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RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • ) 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
  • 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
RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • , 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
RAP03331.pdf (PLOUEZOC'H (29). Sondage au sein de la chambre H du tumulus sud de Barnenez. Rapport de sondage)
  • France. Bibliographie Ard, V. Mens, E. Poncet, D. Cousseau, F., Defaix, J. Mathe, V. Pillot, L. à paraître ‒ Life and death of Angoumois dolmens in west-central France: architecture and evidence of the reuse of megalithic orthostats Bueno Ramírez, P. Balbín Behrmann, R. de, Laporte
  • -Behrmann.R. Barroso-Bermejo, R. Darriba, X. Paz, A. 2016 - Stones before stones. Reused stelae and menhirs in Galician megaliths. In Proceedings of the XVII UISPP World Congress (Burgos 2014), Oxford, Archaeopress Archaeology, p.1-16 Cousseau, F. 2016 – Archéologie du bâti mégalithique
  • international de Saint-Pons-de-Thomières, Sept. 2012; DRAC Languedoc-Roussillon, Saint-Pons-de-Thomières, p.175-191. Laporte, L. Joussaume, R. Scarre, C. 2002 – Megalithic monuments of west-central France in their relationship to the landscape. in Scarre, C. ed. – Monumentality and Landscape
RAP00748.pdf (SAINT-BRANDAN (22). le Rillan. rapport de fouille préventive)
  • afin de se faire une idée générale du site. Ainsi d'Est en West ont été ouverts les sondages (Figuro i ) t m NM12 - N15 - S35 Z
  • compter des fragments de céramique commune. ci Dans la partie Nord du sondage une conduite d ' a c t i o n d'eau a sectionné d'est en West, l e sol et les structures de pierre. Pour se faire une idée des différentes strates sous-jacentes au niveau du sol, une section a été effectuée
  • , la moitié Sud ayant été détruite par la tranchée J d'aduction (la même que celle du sondage K.N.12) Dans un premier cesps un sondage pilote fut ouvert dans l'angle Nord-West. Ge sondage, ( voyez la coupe) (les n° donnés entre parenthèses correspondent au djessin), a livré sous la
  • terre végétale ( l ) et pie couche (2) de remblais un alignement de pierres (p) (M. du plan) Est-West qui correspond à celui observé en M.N.12. Son aspect est identique. I l repose dans une fondation remblayée par le remblai (2) qui a livré dans cet endroit quelques tessons
  • (76091l). De part et d'autre apparait le sol horizontal constitué par de l'arène granitique ( s i ) Dans l'angle Nord-West quelques traces de foyer étaient visibleS. Ge sol recouvrait une couche d'argile grise contenant des charbons de bois, quelques tessons de Serra Rubra, de
  • paroi West une déclivité faisant penser à un drain ou un carniveau (7) On remarqua également unedépot ferrugineux naturel(o). Nous retrouvons donc dans cette stratigraphie, les 2 niveaux d'occupation déjà notés dans M.N.12 5 * U îï.15 6 !
  • correspond à la structure " C ost- raetérlsée par une fondation de mur Est-West avec retour vers le Sud, à l ' i n t é rieur duquel ont été trouvés plusiettrs tessons du 1° siècle (Terra Nigra, cruche à pâte blanche) 5(760925). La construction de cet édifice s'est effectué dans la
  • -West. A ce mur se rattache, au Sut, an sol en terre battue et une fosse dépotoir qui ont livré un important mobilier dont 2 fragments de Drag 27, des fragments de vase ballustre, d'amphore à pâte blanche et orangée, (760922), et deux vases aétallescents à décors de barbotine (760923
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP00724.pdf (SANTEC (29). roc'h croum. rapport de sauvetage programmé)
  • D'ÉTAT - ANTIQUITÉS AFFAIRES CULTURELLES PRÉHISTORIQUES Zone West Circonscription de Bretagne i V l a n Dept. : 2 9 Commune : 5 / 7 A / T E C L i e u - d i t : Tvoc h Crourn N° : Ño ut Date: Relevé : t l e c c r f 1976 Mise au nef : VZ Tomb Tombe Tomh* n- n° Z
  • Tomb Tombe rj°Z Tombe n°11 cl ensemble MINISTÈRE D'ETAT - ANTIQUITÉS AFFAIRES CULTURELLES PRÉHISTORIQUES Zone tombe Circonscription de" Bretagne Dept. : 2 9 West n° 1 Commune : S FIN TEC Lieu-dit : P o e h N° : Croum Date: Relevé : YlecerÇ Septembre 79 Mise
  • au net : Y j L limite 7>/an couvert I de /a ure. 0 Tom Le d. I i1 m Tombe- de foui Ht , MINISTÈRE D'ÉTAT - AFFAIRES CULTURELLES ANTIQUITÉS PRÉHISTORIQUES Circonscription de Bretagne Dept. : ¿ ^ C o m m u n e : Lieu-dit : T?oc'h N° : Relevé West tombe 2. S
  • N° : h Date: Tombe West n° 4- TEC croum Septembre 'P/an 73 Relevé : Y ¿ e c e r f Mise au net : / . / . . I : . >': tsmbe P/
