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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
  • 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
  • T4 may be an indication of the extent of the much earlier site sealed by colluvium. The phosphate distribution of Al 16 may therefore reflect occupation of many periods, and consequently may not relate directly to the distribution patterns of the pottery. THE SEPTEMBER SEASON
  • , 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
  • cadastre shows part of the field to have been divided into narrow bands, but the excavated ditches neither run parai 1 el nor the fui 1 length of the field» They are therefore unlikely to be of a médiéval or post-medi eval date and may possibly be contemporary with the 'prehi stor i c
  • that outlying parts were contemporary» The absence of prehistoric pottery from the areas around thèse ditches may imply that they do not enclose other parts of the settlement» The occurrence of pits beyond the area of settlement that have been used for burning might argue for spécial i sed
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
  • . In some parts cadastral land-use, naming and road patterns themselves indicate former settlement sites, especially where very small fields of very mi scell aneous^ land-use are arranged in relation to tracks, like the curti 1 agesand clos that surround settlements both now
  • 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
  • interests put their mark on this landscape. The bank, which lies in an area of nineteenth-century meadow and is not shown on the ancien cadastre, may therefore relate to earlier land-use; the lynchet lies at the edge of the château arable, about which - at least - it should furnish some
  • 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
  • of évidence suggests intensive cultivation in the late middle âges that was limited in the early modem period with changes in the social status of the 1 andowner and in his method of 1 and management. 8 Envi ronmental , Pottery, Architectural and Language Work, 1984-85 In the course
  • 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
  • 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
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
  • levels to suggest that they for m part of an y destruction layer associated with the building. The greatest part of the stratification does, however, relate to the abandonment and démolition of the building. Most of the gable end wall was removed by digging down to the foundations (65
  • 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
  • ditch, whose function was not precisely established, followed by an other ditch and post holes relating to a timber phase of construction (one? of which was packed with black roofing slate (03-4)), followed by a phase of agricultural use. After this came three walls, two (7, 41
RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
  • archéologique (diagnostic, fouille, document final de synthèse, sondage, sauvetage…) sont des documents administratifs communicables au public, en application de la loi n° 78-753 du 17 juillet 1978 modifiée et portant diverses mesures d’amélioration des relations entre l’administration et le
  • Beg-er-Vil en relation avec le terrain, c’est ce mode de fonctionnement (stage individuel) qui sera mise en place les années à venir pour finaliser le tri de Beg-er-Vil. Il reste moins efficace que de prendre quelqu’un de former au tri en contrat ou que les stages collectifs qui
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
  • d’opération archéologique (diagnostic, fouille, document final de synthèse, sondage, sauvetage…) sont des documents administratifs communicables au public, en application de la loi n° 78-753 du 17 juillet 1978 modifiée et portant diverses mesures d’amélioration des relations entre
  • 81 Péré ou du Souc’h compte deux longs tumulus, la 1.- INTRODUCTION nécropole de Tusson en Charente en possède trois mais souvent un seul a été sondé ou fouillé nous Un long tumulus est un édifice néolithique empêchant de voir les relations architecturales et de très grande
  • possibi- Les études de visibilité ne permettent pas lité de navigation sur le Corniou est au contraire de définir un territoire associé au monument mais peu probable. N’importe quelle personne navi- une relation particulière avec le paysage (López- gante au niveau de l’embouchure
  • mieux voir quel impact vise l’édifice. doit être appréhendé pour chacun. Seulement Seule l’implantation reste la même lui offrant un dans ce cas, les relations de visibilité, les orienta- cadre. tions des couloirs, les jeux de perspective entre les ARPI. Arqueología y
  • morphologies et relations pour les édifices de la nécropole de Barnenez (Giot 1987 ; Giot et al. 1994). Remerciements La tenue de ces recherches a été assurée grâce aux financements de la Région Bretagne, de la communauté d’agglomération de Morlaix, du Conseil Général du Finistère, du
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
  • . 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
  • 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
  • Academy; we are deeply indebted to thèse bodies for their support. We are also especially p grateful to M. Plaine of the Musée de Géologie in the University of Rennes for assistance with identification of local schi stes and to Bill Campbell for use of his software 'Mapics'; to Pat
RAP01557.pdf (PLOULEC'H (22). le Yaudet. rapport final de synthèse de fouille programmée 1996-1998)
  • zone enclose. Une première zone (tranchée 27) fut fouillée en 1997, la seconde étant examinée en 1998. Ces deux tranchées contiguës seront ici considérées comme un ensemble unique. Le but premier de la fouille était d'examiner la relation du chemin laténien et de la structure de la
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP01710.pdf ((56). la ria d'Étel. rapport de prospection inventaire)
  • . Première mention = Données complémentaires» ^ o\o\ Nature de ropération = Année = t Responsable = ...G.K.£^f...hi&&$ï.. Année première mention = ....P.I.Q.S .p&ciï. '.P.A. ^ Organisme = /&.
