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)

732 résultats Exporter les résultats

Trier par Titre : ascendant / descendant
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • the same corner and was 4.5m long; T44 was eut north from the north-east corner of T28 for 4.4m (fig. 3). In T42 two ditches were located eut into the natural . One (24) was lm wide and about 0.2m deep and was fi lied with a loam (23) similar to the plough soil. The other (39) was much
  • suggests that the building did not stand long after the second century, and hence that this ditch fill from the building took place at or shortly after that time. It is difficult to suggest a function for the earlier ditch (5 and 10) other than for drainage. The présence of Iron-Age
  • and reached a maximum depth of 0.35m: this point corresponded with the break in slope. No finds were recovered from layer 4. The only other feature located in T39 was 18m from the north end of the trench and was a shal 1 ow-si ded 'ditch' 0.15m deep (5). It had an irregular profile
  • 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
  • that the clay subsoil at this point had a configuration similéir to that on the surface of the field. In other words, the break in slope mirrors the undulation of the subsoil and is probably a natural feature, perhaps a river ter rate. Trench 41 T41 was 113m long and the depth
  • 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
  • (30 and 57); they did not eut each other. The fill (56) of pit 57 had 1 sherd of a Roman grey coarseware (Fabric 216); that. of pit 30 (29) produced no finds. There? were no features in the trench for a long section of the slope, some 26m, and then there was a further group of pits
  • 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
  • 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
  • : 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
  • ) and then the stones laid on top (51) (fig. 6). This wall, like 7 and 41, had very large blocks of quartz, altered schi ste and conglomerate in its base, and had similar stone to 7 in its other 365kg, although it had more quartzite (7%), more Cambrian siltstone (27.) and 1 ess altered schi ste (22
  • ; most of it. had clearly been protected from plough damage, despite its présence? in the plough soil. The pottery from the other contexts was not di f f erenti ated by layer or feature; hence, the pottery in buried soil 20/29 and in the features eut into the subsoil was still predomi
  • riant 1 y made from Fabric 1. There was indeed one sherd of Roman ware from the earl i est ditch fill (39) but this i s évidence? too slight to suggest any dating for the feature, qui te apart from the façt that other features were eut into it. The other features had 2 sherds
  • 5, an orange ware, was found in jug and bowl forms. The forms of cooking ware are similar to those found on médiéval sites excavated in the Landes de Lanvaux (André 1974). The most common type of rim (34 examples) is that of the gai etti er e; other open bowl forms were comparati
  • 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
  • ) belonging to a substantiel building with massive foundation material, a building which included a hearth at an early phase of use and which later had a substantiel extension (51) attached and a séries of floor levellings; the rël ati onshi p of the other, and much 1 ess substantiel, wall
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • ; 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
  • acing slopes. Upland concentrations were less notable than in 1984 (transects H, J, K) with only a quarter lying between the 50m and 75m contours; more than half 1 ay between 25m and 50m (59.9%), as in the other Carentoir transects. Only 35.3% of sites 1 ay within 250m of streams
  • , and rather more variation than did the other fields, with some tendency for lower readings in the area of the brick/tile/Roman cl ustering. A pl atf orm at the north-western edge of the field produced little material of any type; it is likely that this area has been ploughed down
  • usters of other classes of material. 5 Excavations (EBS85 Tl and T2) Small -scale excavation of earthworks was undertaken in order to begin investigation of the soils and archaeology within field boundaries near sites identified in fieldwalking. As indicated previously, one
  • and 40cm, as was also true of the other material. The pottery, brick, tile and also this schi ste were probably brought on to the field in the course of manuring. Trench 2. The remains of a bank, only 20cm high, were found lying on the natural, midway along the trench. The bank
