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RAP01858.pdf (les sites mésolithiques en Bretagne. rapport de 1re année de projet collectif de recherche)
  • péninsule, adaptations au milieu), - territoires et identités (intégration / réaction face aux flux culturels européens, transformations des territoires d'acquisition au cours du temps, matérialisation des espaces culturels). En 2001, l'accent a été mis sur les analyses des vestiges
  • transformation des peaux en cuir. Les haltes de chasse sont complémentaires de sites spécialisés dans d'autres domaines techniques. La notion de camp de base reste encore à définir, tout au moins dans le monde méditerranéen. Dans la région atlantique, il semble au contraire que les chasseurs
  • techniques de communautés nomades sur diverses aires géographiques. 2. ENTRE L'ECORCE ET L'ARBRE: REFLEXIONS SUR LES PRATIQUES DE L'ARCHEOLOGIE (PIERRE GOULETQUER) L'arbre, c'est la masse noueuse et compacte de l'archéologie de sauvetage, qui plonge ses racines dans le bouleversement du
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
  • , adaptations au milieu), territoires et identités (intégration / réaction face aux flux culturels européens, transformations des territoires d'acquisition au cours du temps, matérialisation des espaces culturels). En 2001, l'accent a été mis sur les analyses des vestiges animaux Beg
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • EAST BRITTANY SURVEY EAST BRITTANY SURVEY SEPTEMBER Introduction B409 (Carentoir ZA161) Fig. A92 1, 2 (Ruffiac ZK67) Fig. A3 1/79 3 (Ruffiac ZN119) Fig. 4 Fig. 5 H 132 (Ruffiac ZL40) Fig. 674 6 (Carentoir YB29) Fig. 7 L26 (Ruffiac YA224) Fi g . 8 D153
  • (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
  • ) 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
  • 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
  • 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
  • large Roman settlement which lies 100m to the south east (see fig. 2). In sura , then , this 6m square produced évidence of an early agricultural phase, followed by two phases of Iron-Age activity, and then a later - perhaps mue h later - agricultural phase. Although there is a large
  • 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
  • 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
  • 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
  • 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
  • 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
  • 0.3kg per square) of brick and tile. The field is lowlyinq and located 100m east of the Château de la Ruée, to the? east of Ruffiac (fi g. 6). The a n c ien çadas t. r e records this field as permanent meadow in the early nineteenth century but it also shows that it forméd part
  • 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
  • , 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
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • , Sussex Bell, M. 1983 'Valley sédiments as évidence of prehistoric land-use on the South Downs', Proceedings of the Prehistoric Society, xlix, 119-150. 1+ EAST BRITTANY SURVEY 1985 £J3 fields walked m 1965 ■— — commune boundaries A • ■ sites A c* U probable • médiéval si tes
  • 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
  • . The remaining concentrations (25.7%) had a prédominance of building material, at présent treated as undatable. 2 As usual , the topographical position of the sites was analysed. About a third of them (29.4%) were on flat 1 and while 17.1% were on south-facing and 16.6% on south-east-f
  • 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
  • . The results confirm the impression that this 1 and was not brought into cultivation until the twentieth century, and confirm the classification made on the basis of transect walking - the field real ly is 1 bl ank 1 . B347 lies on a slight east-facing slope at 35m, beside a stream, and its
  • ; without their help much of this year's season would have been impossible and we are therefore immensely grateful to them. Fieldwalking and excavation were financed by the British Academy, the Society of Antiquaries of London, the University of Reading, the University of London Central
  • Bretagne, ii, 27-34. Astill, G. and Davies, W. 1982a 'Un recherche sur le terrain dans l'Est de Bretagne, xxxv, 24-42. nouveau programme de la Bretagne', Arch. en Astill, G. and Davies, W. 1982b 'Fieldwalking in East Brittany, 1982', Cambridge Médiéval Celtic Studies, iv, 19-31
