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RAP00380.pdf (SAINT-DIDIER (35). les Suriaux. rapport de sauvetage urgent.)
  • jaune + schiste «• E - une couche de tuiles avec quelques briques éparses » f - la terre végétale. Ce carré S.20 a montré (ligure n° 6 ea A) la présence dans l'an le Sud-Est d'une structure grossière, sans mortier, postérieure à la couche - E -, mais il a été impossible d'en
  • ,%,17 Hr^> H.21 l*es résultats sent négatifs» ,9,rfffflft.c,»!7 Dana la zone C.1'7 (cf ligure 6 ai l) après passage des engins de terrassement* il est apparu une couche d'occupation asoes ancienne autant qu'on puisse en juger par l'état des lieux contenant d'infimes fragments de
  • .. •.... Figure . .. f, n° 5. ligure n° 5 (2° feuille) Fi g u r e n*6 + + + + + + O + + + + 4- + + + + -f + 4- m -h:; 1 o -4- o CM + O + €0 4- Cx + F i g u r e n° 8 Figure n°9 5 cm D.19 E. 4 D .20 B.1 F i g u r e n°1 0 E.20 E. 1 Figure n
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
  • ; 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
  • , then, di stincti vely 'blank' zones within the four communes and by contrast zones that tend to produce greater or smaller surface scatters. Either natural schiste or conglomerate are usually présent on the surface of fields in ail three transects, as also is imported 'roofing' si ate
  • 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
  • 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
  • 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
  • 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
  • and early twentieth centuries. Given that vacated buildings are often left to di sintegrate , collapsed buildings are likely to leave a surface scatter of schi ste; where this is distinguishable from natural, the distinction ought I \ to be noted since the material may be just
  • as significant as surface brick and tile. We have made some progress in characterising the local schi stes - which are of very mixed character and considérable local variation - by identifying small quarries within the study area and comparing samples with material from buildings and from
  • . The présence of this material on the fields therefore indicates imports into the study area for building purposes. It is so common on the surface of présent arable that it is reasonable to explain most of it as the product of manuring activities; it only does not occur notably on recently
  • them within the study area, it is probably impractical to attempt to instruct a teamamateurs to do so. However, it would be possible, in some areas, to be précise about the source of local building material and deduce patterns of its movement within the study area over time. More
  • intermittently by Wendy Davies. In the Easter season transects with uneven coverage will be rewalked, especially the northern part of E and parts of A and B, to achieve a relatively even survey of ail parts of the study area. The process of sampling the surrounding communes will be begun
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
  • 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
  • for di sti ngui shi ng between greater and lesser concentrations and for providing a means of référence to them; they do not necessarily dénote the location of former settl ements. ) In accordance with the conventions, the concentrations of surface material (total 219) may
  • of surface scatters Di scussi on Clearly the character of the surface material differs from transect to transect. Transects P and M had areas which produced a little pre-Roman pottery - as had Transect N - a phenomenon that is extremely rare in the core communes (Asti 11 and Davies 1986
  • used locally for building, especially roofing, materials was also recorded for each field (though not collected). Thèse materials were not carried for long distances (10—20km maximum) but can usually be clearly di st i ngui shed from local natural , and o-f ten have nail holes
  • 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
RAP02397.pdf (PLOUHINEC (29). Menez-Dregan I. rapport final de fp 2006-2008)
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
  • exploité cette partie qui présente d’après les photos des blocs d’assez grandes di- P.-R. Giot a aussi photographié la zone mensions. La découverte de la table ou d’autres autour de la table de couverture dans son état éléments mégalithiques présents dans la butte les après l’arrêt
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • Chapelle Gaceline, Caro, Reminiac, Augan and Campélieac in the Morbihan in eastern E
  • 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
  • in order to secure a wide range of possi b i 1 i t i es for testing; in fact, in many cases numbers were far higher than the necessary minimum. It should be stressed , yet again, that the ternis are conventions for di st i ngui shi ng between greater and lesser concentrations
  • of mixed 1 and— use. 1 an des (like B2S and D52) and meadow early ni net eenth-century (ilke BS7 and B90) demand some further investigation, since they previous to the nineteenth imply either arable use or settlement century; sites 1 i ke G21S, 220 and 221, lying in the di sti net i vel