RAP02929.pdf (SAINT-ALBAN (22). pa du Poirier, tranche 1. rapport de diagnostic)
  • graviers (Hi 2) précédé d’une interface mêlant les deux (Hi 1). Dans les zones particulièrement érodées par les travaux agricoles au centre de l’emprise, n’est même conservée que cette interface sur des épaisseurs oscillant entre 0,30 m et 0,40 m. Dans les autres secteurs, entre 0,40 m
  • et 0,60 m de profondeur, un troisième horizon plus argileux apparaît localement  : très argileux et oxydé (Hi 3 - TR 1, Hi 6 - TR 26), blanchâtre dans le nord (Hi 4 - TR 4), gris dans le sud-ouest de l’emprise (Hi 5 - TR 18, 22, 21, 23). Plus généralement, le caractère très
  • . Altérites des métasédiments briovériens détritiques, micaschistes Fig. 3 Contexte géologique de l’opération © IGN, St. Le Berre / INRAP 2014. 95 TR 19 TR 22 96 .00 Hi 5 Hi 1 / Hi2 TV TR 23 TR 21 TR 18 TR 13 98 .00 800 95 .00 94.50 700 X=1 98 .50 Ech. 1: 2000 0 Fig
  • . 4 Contexte topographique de l’opération et profondeurs d’apparition des structures © St. Le Berre / INRAP 2014. TR 24 TR 25 TR 17 TR 12 290 97.50 600 290 X=1 .50 TR 20 TR 16 0 TV TR 4 TR 10 TR 9 TR 11 TR 8 TR 7 TR 6 TR 5 Hi 2 Hi 4 290 800 TR 3 TR 27 TR 2
  • N 150 m Y=7 276 400 Y=7 276 500 argile d’altération altérite de gabbro TR 1 Centre technique communautaire X=1 Hi 1 .20 - 0,50 à - 0,60 m - 0,40 à - 0,50 m - 0,30 à - 0,40 m Profondeur d’apparition 300 276 Y=7 400 276 Y=7 TR 15 96.5 Hi 1 / Hi 2 700 TR 26
  • 97.00 TV 290 X=1 900 TR 14 290 X=1 99.00 290 X=1 TV / Hi 1 tion ZB TV Hi 1 TV Hi 2 Hi 1 Ech 1 : 50 0 S ec TV Hi 1 1m Hi 3 II -Résultats archéologiques 25 99 99 .20 26 Inrap · RFO de diagnostic Saint-Alban (Côtes d’Armor) P.A. du Poirier, tranche 1 1.3
  • TR 1 - F. 8 et F.9 F. 4 F. 20 F. 21 O E TV F. 5 F. 6 Hi 1 1 5 2 6 F. 7 3 4 TR 27 F. 8 F. 9 1 2 3 4 5 6 Argile limoneuse gris foncé, meuble, peu oxydée, rares graviers = Hi 3 ? Argile limoneuse grise, compacte, moyennement oxydée, quelques graviers. Argile grise
  • ( = F. 84) OSO ENE TV ornières F. 10 / 11 Hi 2 1 4 2 3 5 6 extension 1 F. 12 ? 1 2 3 4 5 6 Limon brun gris foncé. Argile limoneuse grise, très fortement oxydée, quelques graviers et blocs de schiste. Argile grise, très oxydée, quelques graviers et manganèse. Argile
  • matérialiser l’existence d’un passage. Dans l’état de nos connaissances, il est impossible de définir véritablement la fonction de ces trois fossés ni leur relations chronologiques. Le fossé F. 9 sert à la fois de limite parcellaire forte et de fossé drainant alors que les fossés F. 5 et F
  • . 8 jouent, quant à eux, un rôle plus modeste. Toutefois, ces derniers Saint-Alban (Côtes d’Armor) P.A. du Poirier, tranche 1 34 TR 12 N TR 23 - F. 77 / 89 / 75 S N TV TR 16 F. 57 TV Hi 1 F. 56 Hi 5 Hi 1 1 2 Hi 5 3 5 F. 59 6 4 F. 60 F 89 F. 60 1 2 3 4 5 6
  • 1 F. 71 TR 19 TV TV TV Hi 1 Hi 5 Hi 1 Hi 1 Hi 5 2 3 Hi 5 1 Limon argileux gris avec inclusions d’argile orangée et manganèse. 2 Limon argileux gris avec inclusions de gravier et manganèse. 3 Limon argileux gris avec inclusions d’argile orangée, de manganèse et de
