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RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • . 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
  • 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
  • ... • • . J. I sites sites f N./< commune médiéval \ boundories sites post médiéval i undated sites 500m 0 sites TRANSECT M I A3 conditions, f eatures, présence of varieti£?s of schiste and local pronunci at i ons were noted on standardised recording forms. 285 fields were
  • 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
  • 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
  • . Further areas
  • ) to check the négative results from Ti 1 and T9. The sections of the trenches were cleaned by hand and recorded. In ail some 50 working days were spent on site? the average size of the team was seven. Trench 9 The plough soil was excavated in 10cm spits. The amount of pottery decreased
  • 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
  • . The absence of archaeol ogi cal subsoil features in H145 supports the view that the surface pottery scatter is the product of manuring » It is difficult to interpret the remains of the wall and hardstanding in T12. They were in ail probabil ity connected with the buildings recorded
  • because it shows that that part of Quoiqueneuc was occupied by the thirteenth century; hence, the buildings recorded in the ancien cadastre on the edge of H 145 did not represent a post-medi eval extension of an earlier settlement. , but an aspect of the médiéval settlement pattern i t
  • (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 the time the macadam road surface had been laid over it. The ditch may have acted as a drain or boundary for the holloway. T26 was eut to the north west of T23 to check that thèse features constituted a road: the same séquence of levels was recorded. Comment The résulte of thèse limited
  • ; field names (landes and f ri ches) over the whole area indicate that it had not been characteri st i cal 1 y cultivated before the 1820s. The field was first wal ked in 1984 and was classified as a 'possible site' (médiéval). In April 1986 it was intensively wal ked and this produced
  • 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
  • , T18, T19, T20, T21). The sections were cleaned by hand and recorded; the remains of the plough soil were removed, and the features thus revealed were excavated, by hand» Extensions were made in some trenches in order to clarify the character of some features, for example
  • between one rira found at HSO and one from A92 (see fig» 6, HBO-5 and A92-2) would perhaps argue for a date that spans the first centuries BC and AD» The 'Roman' character of the assemblage might also be suggested by the substantiel tiles for, although not very wel 1 fired
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)
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
  • , 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
  • . 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
  • 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
  • and A79 were first walked at 50m intervais in 1982; the material which was recovered concentrated where the two fields joined and was classified as a 'probable médiéval site'; Roman pottery was also noted. The field boundaries were subséquent 1 y changed and the eastern part of A31 has
  • ) . At a later stage two further trenches were eut mechanically 30m either side of T39 (T40 to the south, T41 to the north). The sides of the trenches were cleaned by hand and recorded; the lowest part of the plough soil and features were excavated by hand. In one case T39 was extended (T46
  • intercutting pits. Pit 32 (0.62m in diameter, 0.15m deep) had been the first to be eut and bac kfi lied (31); it contained 1 sherd of late Iron-Age/earl y Roman pottery. Two pits were then dug partly into 32 and 31 and partly into the natural. Both were about 0.5m in diameter and 0.1m deep
  • to have been a Spanish amphora; the upper fill (58) produced no finds. The eastern edge of the ditch had been eut into by a group of four pits. Pit 77 was dug first, and then three more -71, 73 and 75: none of the fills produced finds (76, 70, 72, 74). A mètre down slope
  • Asti II and Davies 1985, 90-5; and below, D153) . With the exception of the features at the bottom of the slope which are associated with modem attempts at drainage, the pottery suggests that ail the pits and ditches ware filled in or after the first and second centuries AD
  • , it looks as if the field was used for agriculture at a time when firstand second-centur y pottery was being discarded; in this case the ditches are likely to have been field or enclosure ditches of the first and/or second century. It is clear from the worn condition of the pot
