Rechercher sur le site

  • Chercher les documents contenant un mot OU un autre : tapez simplement les mots à la suite => bracelet bronze
  • Chercher les documents contenant un mot ET un autre : utilisez le mot-clef AND => bracelet AND bronze
  • Chercher les documents contenant une expression exacte : taper l'expression entre guillemets => "bracelet en bronze"

Limiter votre recherche

Type d'opération
Date (Année)

758 résultats Exporter les résultats

Trier par Titre : ascendant / descendant
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • ; 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
  • collection; phosphate analysis and soil magnetic susceptibil ity survey of the four selected areas; and excavation of part of a bank and lynchet near a field from which 'total' collection had previously been made. Three days (21-23 March) were spent in préparation by three people
  • 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
  • samples for future phosphate analysis were taken from the topsoil in ail squares, at 5m intervais, and soil magnetic suscepti bi 1 i ty readings were also taken at 5m intervais, at the spot from which samples had been lifted. Fluxgate gradiometer readings were not taken since 1984
  • 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
  • of the last year pollen analysis has been carried out on samples taken during 1984, in particular from buried soils beneath banks in woods near Le Vivier (not far from the excavation site) and Le Rond Point (Carentoir), areas of extensive 1 ande in the early nineteenth century. Although
  • 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
  • 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
  • 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
  • . Meanwhile Pete Addison will complète the survey of standing buildings; a small team will dévote February, March and April to 'total' collection; analysis of pollens from the Mauffrais podsols and the River Aff \1 backswamps will continue; and work on the local schistes will be pursued
  • : transects will be taken radially from the area of intensive study, and fields within them walked at 50m intervais. Excavation of Allô will begin, in order to ascertain the relationship of this year's excavated features with the settlement and at the same time make some assessment
  • 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
  • , 1984b). The latter analysis has been completed and, as demonstrated below, is of particular significance for fieldwork. The 1985 season involved fieldwalking over large areas at wide intervais, as in 1982 - 84; fieldwalking four selected areas in 5m squares for 'total' surface
  • ; the main team (consisting largely of past and présent students from the Universities of London and Reading) numbered twenty-two, including the directors; it worked for twel ve days, from 24 March, and had one day off; nine people (including one director) remained for an additional week
  • , and one spent three days taking soil samples for analysis at the Institut National Agronomique Pari s-Grignon . The weather varied between bad and appalling for much of the three weeks, with plenty of rainfall , but the crop was not high and fields were often in idéal condition
  • covered, encompassing 772 hectares (4.01% of the surface area of the four communes). 30.99kg of pottery and 93.92kg of man-made building material were recovered from the transects; 45% of the pottery was médiéval, 53.6% post-medieval and 1.4% Roman. No pre-Roman pottery was found
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • ) 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
  • . 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
  • st i es of the former, was separated from the Ruf f i ac/Carentoir core by the great Bruc 'blank'. Work outside the main season. 19B6—B7 During the past year work has continuée) on other aspects of the project, both field and archivai. Mi cromorphol ogi cal analysis of soi 1
  • samples from the 198é> excavations has been undertaken by Anne Gebhardt, under the supervision of Marie-Agnès Courty. Analysis of pottery fabrics has continuée), the sorting and classification of fabrics from the three 19B6 seasons now being half completed. Further work on local
  • then - between October and January 19B7 - undertook the index ing and organisation of this material, together with basic analysis of démographie data she had previously collected. Ail data from the survey of standing buildings has been put on dise, ready for analysis in the coming year
  • 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