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • intervais, using collection units of 100m; field EAST BRITTANY SURVEY 1986 | TRANSECT J TRANSECT B "t— TRANSECT D TRANSECT A TRANSECT E -h— .y. : 75 m ■ ci3 " S Y •m .o-v. Tréal Lo 50ml—' O O .... □ ; C? (Rutfiac g SO TRANSECT G l'ï «2. cm. fl\ □ 1-5km apart
  • intensive covera\ge achieved by rewalking many of the transects did not affect distribution patterns already noted» By contrast , concentrations of surface material are ^frequently found in zones around Le Cleu, La Touche (east of Treal) and - especially - in the southern half
  • .Land whiie 14/. were on south-f aci ng and 19.37. on east-facing slopes. Upland concentrât i on s were not especially notable, with only a quarter lying between the 50m and 75m contours (28. IX) 5 almost a half 1 ay between 25m and 50m (49.17.). Somewhat less than a half
  • and their property less dispersed, with more cattle and altogether a more wealthy air; and, despite récent in the core. remembrement , fewer remembrement mounds than Transect M, running slightly south 01 east from the south~-e?ast corner of Carentoir, was bequn, but most of it remains 209 fields
  • 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
  • sel f . K446 (Ruffiac ZA106) Ruf f i ac K446 is si tuât ed on the eastern outskirts of Becul eu 1 n
  • (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
  • was a ragged v-shaped ditch, 1.3m wide and 40cm deep (46), which followed the slope down the valley side -for at 1 east 90m; subsidiary machine eut s (T26, T27) located the ditch on the saine alignment and f ai 1 ed to produce évidence of a tujrn. Both ditches contai ned small quanti ti es
  • schi ste. Dver the bottom had been laid a layer of compactée! schi ste in which there was at 1 east one rut. (64). On this surface accumulated a layer of silt (63), which was in turn covered by soil which had been tipped in from the south edge of the holloway (61, 62). A new surface
  • east of La Hattaie (fig. 4). The field is in a low-lying position and si opes very slightly down to the north. The ancien cadastre shows that H80 was an area of mixed land-use, parti y cultivated in strips but also with 1 an des (uncul ti vated ) and pasture, in small enclosures
  • 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
  • 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
RAP02603.pdf (PCR Brécilien. étude interdisciplinaire d'une forêt mythique. bilan d'activités 2010. projet collectif de recherches)
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
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
  • (from the area of La Sourigaie to La Houssaie), passing through the communes of Missiriac and Malestroit and the northern outskirts of the town of Malestroit; Transect R ran north east for 7.75km from Trelo to Le Mur at the north-east corner of Carentoir, passing through the communes
  • of Comblessac, Guer and Les Brûlais; Transect M ran due east to the River Vilaine for 21.5km front the area of Bat Colin and Le Boschet in south-east Carentoir, passing through the communes of La Chapelle 1 Baceline, Sixt, Bruc , Pipriac and Guipry, and just south of the bourg of Pipriac
  • the 'blanks' lay on the steep si opes around La Hennelaye and Le Haut Couëdic. In R the 'blanks' lay near the Carentoi r /Combl essac commune boundary and on the steep si opes to the north east of this area; also north of Comblessac bourg , in and around the Lande de Craon. There were also
  • 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
  • of Bruc — for a distance of some 2.5km; thèse 'blank' fields begin already in the eastern part of Sixt commune though do not reach as far as the présent boundary of Pipriac on the east. Everything, including the shape of the fields, suggests that this is an area of late exploitation
  • . 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
  • (23.8%) - north-east especially; in R on east-, north-eastor south-east-f aci ng slopes (37.77.) - east especially. In P 37% lay on -Fiat land, in M 19.47. and in R 22.6%. Ail this is unremarkable in the light of the prevailing local topography. Présence of the imported schi stes
  • on the north-east side of the high land near the Carentoi r /Combl essac boundary and none by the wood in the Lande de Craon, both areas lacking surface pottery too. There was little or no pink material on the western and south-western si des of this high land, and none from Couè'dillan
  • north east to Comblessac, as also north from Comblessac to the Lande de Craon. The pattern of occurrences of the schi stes in thèse transects suggests that the pink schi stes . i.e. material from the Guer quarries, may wel 1 have been the earliest to be used in the roofing industry