  • . ^ 1 MnM, ' ' m M m P ^ P / a n de I 0 I I1 m /a couverture MINISTÈRE D'ÉTAT - ANTIQUITÉS AFFAIRÉS CULTURELLES PRÉHISTORIQUES Lieu-dit : " R o c ' b N° : Relevé : tlecerf SAN TEC J^lan croum Date : West Tombe n° 7 Circonscription de Bretagne Dept. : 2 9
  • Commune : Zone Septembre 73 Mise au net : X L . de /a tombe 1 ANTIQUITÉS PRÉHISTORIQUES Circonscription de Bretagne Zone Tombe West n° 8 Dept. : 2 9 Commune : à f i N T E C Lieu-dit: ~Roc~ h Ctroum N° : Date: Septembre 73 Relevé -.iLecerf Mise au net : YL 1 T^/sins de
  • /s couverture Plà n n m T^lan d
  • ¿One I3Y3 Mise au net Tombe n? 9 0 joaroi Nord 1 m 5 9 , MINISTÈRE D'ÉTAT - AFFAIRES CULTURELLES ANTIQUITÉS PRÉHISTORIQUES, Circonscription de Bretagne Zone West Tombe Dept. : 2 9 Commune : Lieu-dit : TPoc'h N° : 10 Croum D a t e : Rout Relevé : ÎLecerf
  • : //ecerf Mise au net : V l ciu n° / / TEC Tfoc'h croum To^'il-'ton West sjueUtte P/a ns T/an de n°i /a couverture . de la tombe B íi B iHlíliTiTliti,'1'íli'ii'ifrf'rf o Zone mjrran jrg,/ ÍUS( B l> B Xr>3|iS\e aunpí Z ~P!an de la. o n e Est tombe n
RAP01961.pdf (bassin occidental de la Vilaine et centre Bretagne. rapport de prospection inventaire)
  • -West Germany Aerial photographies from the First World War: a contribution to the World War-archaeology in Belgium M. Willbertz Was ist eine Fundstelle? Qu'est-ce qu'un site? What is a site? H. von der Osten-Woldenburg Différent numerical and visual concepts for combining aerial
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
  • 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
  • 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
RAP00316.pdf (BRUZ (35). Fenicat. rapport de fouille de sauvetage urgent.)
  • a u ) au NORD-WEST de l a p a r c e l l e de f a ç o n s i n e t t e q u ' u n r e l e v é p r o v i s o i r e de l a t r a c e a pu ê t r e d r e s s é ( v o i r p l a n c h e N° 3 ) • I l s ' a g i t d ' u n e p e t i t e c o n s t r u c t i o n d ' e n v i r o n 65 m 1 au Sud de
  • é o p h y s i q u e de 1958» première La l i m i t e West de c e b a s s i n , t o u t au moins d a n s s a Sud e s t c o n s t i t u é e par l a f a i l l e de P o n t - P é a n . moitié A l ' E s t du b a s s i n p r i n c i p a l , on p e u t m e t t r e en é v i d e n c e
  • o r i e n t é e s ' s u i v a n t un a x e • p r i n c i p a l Nord-Nord-Est permettant l ' u t i l i s a t i o n des v e n t s dominants sur c e t t e zone ( West- Suê-West ) I l s ' a g i t d ' u n f o u r de p o t i e r q u i a p p a r t i e n t à l a c a t é g o r i e d e s
  • e s s a n t au Nord-West en t ê t e du l a b o r a t o i r e . - Un d r a i n a g e i n f é r i e u r A' o r i e n t é au S u d - Sud West ( v o i r p l a n c h e N° 9 ) , de l o n g u e u r a s s e z i m p o r t a n t e ( 7 , 1 7 m ) t a i l l é dans l ' a r g i l e e t d o n t
  • o r d - N o r d - E s t ( f o n d du l a b o r a t o i r e ) g r è s i m p o r t a n t s de 2 0 x 1 0 cm en moyenne, a y a n t s u b i une forte calcination. Zone E s t e t 'West, g r è s de 10x4 cm en moyenne s a n s t r a c e de c a l c i n a t i o n . Cet ensemble e s t
  • l'aboutissement de c e p r i n c i p e d ' e x p l o i t a t i o n . D e s d e s t r u c t i o n s ( e n t r e a u t r e remembrement ) é t a n t i n t e r v e n u e s s u r l a z o n e West du f o u r , aucune t r a c e ne s u b s i s t e du c o n d u i t de c h a u f f e . La s t r a t i g r
  • WEST stratigraphie VUE B2 WEST détail stratigraphie B 2 7 VUE WEST d é t a i l stratigraphie B2 8 VUE partie NORD du four après décapage - fond du laboratoi re VUE .. »« : ' EST stratigraphie A2
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
RAP02794.pdf (LARMOR-BADEN (56). Gavrinis : à la recherche des représentations d'une tombe à couloir du IVe millénaire. rapport d'opération)
  • technologie numérique ( 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
  • l’Ecosse, a ainsi bénéficié de levés au scanner 3D à l’image de la fameuse tombe mégalithique de Maeshowe, et des cercles de pierres dressées de Stenness et Ring of Brodgar, tous considérés comme appartenant au patrimoine mondial (World Heritage Site). Un programme est prévu se dérouler
  • méthode laserométrique 3D et la technologie d’imagerie numérique, afin de produire un modèle visuel et métrique le plus précis possible sur ce site préhistorique mondialement réputé (« the world famous prehistoric monument »).
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
RAP02448.pdf (SAINT-VOUGAY (29). l'esplanade nord du château de Kerjean. archéologie des jardins. rapport final de synthèse de fp2 1998-1999.)