  • éléments) analysis of documents, including the very detailed cadastral maps and records of the early nineteenth century. This latter analysis has been completed and is of psrticular significance for fieldwork since it allows complète reconstruction of the early ni neteenth-century
  • landscape
  • , Reading, Cardiff and York) numbered twenty-two, ' including the directors, and worked for twel ve deiys, from 22 March, with one day off. Six people went in advance, and worked for one day beforehand. Overall, 330 mandays were spent on this year ' s season, including travelling time
  • (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 pottery, 161.72kg of man-made building material, 23 from thèse flints and 611.72g of haematite were recovered transects , together with two worked pièces of quartz (from M). This breaks down, by transect, as follows: Brick/tile kg 18. 49 P M 121 . 77 21 . 46 R Pre-Rom. Pottery 1 . 47
  • 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
  • for its very 1 ow proportions of médiéval pottery and very high of post-medi eval . Thèse results are striking by comparison with patterns of material recovered from the four core communes. Whereas the amounts of Roman material collected from the surface are mue h the same, the amounts
  • and proportions of médiéval material are 1 ower (especially in R) - as in N - while those of post-medi eval material are considerably higher, though not as high as in N; in the core 507. of pottery collected from the surface was médiéval and 46.77. post-medi eval . The proportion
  • 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
  • to existing settlements was much the same as found in the core communes, with slightly fewer concentrations at distances above 300m from modem dwellings. In ail cases material tends to occur within 50 and 300m of settlements - in P, for example, 33.37. of concentrations lie within 100
  • . 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
  • 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
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • , 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
  • 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
  • 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
  • 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
  • (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
  • the four communes named above, and sampling of fields in the surrounding communes, together with sélective geophysical and geochemical survey, and smal 1 excavations to test results; compl ementa.ry envi r onmental analysis is al so being undertaken . The fieldwalking programme
  • /79, H 132, 874, L26, D153) from which 'total' collection had previously been made (fig. 1). Of thèse, A92 had been started in 1986 and remained to finish. The ai rn of thèse smal 1 excavations was the investigation of surf ace/'sub-surf ace rel at i onshi ps; fields were selected
  • five-day planning trips by two in September 1987 and April 1988. The team, consisting of volunteers from a wide range of places, numbered twenty-six, including the directors, one finds assistant and three supervisors; it worked for f i ve weeks from 28 August, with four days off
  • 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
  • , and the majority (577.) of the post-medi eval wares was ni neteenth-century . Smal 1 quanti ti es of brick and tile were recovered but only from the first three spits (total 23 fragments, 0. 787kg) . Context 1, however, had in addition to local quartz and quartzite large quantities (120kg
  • o-f the trench because o-f lack of space for the spoil, so the trench was reduced in size to 6 X 3m. The pottery from this layer (2), like the stone fragments, provides a complète contrast with that of the plough soil. 61 sherds were found, ail of which were Irôn Age, the most
  • 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
  • . The range o-f pottery recovered -from the top two spits was very différent -from the lowest spit. In the first twenty centimètres 45 sherds were -found; médiéval pottery predominated (837.), -followed by post-medi eval (157.) and a single sherd o-f Roman pottery (27.) ; 52 -fragments o-f
  • -orange clay (24) from the surface of which came 20 sherds of Iron-Age pottery, the majority of which were of Fabrics 86 (607) and 89 (257). There was no sign of feat ures eut into this layer, which 1 ay directly on the degraded, manganèse— stai ned , quartzitic bedrock (05a) (33
  • ) . Comment The occurrence of médiéval and post-medi eval pottery in the plough soil, but not beneath , and the lack of conte;-; ts of thèse période would suggest that this matériel was not deriyed from SLib— surface features. Manuring might wel 1 account for the evenly distributed
