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RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • : 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
  • 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
  • then - between October and January 19B7 - undertook the index ing and organisation of this material, together with basic analysis of démographie data she had previously collected. Ail data from the survey of standing buildings has been put on dise, ready for analysis in the coming year
  • 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
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • material; field E230, where there was also a large tile scatter, provided a parti cul arl y good example of this. Comparison of the distribution of surface material was made with the early n i neteenth-cent ur y p atterri of 1 and -use and settlement, as e v i d e n c e cl b y
  • actor which may explain the relatively large amount. of pottery found on the surface by comparison with that recovered by excavation. Quartz and conglomerate blocks °\ EBS 85-86 0 20 40 60m were -found embedded in the sur-face of the naturel schi ste; since several groups
  • 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
  • originally dug to obtai n clay for daub, and then backfilled with occupation débris. The pits were cut through by a ditch which contained modem glass (56). Rock fragments from the fill of one ditch (8) were of parti cul ar interest by comparison with those recovered from T15
  • , 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
RAP01768.pdf (le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • that are mapped, far less than in 1984, while a further 39% were up to 500m, and 25.6% more than 500m, away; it was largely sites in F that caused this anomaly. Comparison was systematical ly made with the early nineteenth-century pattern of land-use and settlement, as evidenced by the ancien
  • practice. Since the two trenches showed différent amounts of soil buildup and material in the two areas, changes in manuring practice rather than lapse in cultivation may be more relevant in explaining the data from Trench 1. The land-use around Trench 2 clearly changed when
  • by the 'total' collection sites of D221 and B347, even one field can produce distribution patterns that differ by period; the cl ustering of one class of material can suggest structures, the lack of cl ustering of another can suggest the effects of manuring. Comparison with cadastral land
RAP01557.pdf (PLOULEC'H (22). le Yaudet. rapport final de synthèse de fouille programmée 1996-1998)
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • that had provided a wide range of différent surface data so that excavation might produce results that would allow interprétation of the whole mass of surface mater i al. Three days (25 - 27 August) were spent in préparation for the main season by two people, in addition to two spécial
  • loam lay under the plough soil (2). It contai ned little stone by comparison with the plough soil (59kg, as against 188kg) and very little clearly introduced stone (including only 1kg o-f 03-4, 27. o-f stone excavated); there were large amounts o-f charcoal , usually flecks although
  • ZK67) Excavation o-f Trenches 28 and 29, started in 1986, was completed. Thèse two 6m squares were located over a dense tile scatter located by -fieldwalking at 50m intervais in 1982 and rewalked in 5m squares for 'total' collection in 19B6. The fieldwalking data suggested a Roman
  • . 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
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
RAP03536 ((56). Belle-Île en Mer : espaces et territorialité d'une île atlantique. Rapport de PCR 2017)
RAP02529.pdf ((35). activités minières et métallurgiques du massif de Paimpont. site de la ligne de la fenderie au gué. rapport de prospection thématique avec sondages)
RAP02918.pdf (HOËDIC (56). groah denn. rapport de fp 2013)
RAP03068.pdf (PLÉCHÂTEL (35). le bois : architecture et vie quotidienne au néolithique moyen. rapport de fouille)
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)
  • OF RADIOCARBON DATING ANALYSES Mr. Jean-Bernard Vivet Report Date: 12/2/2003 Material Received: 10/29/2003 Sample Data Measured Radiocarbon Age Beta - 1 8483 1 2470 +/- 60 BP SAMPLE : JBV1PMPLTBRO ANALYSIS : Radiometric-Standard delivery MATEPJAL/PRETREATMENT : (charred material): acid
  • =l) La bo ratory num ber: Beta-184832 Conventional radiocarbon âge: 2390±80 BP 2 Sigma calibrated results: (95% probability) Cal BC 780 to 360 (Cal BP 2730 to 2310) and Cal BC 280 to 240 (Cal BP 2230 to 2190) Intercept data Intercept of radiocarbon âge with calibration curve
  • . mult=l) Laboratory num ber: Beta-184831 Conventional radiocarbon âge: 2460±60 BP 2 Sigma calibrated resuit: (95% probability) Cal BC 790 to 400 (Cal BP 2740 to 2350) Intercept data Intercepts of radiocarbon âge with calibration curve: 1 Sigma calibrated resuit: Cal BC 740
  • 280 to 240 (Cal BP 2230 to 2190) Intercept data Intercept of radiocarbon âge with calibration curve: 1 Sigma calibrated resuit: (68% probability) Cal BC 400 (Cal BP 2350) Cal BC 520 to 390 (Cal BP 2460 to 2340) Re ferences : Da tabase used Calibration Database Editorial Comment
  • -mass-spectrometer (AMS) located at one of 9 collaborating research facilities, who return the raw data to us for vérification, isotopic fractionation correction, calculation calendar calibration, and reporting. The Radiocarbon Age and Calendar Calibration The "Conventional 14 C
  • measurements on corals is used. This data is still highly subjective. Calibrations are provided up to about 19,000 years BP using the most récent calibration data available (Radiocarbon, Vol 40, No. 3, 1998). The Pretoria Calibration Procédure (Radiocarbon, Vol 35, No. 1, 1993, pg 317
  • ) program has been chosen for thèse calendar calibrations. It uses splines through the tree-ring data as calibration curves, which éliminâtes a large part of the statistical scatter of the actual data' points. The spline calibration allows adjustment of the average curve by a quantified
  • closeness-of-fit parameter to the measured data points. A single spline is used for the précise corrélation data available back to 9900 BP for terrestrial samples and about 6900 BP for marine samples. Beyond that, splines are taken on the error limits of the corrélation curve to account
  • for the lack of précision in the data points. In describing our calibration curves, the solid bars represent one sigma statistics (68% probability) and the hollow bars represent two sigma statistics (95% probability). Marine carbonate samples that have been corrected for ô 13/12C, have also
  • results should be used only for illustrative purposes. In the case of carbonates, réservoir correction is theoretical and the local variations are real, highly variable and dépendant on provenience. Since imprécision in the corrélation data beyond 10,00 years is high, calibrations
  • 770 to 380 (Cal BP 2720 to 2330) The intercept between the average radiocarbon âge and the calibrated curve time scale. This value is illustrative and should not be used by itseif. ' C13/C12 ratio estimated Intercept data Intercept of radiocarbon âge with calibration curve: 1
  • will occur as shown by the two 1 sigma ranges which Database used occur from sections going outside of a similar "box" which would be drawn at the Intcal 98 Calibration Database 1 sigma limits. Editorial Comment Références for the calibration data Stuiver, M., van der Plicht, H., 1998
  • , Radiocarbon 40(3), pxii-xiii and the mathematics applied to the INTCAL98 Radiocarbon Age Calibration data. Thèse références, as well as Stuiver, M., et. al., 1998, Radiocarbon 40(3), pl041-1083 the Conventional Radiocarbon Age Mathem a tic s and the 13C/12C ratio used should A Simplified
RAP03849 (PLOUEZOC'H (29). La nécropole de Barnenez)
  • appliqué au cours des étapes 1-3 (Archaeology Data Service, n.d.; Schmidt et al., 2015) Présentation La figure 6 présente un diagramme (échelle 1:4000) de l’emplacement du site, mettant en évidence l’étendue de la surface étudiée. La planche I présente une échelle de gris des résultats
RAP03648 (LANNION (22). Route de Petit Camp : un ensemble funéraire et un habitat de l'âge du Bronze. Rapport de fouille)