 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
  • (from east to west s T23 , T24 , Iron Age pottery could be T25) , suc h that the areas producing of the trenches were cleaned by hand and tested. The si des part of the plough soil was excavated by recorded; the lowest features located thereby. The trenches were hand, as were
  • 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
  • the first trench was placed over one of the 'concentrations' of Iron Age pottery. Initial ly ai 6m square (T15) was excavated as at Al 16, A92 and H145, and then five trenches (1 mètre wide) were eut north-south across the field at 30m intervais using a machine (from west to east. T16/17
  • , they are of a size and shape more typical of Roman sites; this impression requires confirmation after a wider study of comparative material» While T15 and T16 have produced settlement data, it is more difficult to interpret the features in the other trenches» Some (e.g. 56, 48, 64) resuit from
  • activities taking place within small enclosures beyond the residential area» One possible interprétation of H80, then, is that it was the site of a late prehistoric settlement, the focus of which lay in the west of HSO and beyond it, with associated enclosures to the east » A92
RAP01574.pdf (SAINT-VOUGAY (29). le château de Kerjean - esplanade nord. rapport intermédiaire de fouille programmée 1998-1999)
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)
  • historiques / The islands of Brittany (France): an archaeological, geographical and historical point of view. Actes du Séminaire Archéologique de l’Ouest, Rennes, 1er avril 2014, BAR International Series 2705, Oxford: Archaeopress, pp. 1-13. LAFORGE M., BAHAIN J.-J., MONNIER J.-L., en prep
  • – Communications 11/02/2015 : RAVON A.-L., “The Lower Palaeolithic in Brittany : between Acheulean and Colombanian”, Lithic Studies Society, Franks House, Département de Préhistoire du British Museum. 18/02/2015 : RAVON A.-L., “The Lower Palaeolithic in Brittany : between Acheulean
  • , Université Michel de Montaigne Bordeaux 3, 88 p. - BAHAIN J.-J., FALGUERES Ch., LAURENT M., SHAO Q., DOLO J.-M., GARCIA T., DOUVILLE E., FRANK N., MONNIER J.-L., HALLÉGOUËT B., LAFORGE M., HUET B., AUGUSTE P., LIOUVILLE M., SERRE F., GAGNEPAIN J. (2012) - ESR and ESR/U-series dating study
  • ., GIBBARD P.L., MacPHAIL R.I., OWEN F.J., PARFITT S.A., PREECE R.C., ROBERTS M.B., ROBINSON J.E., WHITTAKER J.E., WILKINSON K.N. (2000) - Late Middle Pleistocene deposits at Norton Farm on the West Sussex coastal plain, southern England. Journal of Quaternary Science, 15 (1), 61-89
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
  • with an updating of its data which can help to the understanding of the Barnenez group. Key words: Megalith, North-west France, long tumulus, landscape (1) Université de Rennes 1 .UMR 6566-Creaah. florian.cousseau@gmail.com ARPI. Arqueología y Prehistoria del Interior peninsular 03– 2015
RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
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)
RAP03316.pdf (PLOUHINEC (29). Ménez-Dregan 1 : des Prénéandertaliens aux Néandertaliens à l'extrême ouest de l'Europe. Rapport de FP)
RAP02901.pdf (LARMOR-BADEN (56). Gavrinis : à la recherche des représentations d'une tombe à couloir du IVe millénaire. rapport de fp 2013)
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
RAP02794.pdf (LARMOR-BADEN (56). Gavrinis : à la recherche des représentations d'une tombe à couloir du IVe millénaire. rapport d'opération)
  • technologie numérique (http://www.scottishten.org/) appartenant à Historic Scotland, au Glasgow School of Art,et à la société CyArk, décide de numériser le « cœur du Neolithic Orkney ». Une sélection de sites réputés (UNESCO World Heritage Sites), conservés dans ces îles du nordest de
  • /chamber-of-secrets-historic-scotland-launchesvirtual-tour-of-maeshowe.htm Enfin, Pixogram, une société établie à Edinburgh, spécialisée en projets sur le patrimoine architectural (reconstruction et visualisation), propose dans son portfolio un cercle de pierres dressées enregistré par
RAP00311.pdf (BAIN-SUR-OUST (35). Binon. rapport de sauvetage urgent.)
  • . An introduction to the study of terra sigillata. LONDRES 1920. PL. LVI n° 14) datée de 170-180 ap.J.C. - BB52I rebord de forme Walters 79/80, fréquent également à PUDDING PAN ROCK, de même datation. - BB5235 fragment de col de forme Drag 43, courant également à la fin du II0 siècle ( 175-200
  • -West ainsi formée, mesure 4m. X 5m. A l'est, M6 détermine un espace moins vaste, axé N-S, large de Im,50, interrompu au sud par D5(a). L'éventuel prolongementdneM^ pourra être confirmé que par des fouilles. Dans l'axe du seuil découvert en exc.Có, une pièce s'allonge, orientée Est
  • -West. Dans la stratigraphie sud de exc. C6, le mur D6 est postérieur à la construction du sol, tandis que l'alignement qui lui est parallèle et, distant de Om,60, en est contemporain. Ainsi, cette pièce plus vaste vers le sud, aurait été divisée ultérieurement. La fonction de
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)