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 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
  • . 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
  • 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 were 14cm and 20cm (contexte 4 and 5 respecti vel y ) deeps eamples for pollen and soil analysis were taken from context 5» No finds were recovered from the features, but four sherds of pottery came from the surface of the ditch fillings, whose ■fabrics were différent from those
  • represent the; original soil which formed the lynchet» A column of saimples was taken through the de;posits for soil analysis. Pottery from the colluvium was médiéval, similar to that recovered from the surface and from the other trenches; the majority were coarse wares (547. of fabric 1
  • (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 a métal led road, is particularly interesting. It demonstrates that the routes into Becul eu have changed. More importantly, the pottery from the holloway and associated ditch gives an indication that the earlier route was in use in the médiéval period» Thin section analysis of the si
  • 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
  • Chapelle Gaceline, Caro, Reminiac, Augan and Campélieac in the Morbihan in eastern E
  • nineteenth century» This latter analysis has been completed and is of parti cul. ar significance for fieldwork because it allows complète reconstruction of the early ni neteenth-century landscape (Astill and Davies 1982a, 1983, 1984, 1985). THE EASTER SEASON The 19S6 Easter season
  • involved fieldwalking over large areas at wide intervais, as in 1982 85, in the four core communes; sampling in the communes surrounding the core? and excavation of parts of a field from which 'total' collection had previously been made. Two days (21-22 March) were spent in préparation
  • for the main season by two people. The team (consisting largely of past and présent students from the Universities of London, Reading, Durham and Sheffield) numbered twenty, including the directors, and worked for twelve days, from 23 March, with one day off. A smal 1 team, of the directors
  • worked flints were also collected, three from transect E, three from B, two from B and one from D. One possible platform and thirty lynchets were noted, of which fifteen were in Transect D. As in previous years there were considérable variations in the concentration of recovered
  • and also zones that tend to produce more or less of a surface scatter» Surface material is usually markedly absent from areas near the commune boundaries and is also difficult to find in the fields to the north of Qui 1 vain and around Le? Bois Faux; si gni f i cant 1 y , the more
  • of Transect G, from Métairie au Joly to Le Nouai-)» The figures quoted above demonstrate the remarkably high proportion of fields in G with large concentrations of surface material. The présence of tile scatters, sometimes with smal 1 quanti ties of Roman material associated, were notable
RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
RAP00129.pdf (PLOULEC'H (22). le Yaudet. rapport de sondage et de prospection-inventaire.)
  • evidence b u t an e a r l y medieval date seems l i k e l y (Savidan 1935; Mazeres 1936). From 1952 u n t i l 1954 P r o f e s s o r F l e u r i o t examined t h e Roman w a l l a t t h e n o r t h - e a s t corner o f t h e s i t e b o t h west and s o u t h o f t h e Poste de Douane
  • 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
  • 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
  • h e Baie de l a V i e r g e , a wide e s t u a r y a t t h e mouth o f t h e r i v e r Leguer. The promontory, r o u g h l y r e c t a n g u l a r i n shape, i s separated from t h e mainland by a deep v a l l e y a l o n g which t h e minor road from Le Yaudet v i l l a g e t
  • h e headland from t h e mainland was u t i l i z e d as p a r t o f t h e d e f e n s i v e system i n t h e pre-Roman p e r i o d by t h e c o n s t r u c t i o n o f a rampart along i t s n o r t h - w e s t e r n edge running from a prominent granite Beaumanoir, a t t h e
  • 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
  • f t h e a n c i e n t v i l l a g e o f Le Yaudet and t h e r e l i c o f i t s f a r m l a n d , now abandoned. The s i t e was a c q u i r e d by t h e Departement o f Cote du Nord i n 1980, a t t h e r e q u e s t o f t h e Commune, t o p r o t e c t i t from development