  • graviers. F. 57 TR 21 TR 22 TR 22 - F. 73 TR 19 - F. 71 F. 74 F. 77 E O E O TV F. 73 TV Hi 1 F. 75 Hi 5 1 Hi 1 0 Ech 1 : 50 1 F. 78 1 Limon argileux gris clair avec inclusions de manganèse. F. 88 TR 23 F. 76 F. 89 0 10 m Ech 1 : 750 TR. 18 - F. 57, coupe
  • est installé dans un horizon argileux plus ancien (Hi 5). La trame s’organise autour de trois axes perpendiculaires. L’axe le plus important est le fossé F. 75, observé dans les tranchées 19, 22 et 23 (Fig. 13 et Fig. 14). Orienté est-sud-est / ouest-nord-ouest, il est conservé sur
  • : 250 TR 4 - F. 39 / F. 85 / F. 86 S N N S TV Hi 1 1 F. 39 4 3 7 6 5 Stériles Hi 2 1 3 4 2 7 6 F. 39 / F. 86 F. 85 F. 85 0 1m Ech 1 : 50 1 2 3 4 5 6 7 Argile brun-gris foncé, meuble, homogène, très oxydée. Argile grise, mêlée de substrat remanié, meuble
  • 2 Fig. 19 Plans et coupes de la fosse d’extraction F. 63 et des fours F. 61 et F. 62 de la tranchée 14 © St. Le Berre / INRAP 2014. 5 4 1 Hi 1 / Hi 2 F. 62 Coupe 2 du sondage © St. Le Berre / INRAP 2014. us 6 coupe 2 1 2 3 4 5 SSE 2 NNO F. 63 Ech. 1 : 50 0 Soles
RAP03654 (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport intermédiaire 2018 de FP 2017-2019)
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
RAP03300.pdf (RANNEE (35). La Chaussée. Rapport de fouille)
  • , with the western wall of the building perhaps functioning with a palisade. Modern pits related to the planting of trees as well as drains and parcel boundaries are present throughout the study area, with some of the structures identifiable on the Napoleonic maps ; others remain as visible marks
  • relations stratigraphiques observées relèvent principalement de recoupement de fossés modernes/contemporains avec les fossés latèniens. L’étude céramique ne vient cependant pas pallier ce manque car la datation de l’ensemble céramique est centré sur les IIe-Ier siècle avant J.-C. De plus
  • communicables au public, en application de la loi n° 78-753 du 17 juillet 1978 modifiée et portant diverses mesures d’amélioration des relations entre l’administration et le public. L'accès à ces documents administratifs s’exerce auprès des administrations qui les ont élaborés ou qui les
  • 1978 modifiée relative à l'amélioration des relations entre l'administration et le public). Le non respect des règles qui précèdent peut constituer un délit de contrefaçon passible de trois ans d'emprisonnement et de 300 000 euros d'amende (articles L335-3 et L335-2 du CPI). Pour
  • de ces deux fossés septentrionaux, très peu d'éléments permettent de retracer les différentes étapes de structuration et de modification de cet établissement. En effet, la majorité des relations stratigraphiques observées relèvent principalement de recoupement de fossés modernes
  • the site are primarily composed of silty clays (fig 1). The primary objective of the excavation was to compliment data previously acquired in 1990 during the aerial surveys of Gilles Leroux, and recovered by the 1999 test excavations of J.-C. Meuret. These earlier studies identified
  • 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