  • . To a certain ex tent the results from A31/79 are similar to those from A92, one and a half km away, despite the considérable différence in data derived from the surface. Both sites are located on ridges and both suggest nearby structures occupiéd during the first and second centuries AD
  • 0.3kg per square) of brick and tile. The field is lowlyinq and located 100m east of the Château de la Ruée, to the? east of Ruffiac (fi g. 6). The a n c ien çadas t. r e records this field as permanent meadow in the early nineteenth century but it also shows that it forméd part
RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
  • d’une plage fossile avec une nette troncature sédimentaire, à environ trois mètres au-dessus des plus hautes mers et il est coiffé d’un couvert dunaire qui en a assuré le scellement et la protection. Le site a été découvert par G. Bernier en 1970, puis fouillé sur 23 m² par Olivier
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • 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
  • and time off; 270 of thèse were working days. The weather was poor, with very considérable rai nf al 1 ; although the fields themselves were usually in good condition for walking, recording was excepti onal 1 y difficult. Fieldwalking in Runs at 50m intervais (Transect Walking
  • within thèse transects were walked at 50m intervais, using collection units of 100m; some were too sodden for effective and damage-free surface collection. Field conditions, features, présence of varieties of schi ste and local pronunci at i ons were noted on standardi sed recording
  • . 0. 767. 1 . 37. Table 1: Roman Medi eval Post -med . Wei ght Fl int Haemati te by no. kg Pot Pot Pot g 2. 72 1 3. 67 34 . 67. 61 . 17. 2. 97. 545 18 26. 01 347. 61. 57. 3 . 87. 64 4 86. 87. 3. 13 3.77. 8.27. proportions and quantities of material recorded As in the core
  • 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
  • by smelting iron ore in shaf t f urnaces; that from R9, however, weighed 2kg and came from the bottoms of bowl furnaces; first- and second-century pottery was collected from the surface in this 6 area. This season 's work has produced several indications that the core communes
  • and subsoil features, as in 1985 and 1986, in order to be in a position to interpret the now large corpus of fieldwalking data. Analysis of the standing building records will be undertaken in 1987-8, and work on pottery fabrics and soils will continue. •*•*■*•***■ ■*■*•**♦■** The season
  • Foster, Liz Musgrave and Kate Sergeant for their invaluable supervision in the field - with especial appréciation of kate and Liz, who have taken part in ail fieldwalking seasons since 1982; and, as ever , to our team, who coped heroically with sodden recording forms
  • and with the additional strains of scattered accommodation: despite very difficult working conditions, they achieved an astonishing rate of work and easily broke ail records. We owe profound thanks, as always, to ail who have given time, labour and energy to the project, as wel 1 as to those who have
RAP02521.pdf (MOLÈNE (29). beg ar loued : un habitat en pierres sèches campaniformes, âge du bronze ancien. rapport final de fouille programmée 2007-2009)
RAP02402.pdf (MOLÈNE (29). beg ar loued : un habitat en pierres sèches campaniforme. rapport intermédiaire 2008 de fp 2007-2009)
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
  • archéologique est de teinte brune, constitué de limons organiques et de sables, d’une épaisseur comprise entre 30 et 40 cm, directement posé sur le rocher ou la plage fossile démembrée. La fouille a concerné une zone d’un seul tenant de 16 m² à l’ouest, jointive à celle de 2015 et à l’est
  • d’armatures. Depuis le XIXe siècle, ces objets ont été discutés par les archéologues, d’une part comme fossile-directeur du Téviecien, mais aussi par leur fonctionnalité (De Baye, 1872). En effet, à partir des découvertes dans contextes humides de l’Europe du Nord, les bitroncatures
  • mésolithique se matérialise par un niveau de terre noire épais de 0,50 à 0,60 m, rempli de coquilles marines et autres vestiges fauniques, de silex taillés et de morceaux de granite brûlés. Il repose au-dessus d’une plage fossile avec une nette troncature sédimentaire, à environ trois
  • parking. Il s’agit d’un niveau de teinte brune, constitué de limons organiques et de sables, d’une épaisseur comprise entre 30 et 40 cm, directement posé sur le rocher ou la plage fossile démembrée. Ce sont donc à peu près 320 mètres cube qui ont été déplacés pour accéder au niveau
