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RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
  • 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
  • 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
  • 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
  • similar to médiéval and modem pottery and could have been introduced on to the surface. The small quantities of archaeol ogical material recovered, and its gênerai distribution, suggest that it was brought on to the field in the course of manuring; quantities, pattern of distribution
  • . The results confirm the impression that this 1 and was not brought into cultivation until the twentieth century, and confirm the classification made on the basis of transect walking - the field real ly is 1 bl ank 1 . B347 lies on a slight east-facing slope at 35m, beside a stream, and its
  • , a concentration of médiéval pottery ('site') discovered in the course of transect walking in 1982. In 1983 a 'total' collection was organised over the same area, with geophysical and geochemical prospection. The results suggested that there was domestic occupation on some part of the field
  • lynchet some 1.8m high. This area is near the northern periphery of the Ruffiac commune, and the ancien cadastre indicates that it was a zone of extensive 1 ande in the early nineteenth century. Set within the 1 ande was the petit château of Coetion, with its metai ries (associated
  • 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
  • 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
  • quantities of surface material are no sure guide to the ci rcumstances of its déposition: distribution over the field is as significant as quantity and fields - and even gardens - beside long-establ ished inhabited settlements do not necessarily produce the greatest quantities of material
  • 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
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
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)
RAP01858.pdf (les sites mésolithiques en Bretagne. rapport de 1re année de projet collectif de recherche)
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • by the early post médiéval period (Asti 11 and Davies 1985s 92-5, 97)» If the occupation in T4 is prehistoric then it is the first of its kind for the? région and has important implications for survey work» Its low-lying position, in a wet valley bottom and sealed by 70cm of colluvium
  • 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
  • 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 man-made building mater i al were recovered frorn the transects; 6.47. of the pottery was Roman, 34.87. médiéval and 58.8?/;, post-medi evail » This is consi derabl y more brick and tile than recovered in each previous season, rather more Roman pottery and rather less médiéval. Ten
  • were walked (of which to be covered (see fig. B) » hectares (18% of the surface area 6 were in M), encompassing 257 of Transect N) . 7.86kg of pottery and 13.81kg of man-made building material were recovered from thèse transects; 1.37. of the pottery was pre-Roman „ 1% Roman, 29.7
  • because of the weather. Quadrats with 6m si des were chosen since a smal 1er cutting could fall within a structure, failing to reveal its existence. However, in the later stages of the excavation a machine (JCB) was used to eut three 1m wide trenches to extend the investigation
  • 145 10m 0 10 20 F i g. 2 \4- 30 UQ 50 m H145 (Tréai ZB154a) This field was classified as a 'possible site' (médiéval) after •f i el dwal ki ng at 50m intervais in 1984» Intensive collection •from the whole of its surface in March 3.986 indicated smal 1 quanti ti es
  • arable land-use and smal 1 enclosures (çl_os) , with two buildings and ? walled yards inside its western edge - since démoli shed. The site of thèse buildings i s presumably now marked by a remembrement mound near the junction of the two road s. Excavation strategy was the same
  • not reveal were any f eat ures ., Trench 12 The trench was excavated by machine and -for most of its 28m length merely provided a record of the depth of plough soil» However in its extrême north end a section of stone walling was excavated- The wall, 30cm high, consisted of coursed