  • and tile coul d indicate that this happened before brick and tile were in common use. Both trenches have shown that lynchets could have a complicated history, with their origins in other features. From the point of view of land-use history, the pottery suggests that this area of Ruffiac
  • and proposed - as part of an investigation into the application of microscopic techniques to the identification of traces of agricultural and pastoral activities in the soils and sédiments a sustained programme of soil analysis in close association with other field and archive work
  • by the récognition of characteristic seventeenthand 1 ate nineteenth-century types. It is clear that some settlements have a prépondérance of one or other of the two common types of building - the single cell , with ground floor hall and storage loft above, and the long-house, combining byre
  • course, sometimes fields by inhabited settlements produce plenty of material, such as other parts of Gaincru, the field beside La Charmille on the outskirts of Ruffiac, and those beside the château of Peccaduc; most notable are the quantities in and lO around the small settlement
  • as coniferous) can hardly be more than two hundred years old. In such ways surface scatters, in association with other évidence, are beginning to suggest precisely localisable changes in land-use, especially during the 1 ast millenium. This year also saw a major attack on the problem
  • cleared woodland (F231, F594, C405, C436, for example). It is therefore at least a useful indicator of pre-twentieth-century arable. However, there are also différences in colour combinations for there are zones with ail three colours, others without pink-purple and others with black
RAP02046.pdf (PAIMPONT (35). paléosidérurgie diachronique du massif de Paimpont. le vert pignon III : découverte de fours métallurgiques en activité autour du XVe siècle. rapport de prospection thématique avec sondages)
  • . No students or intern researchers who would necessarily be distracted with other obligations and priorities were used in the analyses. We analyzed them with the combined attention of our entire professional staff. Information pages are also enclosed with the mailed copy of this report
  • biogenic activity incorporating récent carbon (bacteria) and the analysis of multiple components of differing âge are just some examples of potential problems. The pretreatment philosophy is to reduce the sample to a single component, where possible, to minimize the added subjectivity
  • materials assume that the material dated was living for exactly ten years (e.g. a collection of 10 individual tree rings taken from the outer portion of a tree that was eut down to produce the sample in the feature dated). For other materials, the maximum and minimum calibrated âge
RAP02448.pdf (SAINT-VOUGAY (29). l'esplanade nord du château de Kerjean. archéologie des jardins. rapport final de synthèse de fp2 1998-1999.)
  • palynologiques au Château de Kerjean 5.3. ANALYSE DU VEGETAL ACTUEL 5. 3. 1 - inventaire et caractéristiques des essences végétales actuelles de l'esplanade 5. 3. 2 - Essai d'interprétation CONCLUSION 3 1 1 ..tamji ,7, ! . St-LO,' i/o Chausey ,> SNl hstf Avranch uc .hateaulin
  • le bois régulier. Elles ont toutes montré un horizon de labour reposant directement sur le socle granitique. Nous avons également veillé à mener une approche pluridisciplinaire en y associant des compétences diverses afin de garantir une approche prudente de tout essai
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • and two others, returned on 28 April for three days in order to complète the excavations. Overall, 317 mandays were spent on this year's Easter seasons (303 by the main team), including travelling time and time off 5 255 (244) of thèse were working days. The weather was dreadful
  • marked patterns» Such schi stes were présent on most fields (largely as a resuit of manuring), with the exception of some areas of 1 an de in the northern part of Transect B and of some isolated, scattered fields (D6 and 7, E267) with no other surface material. However , it was again
  • 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
  • . 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
  • previously recorded from the site. Three of thèse sherds were of a sandy fabric with large rounded quartz inclusions (1mm) and a notable absence of mica. One, a ri m sherçj, has parallèle with later Iron Age forms from Brittany (La Tene Finale) (Biot, Briard and Papes 331—9) » The other