  • i s c o v e r i e s made over t h e years have been c o n v e n i e n t l y summarized by L. Pape (1978, ASSASS) t o which may now be added a discussion o f C e l t i c and C a r t h a g i n i a n c o i n s from a n i n e t e e n t h c e n t u r y c o l l e c t i o n thought
  • t o have come from t h e s i t e (Sanquer 1983). Several excavations extensive nature. have taken place b u t none o f an I n 1935 a number o f s k e l e t o n s were d i s c o v e r e d c l o s e t o t h e church (parcelle 29). They were w i t h o u t d a t i n g
  • . To t h e west he uncovered a Roman gate which gave access t o a convenient of t h e c l i f f s . The e x c a v a t i o n has n o t been p u b l i s h e d b u t i n t e r i m accounts were prepared 1954, 1955). landing place a t the f o o t ( F l e u r i o t 1952, 1953, 1954a
  • a l (Garlan 1969). Finally, i n 1978, a s m a l l sondage was dug t o examine a c i r c l e , which appeared on an a i r photograph, i n advance o f t h e c r e a t i o n o f a car park. P o t t e r y o f Bronze Age type was r e p o r t e d . It i s c l e a r from
  • 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
  • d e p o s i t s was l i k e l y t o be good, w h i l e Trench 2 was l o c a t e d t o examine t h e s t r a t i g r a p h y i m m e d i a t e l y behind t h e Roman d e f e n s i v e w a l l . results, as w i l l be apparent from t h e d e s c r i p t i o n The t o follow
  • , exceeded our e x p e c t a t i o n s . Trench 1 Trench 1 , a c u t t i n g 23 m l o n g and 2 m wide, was dug i n an abandoned f i e l d ( p a r c e l l e 20), which l a y behind, t h a t i s t o t h e west, o f t h e rampart. A t t h e n o r t h end o f t h e t r e n c h s u b s o
  • and potsherds o f N e o l i t h i c and Bronze Age appearance together w i t h f l i n t Phase 2. flakes. I n t h e second phase a s h a l l o w scoop (F26) was dug t h r o u g h t h e o r i g i n a l t o p s o i l and i n t o t h e g r a n i t i c sand beneath t o a depth o f up t o
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. ARPI. Arqueología y Prehistoria del Interior peninsular 03– 2015
  • royale belge d’Anthropologie et de Préhistoire: 259276. Laporte L. 2010a: Innate and/or expressed identities: Their conceptualization through monumentality, funerary practices and grave goods? Some examples from the megalithic tradition of western France., Journal of Neolithic
  • Archaeology, 0, 0. Consultable à Laporte L. 2010b : Restauración, reconstrucción y apropiación : evolución de las arquitecturas megalíticas en el oeste de Francia, entre pasado y presente. Restauration, reconstruction, ap- ARPI
RAP02603.pdf (PCR Brécilien. étude interdisciplinaire d'une forêt mythique. bilan d'activités 2010. projet collectif de recherches)
RAP03187.pdf (QUIBERON (56). Beg er Vil : un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP 2015)
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
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)
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)
  • ., SHAW A., sous presse - Discoveries From La Manche: Five years of Early Prehistoric Research in the Channel Island of Jersey. Archaeology International, sous presse. RAVON A.-L. & LAFORGE M., 2015 - Présentation du PCR: Les premiers peuplements de l’Ouest de la France : dépôts
  • 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
  • of the Palaeolithic landscape at the western most tip of continental Europe: The shoreline seen by the Menez-Dregan dwellers. Environmental Archaeology, sous presse. MONNIER J.-L., RAVON A.-L., 2015 - Terra Amata et Menez-Dregan. Des industries du Paléolithique inférieur à rares bifaces et riches
  • , Quaternary International, RAVON A.-L., GAILLARD C., MONNIER J.-L., 2015 - Menez-Dregan (Plouhinec, Far Western Europe): the lithic industry from layer 7 and its Acheulian components, Quaternary International, sous presse. 5.2
  • – 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
  • /03/2015 : RAVON A.-L. & LAFORGE M., “Presentation of a new regional project: The first human settlements in North-Western France: pleistocene deposits and palaeolithic occupations in the Brittany region”, Jersey Research Meeting, Institute of Archaeology, Londres. 02/04/2015
  • , 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
  • and Environment alog the European Atlantic Coasts / Anciens peuplements littoraux et relations Homme/Milieu sur les côtes de l'Europe atlantique. Proceedings of the HOMER 2011 Conference, Vannes (France), 28/09-1/10/2011. British Archaeological Reports, International Series 2570, Oxford
RAP01858.pdf (les sites mésolithiques en Bretagne. rapport de 1re année de projet collectif de recherche)