  • , nearest the settlement of Becul eu. A shallow (15cm) pit rnay be dated by the single médiéval sherd in its filling (5), and may be associated with other features which apparent 1 y constitute a roadway. A deep (2m) ditch or holloway (66) had either been eut or worn into the natural
  • ). The surface had been fragmented through plough destruction. Five mètres south of the holloway a ditch 1.5m wide and 45cm deep was excavated (.1.0); its filling contained one médiéval sherd of pottery (7, 8, 9). It was apparently on the same alignment as the holloway and had silted up
  • Its in the holloway wi 1 i provide an interesting comparison with those samples taken -from the lower plough soi 1 s in T24 and T25 , which may be expected to be colluvial in charaicter. ^1 H80 (Treal ZN4b) 1-180 is located right on the western edge of Treal commune, some 150m
  • , 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
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
  • . An oval pit (29: 1.15 x 0.6m and 0.08m deep with fill 30) had been eut by a circular pit (17: diameter 0.75m and 0.15m deep) which had a thick deposit of charcoal (14) in its base and then a sandy fill (18). This had in turn been eut by a circular pit (19: 0.6m diameter and 0.1m deep
  • without more extensive investigation. The séquence from T36 is important. The trench was sited on the highest part of the field, near the top of the slope, yet it has a much deeper stratification than T37 lower down the slope. The buried soil 32, with its charcoal, might represent
  • into natural. The edges were not as clearly defined as ditch 5, and the profile was more irregular; a 2m length was excavated, which was 0.6m deep and 1.2m wide. Although it was parallel with 5, its filling (12) was much sandier and the range of finds was différent. Large quanti ties
  • and ear 1 y Roman pottery in its fills, and the virtual absence of roof tile, implies that it had been filled before the buildings went put of use; the pebbly, foreign, nature of the fills shows that thèse were deliberate. This ditch may have been in existence before the structure
  • was built and may have been made redundant by its construction - hence the fills. Although, then, excavation of A92 was very limited, it cl earl y demonstrates that. there was a Roman-period building on or near the ridge, which was occupied in the first and second centuries
  • southerly, 0.S lm wide and 0.4m deep (51: filled with 50), appears to have been reçut, for a smaller ditch (80: fill 81) 0.5m wide and 0.15m deep had removed the eastern side of ditch 51. Neither ditch produced finds. Ditch 53 was wider (1.2m) and deeper (0.5m) and its fill (52) contai
  • ned four' sherds of southern Gaulish Sami an , and one of grey coarse ware (Fabric 37). The most northerly ditch (55) was 0.9m wide and 0.4m deep, and from its fill (54) came three pièces of tile (Fabric 1). In so far as can be seen in a narrow trench, the three ditches appear
  • was to check the course of thèse ditches, and both original ditch and reçut were found; however they produced neither pottery nor tile. A f 1 at-bottomed pit (17), 1.4m wide and 0.5m deep , was located close to ditch 3. Its fill (18) contained 3.7kg of tile (Fabric 1) , 7kg of quartz, one
  • dug parallel, 6.4m apart. Ditch 19, 1.75m wide and 0.6 m deep, had within its fill (20) two sherd s of late Iron- Age/ear 1 y Roman pottery (Fabric 13) and 6 small pièces of iron— working slag. The more northerly ditch, 2:4, had a primary silt (60) with no finds and then a loam
  • and was différent from the other ditches located on the site; its fill (11) yielded no finds. This may represent another récent attempt at drainage. The trench al so eut through the earthwork which was located at the bottom of the slope; no additional layers were found and it seemed
  • 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
  • and ditches. A f 1 at-bottomed ditch, 0.5m wide and 0.2m deep (42), was e:;cavated; its fill (41) contained a ri m of a late Iron-Age/earl y Roman fabric (Fabric 13) and 7 sherds of grey coarse wares (Fabrics 57 and 100) with a small quanti t. y of ceramic roof tile (Fabric. 1, 0.81kg