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)
  • , aujourd’hui masqué par les dunes. L’habitat mésolithique se matérialise par un niveau de terre noire épais de 0,50 à 0,60 m, rempli de coquilles marines et autres vestiges fauniques, de silex taillés et de morceaux de granite brûlés. Il repose au-dessus d’une plage fossile avec une nette
RAP00239.pdf ((35). le bassin de Rennes. rapport de prospection inventaire)
  • pour le point mensuel sur la sécheresse. En août tous les records d'assèchement des cours d'eau et des nappes phréatiques ont été battus. La France entière enregistre des débits d'eau sous la normale. 11 000 kilomètres de rivières sont à sect Tirer les leçons Brice Lalonde est
  • 70 mm 6) 25450 mm Si 15425 mm Le cumul des pluies en juillet et août, cette année et l'an dernier, comparé au record local et à la normale: le sort différent des régions. la normale. C'est le cas du Val de Loire, du nord de la Vendée, d'une grande partie du Calvados, ainsi que du
  • Bessin et d'une partie du Cotentin, où il n'est pas même tombé 25 mm d'eau en deux mois. Une constante, à de rares exceptions près, les cumuls de juillet et août sont inférieurs à ceux de 1989 (voir le tableau). Ils constituent môme des records selon les chiffres relevés par la
  • fossés rectilignes et orthogonaux (portion). : Deux enclos contigus à fossés rectilignes et orthogonaux. 34 ■ le Rocher : Enclos à fossés rectilignes et orthogonaux. 35 ■ le Petit-Rollier : Structures parallèles, parcellaire fossile (?). 36 CHATTLLON/SEICHE - Coquelande
  • Hattais : Enclos à fossés rectilignes (ou parcellaire fossile ?). 98 - le Château : Motte castrale et 2 structures circulaires associées. paracurvilignes accosté 99 PLEUMELEUC - la Motte I : Villa gallo-romaine et son enclos périphérique quadrangulaire - Inf.compl. 100
  • . 110 - Copreuil : Enclos à fossés paracurvilignes ou parcellaire fossile. 111 - la Charormière I : Enclos à fossés paracurvilignes cloisonné. 112 - la Charormière II : Vaste enceinte circulaire à double fossé à interruptions multiples, Néolithique. 113 - la Gibretais
  • PLAN ARCHÉOLOGIQUE STATISTIQUES ET ANALYSES Répartition des grands types d'indices N % 12 9,2 88 67,1 7 5,4 15 11,4 Autres enceintes 2 1,5 Parcellaires fossiles 7 5,4 Sites à fondations en dur Enclos à fossés rectilignes 52 Enclos à fossés curvilignes ou
RAP03364.pdf (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport de FP 2014-2016)
  • knowledge of these groups is however unequaled: if the Late Azilian and the Pleistocene/Holocene transition communities are now well known after some recent works, this is not the case of the Magdalenian and first Azilian societies. The launching of a research program in 2013 in a small
  • rock shelter discovered by M. Le Goffic at the Rocher de l’Impératrice at Plougastel-Daoulas, aims to progressively fill in this gap. The first results of this archaeological operation actually suggest this shelter dominating the Elorn estuary and the Brest roadstead to have been
  • occupied during the Early Azilian. The obtaining of radiocarbon dates (the first ones for the Lateglacial of Brittany) places the Azilian occupations between 13000 and 12000 cal. BC, that is to say during the GIS-1e (Bølling). Several evidences suggest this site to be the result
  • , development of a weaponry essentially constituted of axial points). More than 50 engraved schist tablets were also discovered at the Rocher de l’Impératrice. This discovery is particularly interesting since it constitutes the first evidence of Paleolithic art in Brittany. These engraving
RAP04033 (RENNES (35). 18 allée Coysevox. Rapport de fouille)
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
RAP03920 (VANNES (56). 5, 7, 9 rue du Colonel Pobéguin. Rapport de diagnostic)
  • matelassure quartier sanglon Fig. 31 Schéma de répartition des différents morceaux de cuir constituant une selle © S. Jean, Inrap Fig. 32 Dessin d’une selle ancienne montrant des zones cousues et d’autres cloutées (Diderot 1769, planche de Goussier, Harguiniez et Soufflot) tapis en
  • jusqu’alors méconnus. II. Résultats 3.1 Etudes du mobilier (F. Labaune-Jean) 43 Fig. 33 Système d’harnachement d’un cheval attelé (Megnin 1904) Fig. 34 Planche montrant différents types de sangles pour l’harnachement (Diderot 1769, planche de Goussier, Harguiniez et Soufflot) Fig
  • . 35 Planche montrant différents types de sangles pour l’harnachement (Diderot 1769, planche de Goussier, Harguiniez et Soufflot) 44 Inrap · Rapport de diagnostic Fig. 36 Détail d’une planche avec un cheval monté où apparait un tapis de selle bordé (Diderot 1769, planche de