  • between this two northern ditches, there is little evidence demonstrating the structuring and modification of the site. Indeed, the majority of the observed stratigraphic relationships are primarily modern / contemporary ditches that cut the earlier late Iron Age structures
  • 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
  • on the landscape today. Overall, the density of structures and artefacts recovered from the study area was relatively low, suggesting a short occupation. 4 ÉTAT DU SITE L’occupation se poursuit à l’ouest et à l’est de l’emprise de fouille comme l’attestent les photographies aériennes de G
  • Tertiaire. Cette US correspond, au plus profond des sondages, à une roche meuble au sein de laquelle la texture originelle de la roche-mère et les relations spatiales entre les minéraux sont conservés. On parle alors d'isaltérite, surmontant la roche-mère fissurée mais saine, et
RAP03312.pdf (CHARTRES-DE-BRETAGNE (35). ZAC des Portes de la Seiche, tranche 1B1. Rapport de fouille)
  • rapports d’opération archéologique (diagnostic, fouille, document final de synthèse, sondage, sauvetage…) sont des documents administratifs communicables au public, en application de la loi n° 78-753 du 17 juillet 1978 modifiée et portant diverses mesures d’amélioration des relations
  • relations entre l'administration et le public). Le non respect des règles qui précèdent peut constituer un délit de contrefaçon passible de trois ans d'emprisonnement et de 300 000 euros d'amende (articles L335-3 et L335-2 du CPI). Pour citer ce document Leroy 2016 : LEROYO B., Chartres
  • en lien avec les dernières productions potières du début du XXe siècle à Chartres-de-Bretagne. 4 ABSTRACT The excavation located in Chartres-de-Bretagne, ZAC des Portes de la Seiche, have revealed remains from medieval, modern and contemporary period. The main layout is dated
  • to the late medieval and early modern period. Two lime kilns, related to a ditch system and the foundations of a little building have been found. The kilns and building 's datations revealed that they were in use from the second half of the XIVe century to the second half of the XVe
  • century. After their abandonment, the kilns and the entire space were subjected to several phases of fillings between modern and contemporary period. A quarry for extracting clay, located into an ancient pond was partially revealed. It would mesured about 4 000 m². The extraction
RAP01583.pdf ((35). le bassin de Rennes. rapport de prospection inventaire)
  • connexions entre sites sont possibles (cas des "grands domaines") mais aussi un questionnement sur le rapport entre le site et son environnement. Qu'il soit naturel : relation avec les sol travaillés, exposition au vent, présence de cours d'eau, de nappe phréatique ou de source
  • au travers des relations des sites avec leur environnement ne suffit pas : il faut également s'interroger sur la continuité ( ou la non continuité) de l'occupation humaine dans certains secteurs. A ce niveau l'absence de site, si elle peut être affirmée, dans un secteur cohérent