  • tile (Fabric 1, 0.778kg). A large ditch (61), 2m wide and 1.5m deep, was located two mètres farther down the slope. It had a 'U' shaped profile and its primary fill (59) contained a late Iron-Age/Roman rim sherd, a terra-ni qra-type spout of a f lagon and a sherd from what seems
  • the second century, or even in the prehi stor i c period, since i t does not respect, any of the? demonstrâbly Roman ditches or pits (see fig. 4). It is, however, différent from other s that have been excavated: the 1 ynchet lacks a ditch or bank at its core, as did Tl , T2, and T35 (see
  • . The pottery was abraded, which implies that some time and/or distance separated its use as pottery from its place of déposition in A31/79. Now, the pits were largely confined to the ridge while a séries of approx i mat el y parai lel ditches, most with the same profile, extended from
  • that this phase of agricultural land-use lasted for some time without fresh sherds being added; indeed, at least. two ditches were reçut. There is, however, one ditch R (64) and its reçut (3) that do not fit this pattern for they were larger and were dug at right angles to the other
  • material collected from this field originally suggested thaï i t was a likely site to find évidence of continuity from Roman into later periods, with its distribution of Roman, médiéval and post-medi eval pottery and brick and tile too, as wel 1 as earthworks. It is therefore very
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
  • 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
  • predomi nanti y médiéval or predomi nanti y post-medi eval sherds, others more than the necessary minimum proportions of médiéval and post-medi eval sherds, and others had a prédominance of man-made building material. The proportions of such concentrations are as follows, by transect
  • : 115). P is notable for its relatively high proportion of fields with significant concentrations of surface material, high by comparison both with Transects M and R as also by comparison with the core, where fields with notable concentrations averaged only 24.27. of those walked
  • of material (15.67. 'possible', 177. 'probable' and 4.57. 'site'). Transect M itself produced unusually high quanti ti es of brick and tile, and a high proportion of its concentrations were characterized by brick and tile - some of which had Roman pottery associated. Transect R was notable
  • 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
  • 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
  • scatter with Roman material lies near the bourg of Comblessac and not on some distant periphery, as is more usual . In Transect M there were 'blank' areas on the banks of the River Aff and its tributaries but most notable was a very marked and very large 'blank' zone in the commune
  • 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
  • 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
RAP03350_2.pdf (SARZEAU (56). Le château de Suscinio : le logis nord. Rapport de FP 2013-2015)
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
RAP02211.pdf (ÎLE-MOLÈNE (29). beg ar loued. un habitat en pierres sèches de la fin du néolithique / âge du bronze ancien. rapport de fp 1)
RAP02367.pdf (BERNÉ (56). rapport de sondages archéologiques sous des pieds de fragon petit houx en forêt domaniale de Pont-Calleck)
  • accrochées aux cladodes2 des mois durant. Hillman pense qu'au regard de la possible origine méditerranéenne du fragon, l'agent disperseur n'est pas forcément présent en Grande-Bretagne où a été effectué le suivi. Outre l'avifaune, sur les îles d'Hyères, certains contenus stomacaux de rats
  • ' i 1 a du être appel é épine de rat en France ou mâusedorn4 en Allemagne (Rameau, 1989). Cette propriété peut aussi lui valoir une forme de sélection au niveau des haies, afin de renforcer l'effet barrière. Sûrement du fait de ces différentes propriétés, le docteur Chassagne
RAP03070.pdf (DOMLOUP (35). le Petit Bénazé : une occupation du Ier au IIIe s ap. J.-C. aperçu sur l'organisation de l'espace rural en territoire riedone. rapport de fouille)
  • Fouille archéologique Rapport d’opération LGV Le Mans-Rennes, section 1 Domloup, Ille-et-Vilaine, Le Petit Bénazé Une occupation du Ier au IIIe siècle après J.C., aperçu sur l’organisation de l’espace rural en territoire riedone sous la direction de Anne-Louise Hamon Inrap
