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RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
  • . 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
  • material and not pink. Pink schi stes are found, however, in some discrète areas: close to south-eastern Carentoir, in western parts of the Bruc 'blank', in odd fields near Pipriac, around Patis de la Porte, Château La Frèche, La Glonnais, Malon and in small quantities around Les
  • 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
  • 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
  • was found near Le Boschet, Château de la Boulaye, 'Château Gaillard' (ail in M) and near le Mur (R) . There are, however, two cases of such material being found near (apparently) non-seigneurial settlements 300m from Comblessac in R and 100m from La Rigaudiere, 1km south of Pipriac, in M
  • 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
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • pottery (maximum 5 sherds per square) was more evenly spread. Smal 1 quanti ti es of brick and tile (maximum 0 .5kg per square) were uhevenl y distributed, but tended to concentrate in the south of the field, away from the cl Lister i ng of pre—médiéval and médiéval pottery
  • ) 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
  • 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
  • to that of 10. The finds, though more plentiful, were similar in range: 14 sherds of grey coarse ware jars, 4 sherds of ter ra-ni qra -type pottery, 6 sherds of Iron-Age fabric and two pièces of ceramic tile were found. There was another ditch (11) in the south of the trench, eut
  • ) . 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
  • ) by machine in order to understand a feature. The archaeological préservation was of varying quality; features were only located if they penetrated the natural subsoil. On the ridge and top of the slope the features had clearly been truncated by ploughing so that few were deeper than 0.1
  • 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
  • at the bottom of the valley slope. The part of T39 which was on the ridge produced one shallow feature only, perhaps the base of a pit (65: 0.6m wide, 0.1m deep), whose fill (9) produced no finds. Between the brow of the ridge and upper part of the slope (between 30 and 60m from the south
  • 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
  • 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
  • with the wall. Perhaps, but not certainly, after the wall had gone out of use and maybe had been parti ail y démoli shed, foundation trenches (64 and 40) were dug into the buried soil (20 and 29) for two wall s to the south of 9/17. The trenches were of unequal depths but were clearly
  • , 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
  • south of wall 7/51 had far 1 ess material: 28 médiéval sherds, of which 27 were of Fabric 1, from context 5; 63 médiéval sherds, ail Fabric 1, from context 11; 9 sherds, ail Fabric 1, from context 25. The pottery was in a very good condition, surviving in large, unabraded sherds
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
  • 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
  • .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
  • , 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
  • 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
  • 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
  • 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
  • working days were spent on site and the average size of the team was six. Trench 25 This was the most westerly trench and was 39m long. The depth of plough soil varied from 36cm at the south, uphill, end to 1.10m lower down the valley side. The plough soil (1, 36) overlay the natural
  • clay subsoil (37), into which features had been eut. A small pit (35) was excavated in the south end of the trench, and a séries of uneven holes, interpreted as root holes (40) , were also found. The remaining features consisted of two irregular spreads of charcoal (39, 43), which
  • 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
  • completely the dépression of the holloway. 6 médiéval sherds came from this layer. A macadamised surface of quartz and bitumen was then laid over the filling of the holloway, and for a considérable distance to the south so that the road was virtually doubled in width (18, 21, 55
  • ). The surface had been fragmented through plough destruction. Five mètres south of the holloway a ditch 1.5m wide and 45cm deep was excavated (.1.0); its filling contained one médiéval sherd of pottery (7, 8, 9). It was apparently on the same alignment as the holloway and had silted up
  • 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
  • of which contained Iron Age pottery. Trench 16 4.5m south of the ? eaves trench in T15 a collection of at least 4 intercutting pits was excavated,, Thèse may have been dug to extract clay. Ail the pits seem to have been filled at the same time. 4 separate layers were identified; thèse
  • was then allowed to silt up , a layer of clay with some charcoal accumulated (60), followed by perhaps a more deliberate backfilling with more clay (58) and a mass of burnt stone which had been thrown in from the south (59). Thèse were nearly ail hard blocks of conglomerate (387.), quartzite
  • (277.), greywacke (147.) and quartz (107.). The stone may have been used when the pit was used for firing, piled on to the south si de, and then pushed back. No finds were recovered from this feature. Half a mètre to the north a pit containing burnt clay fragments was excavated (18
  • to the south. The stone seems to have been piled into a large irregular pit which had been cut into the natural subsoil (48). It muet represent. collapse from some structure in the vicinity, but the cadastral map shows no trace of any structure or track in the area in the early nineteenth
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
  • . 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
  • , 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
  • /grey and red/yellow) and three sizes (1.5cm) in an attempt to find criteria for distinguishing between local and imported material. A107 lies just below a flat, exposed hilltop on a south-facing slope 75-80m high. The area was arable when the cadastral survey
  • 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
  • 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
  • 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
  • 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
  • , 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
RAP00129.pdf (PLOULEC'H (22). le Yaudet. rapport de sondage et de prospection-inventaire.)