  • and the western section of M). Some of the Roman fabrics in eastern ti had not been noted before, and included a late Roman roi 1 er-st amped sherd of Argonne ware from M447, near 'Château Gaillard', 2.5km east of Pipriac bourg ■ This ware has an essentially coastal distribution, although
RAP02005.pdf ((29). le mésolithique en Bretagne. rapport de projet collectif de recherches)
  • aux flux culturels européens, transformations des territoires d'acquisition au cours du temps, matérialisation des espaces culturels). En 2001, l'accent a été mis sur les analyses des vestiges animaux et marins, avec des prélèvements à Beg-an-Dorchenn et à Hoëdic. Au cours de
  • simple transformation à l'état solide de la roche. Dans le premier cas, on devrait observer des proportions assez élevées de la phase amorphe au sein des échantillons . il est à noter que dans ce cas il s'agit des échantillons de roche qui pourraient être des « Pseudotachylites ». La
RAP02205.pdf (CARHAIX-PLOUGUER (29). un quartier de la ville antique de vorgium. les fouilles de la réserve archéologique. rapport de fp 1 2006)
  • géologique de certaines régions), -territoires et identités (intégration/réaction face aux flux culturels européens, transformations des territoires d'acquisition au cours du temps, matérialisation des espaces culturels). En 2001, l'accent a été mis sur les analyses des vestiges animaux
  • par simple transformation à l'état solide de la roche. Dans le premier cas, on devrait observer des proportions assez élevées de la phase amorphe au sein des échantillons . il est à noter que dans ce cas il s'agit des échantillons de roche qui pourraient être des « Pseudotachylites
RAP02333.pdf (LE QUIOU (22). la villa gallo-romaine de la gare. rapport intermédiaire 2007 de fp 3 (2006-2008))
  • utilisée sera la suivante : Un premier chiffre arabe pour la zone fouillée, une lettre pour caractériser la phase, un chiffre arabe pour l'état et enfin une lettre pour le sous-état, soit pour le premier état de la phase B de la zone 2 : 2B1. L'ordre de numérotation est croissant de
  • , transformations chimiques, animaux fouisseurs) et certainement des réaménagements anthropiques (travail de la terre...) que la fouille n ' a pu déceler. •tSea c î po o F ' m UH3^ ; .10^/ .oq'0',, liaofl? taa'q'S „ _ _ Î9£tp a Baignoire 141 | jWV Q Figure 13 : Plan des structures
RAP01944.pdf (ÎLE-MOLÈNE (29). inventaire du patrimoine archéologique du paléolithique au Moyen Âge. rapport de prospection thématique)
  • la recherche actuelle est d'essayer de comprendre ce processus de néolithisation, c'est-à-dire d'établir un lien entre le comportement des populations réputées nomades du Mésolithique final et celui des populations supposées sédentaires du Néolithique. Tenter d'appréhender les
RAP02901.pdf (LARMOR-BADEN (56). Gavrinis : à la recherche des représentations d'une tombe à couloir du IVe millénaire. rapport de fp 2013)
RAP00563.pdf ((56). l'arrondissement de Vannes. rapport de prospection inventaire)
  • direction et 33 EAST BRITTANY SURVEY 1982 i i / i \ Carte A : Localisation de la zone étudiée. ■—■ —- major geological boundories transect A transect B 5 km 34 le code des -unités de ramassage et le nom des prospecteurs. Ces fiches étaient remplies sur le terrain. Un examen
  • le cadastre du dixneuvième siècle indique un groupe de maisons inhabitées mais où l'on ne voit plus rien aujourd'hui, nous avons découvert une proportion de céramiques paraissant fort élevée si on la compare à celle des briques et des 36 EAST BRITTANY SURVEY 1982 tOOm «T
  • communes concernées ainsi que l'indulgence et l'intérêt dont ont fait preuve les agriculteurs. Les Universités de Reading et de York, VUniversity Collège (de l'Université de Londres, le Colt Fund de la Society for Médiéval Archaeology et un donateur anonyme, ayant versé une contribution
RAP03300.pdf (RANNEE (35). La Chaussée. Rapport de fouille)
  • a rural habitation dating between the second century BC and the first century AD. Excavations at La Chaussée provide data documenting the western edge of this site. The La Chaussée site is characterized by a series of parallel east-west ditches that cross the study area ; the two
  • layers as well as from the upper fillings of the ditches. In the southern part of the study area, and organized parallel to one of the ditches, a possible semi-circular building (apse) was identified. While the plan is incomplete, the structure is oriented on an east-west axis