  • Grand Ouest janvier 2015 35099 Fouille archéologique Rapport d’opération Code INSEE 2012 - 017 — Arrêté de prescription Système d’information Code Inrap DB05030809 LGV Le Mans-Rennes, section 1 Domloup, Ille-et-Vilaine, Le Petit Bénazé Une occupation du Ier au IIIe siècle
  • scientifiques Notice scientifique Découvert en 1985 lors de prospections pédestres, le site gallo-romain du Petit Bénazé, placé sur le tracé de la Ligne à Grande Vitesse Le Mans-Rennes a fait l’objet d’un diagnostic archéologique en 2011, auquel a fait suite en 2012 la fouille sur 1.6ha
  • d’implantation d’une nouvelle ligne ferroviaire à grande vitesse par le groupe Eiffage Rail Express entre les villes de Le Mans et de Rennes est à l’origine de la mise en place d’une campagne de sondages archéologiques menée entre les années 2010 et 2012 sur les trois sections de la ligne, en
  • . Fig.4 Gabarits pour engins de chantier. © Inrap Intégrée dans la série de chantiers prévus sur la LGV Le Mans-Rennes, la fouille du site archéologique du Petit Bénazé a suivi les directives du Plan général de sécurité émis par le maitre d’ouvrage gérant l’ensemble des travaux de
  • . (Ouest France 2012) L’abondance de données archéologiques obtenues à l’occasion de la création de la ligne LGV Le Mans-Rennes a donné lieu à la mise en place d’une exposition itinérante qui, en synthétisant les résultats des opérations de fouille a permis la diffusion des principales
  • archéologique menée durant l’année 2011 par Sandrine Barbeau (Inrap) sur le secteur 1 de la LGV Le Mans-Rennes (Barbeau 2011). La mise en évidence d’un reste de mur et de nombreuses structures en creux dont les comblements livraient des éléments céramiques datés du premier au troisième
  • -Juliomagus) à proximité de laquelle plusieurs sites bâtis semblent fonctionner en lien étroit, et, plus au nord, un second tracé avec la voie reliant Rennes à Le Mans (Condate à Vindunum). Condate, capitale des riedones créée ex nihilo aux tout débuts de l’Empire, connait, entre le
  • l’espace rural en territoire riedone Le Mans Le Petit Bénazé Angers 0 1km Enclos gallo-romain Enclos âge du fer Enclos non daté Villa, bâtiment en dur Gisement de surface gallo romain Diverses occupations gallo-romaines fouillées Funéraire gallo-romain Funéraire non daté Fig.10a
  • numéro 27 : La Retardais). Dans le cadre des fouilles effectuées sur le tracé de la ligne LGV Rennes-Le Mans, nous signalerons également l’étude du site de la Salmondière, occupé des âges des métaux au haut moyen-âge. Placé à 1200m au nord-ouest de notre décapage, il se compose d’un
RAP03654 (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport intermédiaire 2018 de FP 2017-2019)
  • (rouge : réalisées sur fragments osseux indéterminés). 9.2. État de conservation des niveaux archéologiques Comme beaucoup de sites en abris, le gisement du Rocher de l’Impératrice a connu une histoire complexe aux implications parfois importantes pour la conservation des niveaux
RAP03565 (PLUMAUGAT (22). Saint-Pierre : un vaste étabissement de la fin de l'âge du Fer. Rapport de fouille)
  • Dinetière à Brielles sur le tracé de la LGV Rennes-Le Mans (D.Pouille, Inrap, août 2011) où un site d’habitat de l’époque romaine vient supplanter une occupation de la Tène, matérialisée par un important fossé comblé à la Tène finale. On peut également mentionner les sites antiques de
  • suggérer la présence d’un ou plusieurs bâtiments. Celles-ci feront l’objet d’un décapage puis d’une fouille fine afin d’en restituer un plan précis. Enfin, les éléments isolés et déconnectés de toute implication dans la compréhension du site seront négligés. En complément des datations
RAP00782.pdf (MELRAND (56). lann gouh. rapport de fouille programmée)
  • circulati c 0 n cou ran t e n une p e t ite place située à 1 ' e n d r o i t le plus élevé du s i t e . De u x de ce s axes, vers le nord et vers 1 'ouest débouchent v e r s 1 ' e x t é r leur, t an dis que la branche sud-es t d escend vers un e a u tre pl ace, un P eu plus grande, en t
  • < OiY\ 22 La r éd a c t i o n des fi c h e s a é t é dictée par de ux i mpé rat ifs : les p r i n c i P e s thé o r i q u e s r api d eme n t rappelés c i - dessus e t bien d é v e 1 o p p é s pa r 1' équipe d e La ttes ï mais aussi le s c a r a c t é r istiques du s i te, c ' e s