  • épées de l'Age du Bronze (Briard, 1971, fig. 1, 1-3) et deux crânes, probablement anciens. - le site de l'Age du Fer: la situation du Yaudet, à l'embouchure d'une rivière importante, donne à penser que nous n'avons pas là un promontoire barré ordinaire, lieu de refuge temporaire pour
  • l'Age du Bronze, Annales de Bretagne, L X X V I I I , 1971, p. - D'ARGENTRE, Histoire de Bretagne, 1681. - DE L A BORDERIE, A. 1853, Notes sur les origines du diocèse de Tréguier l'importance ancienne du Coz-Yaudet (Lannion). et - DE L A BORDERIE, A . , 1882, Le Yaudet en 1778
  • Galliou Institute of Archaeology., University of Oxford and Centre de Recherche Breton et Celtique, University of Brest The e x c a v a t i o n o f 1991 The s i t e o f Le Yaudet i n t h e Commune o f P l o u l e c ' h (C d'A) occupies a promontory j u t t i n g o u t i n t o t
  • south-west, east. outcrop, Les Rochers de t o t h e c l i f f edge a t the n o r t h ­ The e n t r a n c e p r o b a b l y passed around t h e n o r t h - e a s t end o f t h e rampart, a p o s i t i o n taken now by t h e modern road. The headland i s occupied by t h e core o
  • the archaeological i n v e s t i g a t i o n s and casual d i s c o v e r i e s and from t h e h i s t o r i c a l r e c o r d (De La B o r d e r i e 1853, 1896; Fleuriot considerable h i s t o r i c a l 1954b) t h a t Le Yaudet i s a site of potential: the promontory has produced
  • be determined? W i t h these o b j e c t i v e s i n mind a j o i n t F r a n c o - B r i t i s h e x c a v a t i o n was mounted o r g a n i z e d by Le Centre de Recherche Bretonne e t C e l t i q u e , U n i v e r s i t y o f B r e s t and t h e I n s t i t u t e o f Archaeology, U n
  • . e . w i t h o u t bonding o f or clay. Nothing i s y e t known o f t h e i n s i d e o f t h e s t r u c t u r e , t o t h e south o f t h e w a l l , n o r are o t h e r w a l l s o f t h e structure yet defined. To t h e n o r t h a few l a r g e stones were l a i
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
RAP03364.pdf (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport de FP 2014-2016)
  • rock shelter discovered by M. Le Goffic at the Rocher de l’Impératrice at Plougastel-Daoulas, aims to progressively fill in this gap. The first results of this archaeological operation actually suggest this shelter dominating the Elorn estuary and the Brest roadstead to have been
  • 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
RAP02029.pdf (l'âge du bronze en centre Bretagne. rapport de prospection thématique)
RAP02179.pdf (FOUESNANT (29). l'île aux Moutons. rapport de fp intermédiaire 2005 de fp 3 2005-2008)
RAP03654 (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport intermédiaire 2018 de FP 2017-2019)
RAP03187.pdf (QUIBERON (56). Beg er Vil : un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP 2015)
RAP02603.pdf (PCR Brécilien. étude interdisciplinaire d'une forêt mythique. bilan d'activités 2010. projet collectif de recherches)
  • 1971). La température moyenne annuelle avoisine les 11°C (Figure 6), avec des hivers cléments (45 °C en moyenne) et des valeurs estivales d'environ 17 °C. Sur les lignes de crête, des variations locales peuvent être observées. Elles présentent une baisse des moyennes annuelles de
  • l'ordre de 1 °C (Corillion 1971). Figure 5 : carte des précipitations annuelles en Bretagne : moyenne sur la période 1997 - 2006 (d'après les données Météo France) Figure 6 : carte des températures annuelles en Bretagne : moyenne sur la période 1971 - 2000 (d'après les données Météo
RAP02568.pdf (Corephae thématique : ouvrages de terre médiévaux. rapport d'étude)
  • A L'INVENTAIRE SUPPLEMENTAIRE IDENTIFICATION DEPARTEMENT COTES D'ARMOR COMMUNE CARNOËT LIEU-DIT Rospellem - Pont Troël NOM DU SITE DENOMINATION Motte et basse-cour CADASTRE 1971 -ZB (3) COORDONNEES LAMBERT 160,55 X 93,98 CARTE I.G.N. 717 ouest PROPRIETE Carnoët, Rospellem
  • vocation non seulement militaire (fortes défenses) mais aussi économique (contrôle d'un lieu de passage). Une protection au titre des M.H. est recommandée. DOCUMENTATION SOURCES FIGUREES Extrait du cadastre de 1810 Extrait du cadastre de 1971 Extrait de la carte I.G.N. au 1/25 000e
  • , feuille 717 ouest Carnoët, Rospellem - Extrait du cadastre 1971, section ZB A Carnoët, Rospellem - Extrait du cadastre 1971, section ZB A KoHc 3 : S^ii *■ ~Qï^
  • kilomètres e^st of Arzano on the road to Plou/sy is a magnificent example of a médiéval motte and bailey standing on the south side of the road. On each side, except the east, there is an almost sheer drop of several 100 feet. The motte stands on the east of the promentary v.here
  • . The motte itself was 30 feet a^cross the top and on a level with the middle of the "bailey. the south side PHnniHg. There is a stream down on In the middle of the bailey there stands a deserted 18th century chapel. ï FICHE DESCRIPTIVE DE SITE ARCHEOLOGIQUE EN VUE D'UNE INSCRIPTION
RAP02142.pdf (LE CONQUET (29). "île de Béniguet". fouille de l'amas coquillier. rapport de sondage)