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RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • . 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
  • was used as a dump , such that a ridge or mound was -formed (context 2); the trench opened (T36) was too small to establish the character o-f this dump, but it indicates the continued existence of a nearby settlement. The sise of the dump, and the character and relatively small amount
  • 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
  • , i.e. with hand too] s and a 5/1 sample kept for sieving to check recovery rates. In ail 173 working days were spent here, with an average team of 6. Trenches 32 and 38 Although the area opened was very small it revealed a séries o-f structural and floor levels, associated
  • : 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
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
  • 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
  • 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
RAP00631.pdf (BRENNILIS (29). Karaes Vihan. rapport de fouille programmée)
  • >A
  • NOUA n'avons aucun élément qui nous permette d'établit avec cer titude le nom d'origine du village. Une recherche e{{ectuée danó la commun de Btennilis à Plouenez (un village proche du ¿ite) a prouvé que le nom cou rant du ¿ite en breton est KARTÌAES-VÌHAN, en {¡ranq.aU "le
  • petit Carhaix" in.b.fiémininen breton) ; par raison de clarté, ce nom courant, mais nonhistorique, a été choisi. LES BATIMENTS APRES LES RESULTATS VE LA FOUILLE : Lei, {outlles e^ectuées ¿ut le ¿ite depuis 1978 ont montré que la maison typique est la maison mixte ou la maison
  • évidence les différentes étapes de modifications des talus et V existence d'un bâtiment [n° 111-A) constAuit en bols et mottes de gazon. ORGANISATION, TECHNIQUE VE LA FOUILLE : Depuis 1978, la méthode open area de {¡ouille [BARKER, 1 977) a été utilisée SUA ce chantleA. En 1984, comme
  • Ite muhA avaicnt fìait l'obj'et de. quelqueA modifiicationò. Suite a un efifiondnment, le pahement nohd a l'eAt de la ponte d' (M2) a ete n.enfion.cé ¿UA. ¿afiace.exténie A l'OueAt de la ponte d'entnée no Ad leA baMj>t>eunj> ont néutiliAé en pantie leA muAA nuinéi> de
  • batiment et ¿eA dififiéhe étapeA de. modi Ricatto nò ¿uggene au moinó deux phaòeA de conAthuction. En ph.e mieu lieu, nouA avonA constate que le. batiment VI et ¿on jàhdin ont ite inò- tallé-i entne deux taluA en te/me. phé.-exiòtant onienté apph.oximativeme.nt n eAt. La ph.eAe.nce
  • , de conAtnuctionA anté.hieuh.ej> aux bàtimentò viò de ¿uAfiace eAt dijà atteAtée ¿uh. le: ¿ite de KanhaeA Vihan. Lafiouillemetko dique nouò a penmiò d'identifiieA V emplacement de. deux muAA légehA, ^¿¿iti¿te ¿ouA l'eboutCò deA muhA ¿ud du batiment VI. Le pian de. lafiouille(fiig
  • . 4) nouA montne que ceA muhA legeAA ont pu appahtenih. a deux bàtimentA de. petiteA dimenAionA, dont leA axeA pnincipaux etaient onientu nohd-rud. Vejux pkaòeA de. conòthuction ¿ont ¿uggen.ée¿ pouh cette pahtie du ¿ite,. i PHASE I - Deux bàtimentò de petiteA dime.nAÌonA avec une
  • , les meules po¿ent un problème car on trouve le même type de meule ¿ur les ¿ite¿ d'habitats ruraux du Moyen-Age en Europe occidentale. Les fouilles de 1984 ¿ur le bâtiment t/T ont localisé d'autres fragments de meules à grain utilí¿é¿ en remploi dans les murs du bâtiment ({ig. 6
RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
RAP02357.pdf (SAINT-MARCEL (56). "la Sente Verte". le bourg. rapport final d'opération de fouille préventive)
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
  • 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
  • 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
  • black and grey.) This needs more observation and more testing but at présent it suggests that the présence of pink-purple imported roofing schi ste is an indicator of areas of 1 ate médiéval and early modem arable while its absence is an indicator of land more recently taken
  • 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
  • ; without their help much of this year's season would have been impossible and we are therefore immensely grateful to them. Fieldwalking and excavation were financed by the British Academy, the Society of Antiquaries of London, the University of Reading, the University of London Central
  • , Sussex Bell, M. 1983 'Valley sédiments as évidence of prehistoric land-use on the South Downs', Proceedings of the Prehistoric Society, xlix, 119-150. 1+ EAST BRITTANY SURVEY 1985 £J3 fields walked m 1965 ■— — commune boundaries A • ■ sites A c* U probable • médiéval si tes
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)
RAP01961.pdf (bassin occidental de la Vilaine et centre Bretagne. rapport de prospection inventaire)
  • des bâtiments agricoles... » Fig. 14 - Illifaut (22). La Ville Aumont. Bel ensemble d'enclos menacé par la possible extension des carrières de sable pliocène ! 15 1. IWednesday 08,00-09,30 Regislration/lnscription 09,30-10,30 ...■
RAP01710.pdf ((56). la ria d'Étel. rapport de prospection inventaire)
  • ). (Annexe 2) □ WHEELER M., RICHARDSON K.M., 1957 - Hill-Forts of Nothern France, Reports of Research Committee of the Society of Antiquaries of London, XIX, p. 35, 37, 94, 96, 100, 101. (Annexe 3) □ COPPENS Y. - "Inventaire des stations à augets du Morbihan", AB 61, 2, 1954, p. 295
RAP03801 (Corpus des signes gravés néolithiques, Art rupestre néolithique en Armorique. Rapport PCR.)
  • ................................................................................................................................................................613 Annexe 8. Parthenos...........................................................................................................................617 Annexe 9. Invitation à l’Institute for Culture and Society, Prehistoric Archaeology, Aarhus University, Højbjerg (Danemark
  • . Gendron) ; Dépôt archéologique des Côtes-d’Armor, Quessoy (J.Y. Tinevez). 25 Corpus des signes gravés – 2019 Au cours de ces quatre dernières années, Andrea Arca (Université de Pise, Footsteps of Man Archaeological Society, Valcamonica), Thomas Huet (SIG et analyses spatiales de
RAP01557.pdf (PLOULEC'H (22). le Yaudet. rapport final de synthèse de fouille programmée 1996-1998)
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • 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
  • 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
RAP03654 (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport intermédiaire 2018 de FP 2017-2019)
RAP03536 ((56). Belle-Île en Mer : espaces et territorialité d'une île atlantique. Rapport de PCR 2017)
  • renseignant le territoire bellilois. Celles-ci sont distribuées soit sous licence Open Source, soit via la licence Enseignement Recherche de l’IGN. Toutes les sources cartographiques ont été mises en forme pour faciliter leur usage par les membres du PCR, depuis une plateforme de logiciels