  • 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
  • of local naturals and there are consequently far more fields with a mixture of black and pink/purple roofing schi stes , often with a prédominance of the pink. However, there were still zones that could be di st i ngui shed s black roofing schi stes overwhel mi ngl y predomi nated
  • , 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
RAP03498 (Les zones côtières et les évènements climatiques. Rapport de PI 2017)
  • Commune principale Lieu-dit du cadastre Année Section(s) . Parcelle (s) Perros Guirec Ploumanac’h 2014 AB . 42 . Commune secondaire(s) (s) Lieu-dit du cadastre Année Section (s) Parcelle (s) IDENTIFICATION DESCRIPTION OHV DI¿[HV HW VRQW j FKRLVLU GDQV OD OLVWH GHV DI
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  • charbon. Lors de la visite de terrain, aucune stratigraphie claire n’a pu être établie, cependant, cette couche se trouve entre l’humus dans le niveau supérieur et un limon dans le niveau inférieur. INTERPRÉTATION OHV DI¿[HV HW VRQW j FKRLVLU GDQV OD OLVWH GHV DI¿[HV PDWLqUH
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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
  • 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
  • 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
  • %). Some of the Brioverian shale was tooled; and the quartzite was di st i net i vel y like that recovered in 1986 from excavations on H80 1km away (Astill and Davies 1987, 116). In maki ng the extension a gap of about lm was left between the corner and the new wall to make a doorway
  • ; most of it. had clearly been protected from plough damage, despite its présence? in the plough soil. The pottery from the other contexts was not di f f erenti ated by layer or feature; hence, the pottery in buried soil 20/29 and in the features eut into the subsoil was still predomi
  • 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
RAP01573.pdf (ARRADON, PLOEREN (56). rapport de prospection inventaire)
  • Nom du sie: Lieu oft: Gallo romain / Centre X: Centre Y: AT Sie: 209,275 2 304,075 56-003 Nom du sie: 9 N'Site: AH Lieu d»: 209,800 2 305,350 56-003 Centre X : Centre Y: 10 AH Lieu di: 213,575 2 306,825 56-003 Centre X: Centre Y: 11 Année du cadastre: 1983
  • parcelles: ZB.191. ZB.192. ZB.193. ZB.251. AH Lieu di: Gallo romain / Mur Gallo romain / Gisement de surface 56-003 Nom du sie: 12 AH - Lieu dt: 213,775 2 306,700 56-003 Nom du site: Centre X: Centre Y: N'Sie: Gisement de surface Année du cadastre: 1983 parceBes: ZC.129. ZC
  • .130. ZC.187. ZC.188. ZC.322. ZC.323. ZC.81a. ZC.81b. ZC.82. - Lieu di: Gallo romain / Gisement de surface Gallo romain / Mur 214,925 2 303,850 ROGUEDAS Année du cadastre: 1983 parcelles: ZD.169. ZD.86. ZD.90. ZD.91. 14 AH - Lieu di: Gallo romain / Centre X : Centre Y
  • : 214,500 2 305,100 56-003 Année du cadastre: parcelles: 777 1983 18 . Lieu dt: Néolithique / Centre X : Centre Y : 1983 19 . Nom du sie: Centre X : Centre Y : N'Sie: Ueu di: Néolithique / Dolmen Néolithique / Menhir 214,500 2 305,950 56-003 Année du cadastre: parcelles
  • : 777 20 . Lieu di: Néolithique / N° Sie: 214,000 2 303,800 56-003 Nom du sie: Centre X: Centre Y: LA CHENAIE 1983 Nom du sie: Centre X: Centre Y: LE TREH Dolmen Année du cadastre parcelles: 777 56-003 KERAVELLO Dolmen Nom du sie: N'Sie: PETIT LOGODEN Four de
RAP03383.pdf (RENNES. Église Toussaints : la sépulture de Louis du Plessis (†1661). Rapport de sondage)
RAP02726.pdf (PAULE (22). l'habitat aristocratique de Bressilien à Paule)
  • , Northamptonshire Oxfordshire), Oxford University Department for External Studies, Oxford, 1982, 202 p. MENEZ, Y., BATT, M., BARDEL, J.-P., LE BIHAN, J.-P., 1988 - L’habitat du Haut Moyen-Age de Creac’h Gwen à Quimper (Finistère), in : Revue archéologique de l’Ouest (RAO), n°5, Rennes, 1988, p
RAP00564.pdf ((56). l'arrondissement de Vannes. rapport de prospection inventaire)
  • * / | A o 0 Q pottibl* sitvs * Roman ittt* • m«di«val sittt ■ po*t mcditval litis Figure 1 253 - on ajoutera enfin que.de nombreuses enquêtes similaires ayant été entamées dans d'autres parties de la Bretagne au cours des dernières années, le matériel de comparaison est abondant, et
  • millénaires. (Traduction : Patrick GALLIOU, Université de Bretagne Occidentale, Brest) Notes. Cl) On consultera également : G.G. ASTILL,W.DAVlES,"Fieldwalking in East Brittany, 1982", Cambridge Médiéval Celtic Studies, IV , 1982, 19-31 ;id. , "Un nouveau programme de recherche sur le
RAP01079.pdf (LA MARTYRE (29). le Bois Noir. rapport de fouille préventive)
  • di 100 à 300 ap. J . G.). la cite des 5 Vi s I, à 37 de la d*c 7225 -
RAP00025.pdf (PLOUBAZLANEC (22). karreg ar yellan.. rapport de sauvetage programmé)
  • ) est d'épaisseur assez régulière. L'industrie moustérienne apparaît surtout dans la partie supérieure de la couche 7. Un éclat situé dans la couche 6 peut appartenir à la série Paléolithique II/.2.4. Coupe nord-est Déjà (A-B) ligure supérieur. 7. décrite en 1982, cette coupe
RAP01782.pdf (LA ROCHE-MAURICE (29). château de roc'h morvan. rapport de fouille programmée annuelle.)