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RAP02918.pdf (HOËDIC (56). groah denn. rapport de fp 2013)
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • , 1984b). The latter analysis has been completed and, as demonstrated below, is of particular significance for fieldwork. The 1985 season involved fieldwalking over large areas at wide intervais, as in 1982 - 84; fieldwalking four selected areas in 5m squares for 'total' surface
  • to qualify a concentration for comment has been de! iberately fixed at a low level in order to secure a wide range of possibil ities for testing; in fact, in many cases numbers were far higher than the necessary minimum. It should be stressed, yet again, that the terms are conventions
  • 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
  • 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
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
  • ) . Comment The occurrence of médiéval and post-medi eval pottery in the plough soil, but not beneath , and the lack of conte;-; ts of thèse période would suggest that this matériel was not deriyed from SLib— surface features. Manuring might wel 1 account for the evenly distributed
  • Roux) documented from eighteenth and fifteenth centuries respect! vel y , with a possible médiéval structure near T36 (see fig. 2). It is potentially of the highest significance for long—terni settlement history and would merit a much more extensive investigation. A92 (Ruffiac
  • that this ditch was filled (and perhaps eut) at a later date than ditches 5 and 10. Indeed it may have been filled during the 9 destruction o-f the buildings. Comment The fabric and forms of the pottery, similar to the material from HSO (excavated in 1986: Asti 11 and Davies 1987, 120-1
  • posthole produced no finds (38: fill 37), and a shallow 'U'-shaped ditch (40: 0.85m wide, 0.42m deep) had a fill with 3 sherds of Roman coarse ware (39: Fabric 89). Comment It is difficult to interpret the résulte of thèse limited excavations. The laçk of features associated
  • 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
RAP03738 (ILE MOLENE (29). Le Bourg. Rapport de diagnostic)
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • - 13 1, 2 14 H 145 15 K446 18 Fig. 3 19 H80 Fig» 22 4 23 A92 ' 28 9 Fig. 5 Fig. 6 □ t h e r Work, 32 1985- 6 33 General Comment and Acknowl edgements 34 Re-f erences 35 P 1 a t. e s 1 - 1 0 f ollowing 35 The fifth and sixth seasons in a programme
  • nineteenth century» This latter analysis has been completed and is of parti cul. ar significance for fieldwork because it allows complète reconstruction of the early ni neteenth-century landscape (Astill and Davies 1982a, 1983, 1984, 1985). THE EASTER SEASON The 19S6 Easter season
  • concentrations of material not covered by the above catégories for example, one unit with five or more sherds of the same period •- have been termed 'possible sites'. (The minimum number of finds necessary to quai if y a concentration for comment has been del i beratel y fixed at a 1 ow level
  • , 11?/» quartzite and 6% qres) . The area appears ta have been devoted to rubbish disposai during the médiéval period; it is possible that the pit, or perhaps tree hole, was filled with mater i al from a building. Comment The results of thèse excavations are extremely usef ul
  • 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
  • Comments 2 IA, 2 tile 1 flint flake ., 10 7 IA,1 tile, 8 daub 3 fi11s modem qlass 2 f i 1 ls ? terminal reçut of . 16 i 1 Is T21/41 1.13 T21/42 1.75 T21/47 "21/49 1.0 Comment The lack of certain médiéval features would encourage us to regard scatters of the same character
RAP03449 ((56). Autour du Golfe du Morbihan, les landes de Lanvaux et le sud de la vallée de la Vilaine. Rapport de PD 2016)
  • land/property divisions which are still indicated on the project mapping. 3.1.4 Numerous week trends are evident throughout this survey location, some of which are rectilinear in form. These are at the limits of instrument detection and their potential archaeological significance
  • are evident in the results from M3. Responses of possible interest are indicated, mainly in the central and western region of survey (12 & 13). The archaeological significance of these anomalies is uncertain. Insufficient survey area available in M3 and an abundance of modern ferrous
  • of anomaly 17 and W of 23 likely derive from natural soil/geological variation. Further potentially significant responses include a linear arrangement of anomalies (20) running almost parallel with the upstanding Iron Age ramparts enclosing the site; several weak linear © Target Client
  • to the building in M1 has also been recorded, and this may extend over an area c.80m x 48m in size. Further potentially significant responses at Coet Sürho include a possible dwelling (15) to the NE in M4, and a group of linear responses and weak trends (16) also in M4 to the S/SW. Survey
  • remains somewhat speculative. Excluding the building foundation (17) highlighted to the north most of the anomalies in the Pen Castel results are poorly defined and masked by soil/geological variations. Groups of anomalies highlighted as potentially significant include potential
  • building footprints 18, 19 and 23 to the N/NE and E, and a linear arrangement of responses to the S/SW. The potential that a large ferrous response NE of survey centre in the Pen Castel results has masked areas of significant archaeological response should not be dismissed. RÉFÉRENCES
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
  • : 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
  • the local topography. In ail transects most concentrations lay between 25 and 75m (in P 747., in M 77.57. and in R 93.67.). 4 (In R none lay below 25m.) Most lay within 250m of a mapped stream (44.47. in P, 63.17. in M and 717. in R) though a significant proportion in P lay over 250m
  • significant. In Transect P there are none of thèse materials on the high ground west of Ruffiac boundary, precisely in those areas which produced no surface pottery either; there are also no pink schi stes in and around Malestroit and close to the River Oust. In Transect M there are none
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
RAP02521.pdf (MOLÈNE (29). beg ar loued : un habitat en pierres sèches campaniformes, âge du bronze ancien. rapport final de fouille programmée 2007-2009)
RAP03548 (DINEAULT, PLOMODIERN, ROSNOEN (29). Prospection diachronique Basse vallée de l'Aulne. Rapport de PD 2017)
  • locale. En définitive, ce travail traite des rapports entretenus entre les sociétés du passé et leur espace. L’objectif est de comprendre comment les communautés anciennes se sont adaptées à leur environnement, comment elles ont aménagé leur territoire et comment elles ont géré leurs
RAP02648.pdf (LILLEMER (35). les Hauts. rapport de fouille)
RAP03364.pdf (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport de FP 2014-2016)
RAP03316.pdf (PLOUHINEC (29). Ménez-Dregan 1 : des Prénéandertaliens aux Néandertaliens à l'extrême ouest de l'Europe. Rapport de FP)
  • anciens d'Europe (465 ka par datation RPE / ESR). Ce site permet de mieux comprendre comment et dans quels environnements ont évolué les premiers peuplements humains de ce Finistère, qui constitue l'un des « culs de sacs » occidentaux de l’Eurasie (fig. 1). Problématique de la
  • endroits aujourd’hui complètement érodés. L’emplacement de nombreux blocs effondrés et des structures de combustion donne indirectement la morphologie et les dimensions de la grotte lors de chaque phase d’occupation, et montre comment l’espace habitable s’est peu à peu réduit au fur et
RAP01969.pdf (BERRIEN (29). " le Goënidou". l'impact d'un habitat médiéval sur le paysage et l'environnement. rapport de sondages dans le cadre de la prospection thématique)
  • est normale pour chaque modalité. Une analyse normale de variance (Anova) a été réalisée. La comparaison de ces classes 2 à 2 a été obtenue grâce au test LSD (Least Significant Différence) celui-ci étant le plus résolutif dans le cadre de cette analyse. • La distribution n'est