  • of this deposit in T5 and T6 made it clear that the platform earthwork was a lynchet, similar in character to the? lynchet sectioned in 1985 on the other si de of the valley. Around the crest of the lynchet a slight change in the colour and texture of the 1 owest colluvium (T5, context 4) may
  • 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
  • . The depth of the plough soil varied between 30 and 50cm and in some places overlay the natural clay subsoil and in others the natural bedrock. No archaeol ogi cal features were encountered ., Trench 11 The plough soil was excavated by hand and found to be between 35 and 45cm deep. It 1
  • , 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
  • days were spent on site, with an average team of 6. The majority of features excavated were sections of ditches. An account. of al 1 thèse would be repetitious; instead the détails are tabulated after a discussion, by trench, of the other contexts. Al I the ditches had been dug
  • of this feature is that it represents the eaves trench, 16.8m in diameter, of a circular structure. No internai features were located in T15 however, nor was the other si de of the 'eaves trench' located in T17, although T17 could have gone through a causewayed entrance. Al ternat i vel y
  • reçut (35/50, 37/51). Trench 21 Four ditches were excavated (41, 42, 47, 49), détails of which are given below. The only other feature wais a modem tree hole (46) ". Trench 22 S by 4m was cleared of approx i matel y An irregular area Of plough soil and a deposit of hard stone
  • , 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
  • settlement» Some of those close to the pit group 7 do have small quanti ti es of prehistoric material (8, 25) but other s in the same trenches do not» This might imply that the disposai of rubbish was confined to the settlement area, and therefore it would be difficult to show
  • 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
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
  • du laboratoire « Anthropologie-PréhistoireProtohistoire-Quaternaire Armoricains », Rennes, 1987 GOULETQUER P. (1991) - Barnenez-Ar-Zant et ses symboles, La Bretagne linguistique, 7, p.p. 103 134. GOULETQUER P. (1993) - Essai de synthèse, Penn Ar Bed, , 148/149, p.p. 83 92. STÉPHAN
  • Barnenez’s term is associated to the cairn, excavated and restored during the 50-60’s by PierreRoland Giot. It seems isolated now but other adjacent buildings are known and specially a second long tumulus next to the cairn at its north. This work wants to bring to light this monuments
  • .-R., Chauris L., Morzadec H. 1995: L’apport de la pétrographie à l’archéologie préhistorique Gouletquer P. 1991: Barnenez-Ar-Zant et ses symboles. La Bretagne linguistique, 7: 103-134. Gouletquer P. 1993: Essai de synthèse. Penn Ar Bed, 148/149: 83-92. Le Guennec L. 1979: Le
RAP03801 (Corpus des signes gravés néolithiques, Art rupestre néolithique en Armorique. Rapport PCR.)
RAP03659 (Corpus des signés gravés néolithiques. Rapport de PCR 2018)
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
  • en charge celles concernant Beg-er-Vil. Des essais seront menés sur des ossements de ce site, afin d'affiner la chronologie de l'amas. Ludovic Soler présente son projet de thèse concernant l'anthropologie des populations mésolithiques et néolithiques sur la façade atlantique. Il
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
  • 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
RAP02287.pdf ((35). étude documentaire. étude documentaire préalable à la mise en valeur du couvent des jacobins de Rennes)
  • repris par l'abbé Henri Poisson, Essai de 8 2 83 8 4 8 5 8 6 8 7 8 8 monographie de la paroisse de Saint-Aubin en Notre-Dame de Bonne-Nouvelle, Rennes, 1935. Le témoignage contemporain d'Yves Pinsard permet de mesurer la ferveur entretenue autour du tableau : « Dieu semble si
RAP00141.pdf (ARZON (56). Bilgroix. pointe de Bilgroix. rapport de fouille programmée.)
  • Aff, 35. Bruzulier Jean Luc,professeur d'Histoire, Vannes, 56. Draper John, étudiant en Histoire, Reading, Gde Bret. Evain Paulette, institutrice, la Baule, 44. Fernandez Gonzalez Sabela,étudiante en Philosophie, Pontevedra, Espagne. Gabernet Laetitia, étudiante en Médecine
  • , Mirande, 32. Garcia Sanchez Natalia, étudiante Tourisme,à la Corogne Giomez Sanin Asuncion, étudiante en Philosophie, Ponteve- Ficjl • Extrait de la carte IGN 1/25000 Vannes-Golfe du Morbihan. 4 * i ^0^*^^^%,^ Route d'accès à la pointe de Bilgroix ; Site de Bilgroix, Arzon
RAP03654 (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport intermédiaire 2018 de FP 2017-2019)
RAP02357.pdf (SAINT-MARCEL (56). "la Sente Verte". le bourg. rapport final d'opération de fouille préventive)
RAP03523 (Corpus des signes gravés néolithiques. Rapport de PCR 2017)