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RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • of the relationship between land-use and settlement during the 1 ast two thousand years, took place from 25 August - 1 October in the communes of Ruffiac, Tréal , St-Ni col as-du-Tertre and Carentoir, in the department of Morbihan in eastern Brittany. The ai m of the study is to détermine when
  • some pièces were 5mm across. This layer varied in thickness -from 0.75m on the eastern, up-slope, side o-f the trench to 0.38m on the west. At the east end the top sur-face o-f 2 curved as i -f the layer had been mounded up. This layer could not be total ly excavated over the whole
  • ) . 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
  • that the black siltstone (03-4) was ploughed in to break down the clay, since it was présent in such unusual quanti, ti es, but this explanation cannot account for it al I since some fragments had nailholes. Notably, although there was mixed building stone on the surface of T37, 03-4
  • 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
  • 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
  • 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
  • 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
  • ? in this period of the building 's history. Further levelling (30, 35) later seems to have? taken place within the extension, the last contemporar y with the blocking of the doorway (49). This seems to have been done while the building was still in occupation for there is nothing in thèse
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • years, took place from 20 March - 4 April in the communes surrounding Ruffiac, Treal , St-Ni col as-du-Tertre and Carentoir, in the departments of Morbihan and 1 1 1 e-et-Vi 1 ai ne in eastern Brittany. The aim of the study is to détermine when, how and why the exploitation
  • . However, P, an area topographi cal 1 y characterized by the drop of land down to the River Oust, was not dissimilar to the eastern section of M, where the land dropped down to the River Vilaine; here, for a comparable distance, 6.77. of fields walked had notable concentrations
  • of Bruc — for a distance of some 2.5km; thèse 'blank' fields begin already in the eastern part of Sixt commune though do not reach as far as the présent boundary of Pipriac on the east. Everything, including the shape of the fields, suggests that this is an area of late exploitation
  • material and not pink. Pink schi stes are found, however, in some discrète areas: close to south-eastern Carentoir, in western parts of the Bruc 'blank', in odd fields near Pipriac, around Patis de la Porte, Château La Frèche, La Glonnais, Malon and in small quantities around Les
  • examination o-F it. Preliminary examination of the pottery suggests that there are some distinctions between the fabrics collected between Pipriac and the Vilaine (Transect M, eastern portion) and those characteri sti c both of the core and of sample transects near it (N, P, R
  • and the western section of M). Some of the Roman fabrics in eastern ti had not been noted before, and included a late Roman roi 1 er-st amped sherd of Argonne ware from M447, near 'Château Gaillard', 2.5km east of Pipriac bourg ■ This ware has an essentially coastal distribution, although
  • there are finds from the Rance/ Vi 1 ai ne river Systems and one sherd from Pipriac is already known (Galliou 1977: 91-2). The médiéval fabrics from this eastern région seem to have less mica, fewer spi cul es and more grog. Some of the fields with Roman material are of particular interest
  • provided financial support. G. G. Astill Department of Archaeology University of Reading Whi tekni ghts Reading RG6 2AA Wendy Davies Department of History University Collège London Gower Street London WC1E 6BT 9 July 1987 REFERENCES Astill, G. and Davies, W. 1982 'Un nouveau programme
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • Chapelle Gaceline, Caro, Reminiac, Augan and Campélieac in the Morbihan in eastern E
  • presurnabl y some kind of hardstanding or floor (9) « The northern extent of the standing was established by augering and was found to peter out some three mètres north of the wall. The eastern extent. of the wall was similarly established and found to end 1 » 2m from T12, with no sign
  • sel f . K446 (Ruffiac ZA106) Ruf f i ac K446 is si tuât ed on the eastern outskirts of Becul eu 1 n
  • 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
RAP03967 (QUIBERON (56). Beg-er-Vil à Quiberon. Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de fouille programmée 2020 )
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • place between 21 March and 13 April in the communes of Ruffiac, Tréal , St-Nicol as-du-Tertre and Carentoir in the Morbihan in eastern Brittany. The aim of the study is to détermine when, how and why the exploitation of the environment changed direction within the historic period
  • of brick and tile (50.82g). The assemblage included second-century Roman wares, fifteen fragments of tegul a and one of imbrex. Médiéval and post-medieval pottery were gênerai 1 y distributed over the field but both Roman pottery and brick and tile cl ustered in the north-eastern third
  • 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
  • Department of Archaeol ogy University of Reading Wendy Davies Department of History University Collège London Whi tekni ghts Reading RG6 2AA Gower Street London WC1E 6BT 30 July 1985 REFERENCES André", P. 1974 'Le site médiéval de Kerl ano-en-Pl umel ec (Morbihan)', Archéologie en
RAP03096.pdf (LAIGNELET (35). Rapport de sondage)
  • Fondation Américaine « History Flight » en Février 2012. 2  Recherche : Le recherche s’est effectuée par la Fondation Américaine « History Flight », fondation agréée par le gouvernement des Etats-Unis dans la recherche des disparus de guerres. Professeur PANTEL 3  Plan de
RAP00321.pdf (LA CHAPELLE DES FOUGERETZ (35). le Bas Plessis. rapport de sauvetage urgent.)
  • , A corpus of Roman engraved gemstones from British site;: Oxford,1974,2 vols.(B.A.R,8). -Higgins,1961= R.A Higgins, Greek and Roman jewelIry, London,1961. -Iliffe,1934= J.H Iliffe, Rock-cut tomb at Tarshiha.Late IVth century, The Quarterly of the department of antiquities of Palestine
RAP01961.pdf (bassin occidental de la Vilaine et centre Bretagne. rapport de prospection inventaire)
  • Photography in Italy (1899-2004) 15,30-16,00 M. Gojda Ancient Landscapes hidden and visible. Air Survey and Rethinking the History of Space and Seulement in Central Europe: towards a SynIhesis 16,00-16,30 Coffeebreak - Pause café To overcome infirmity: current approaches to aerial
  • & H. Becker M. Schônherr Aerial Archaeology and new discoveries by a flying wing model 11,30-12,00 Coffeebreak - Pause café 3 o CQ —i Q) 3 3 CD 12,00-12,30 M. De Meyer 12,30-13,00 M. Lodewijckx, K. Verfaillie, I. Ro- Aerial survey in Eastern Flanders: a starl
  • Photography and Trenchmaps 15,30-16,00 F. Vermeulen, M. Antrop, T. Wiedemann & B. Hageman F. Vermeulen, G. Verhoeven & J. Semey M. Willbertz 16,00-16,30 Coffeebreak - Pause café 16,30-17,00 Early médiéval fortifiée) sites in north-eastern Poland: a proposai for an archaeological
RAP01008.pdf (MELRAND (56). Talrest. rapport de fouille préventive)
  • a : participé au déga^ aient : J» Looorne~,oe3 'té trois journées de travail «Ont nt ae la otion, jadré,correspondant de la Direction des Antiquités Histori —, Ph* Le Breton,professenr à Auray,Ces Le Verger. A l'issue des travaux le remblsieiaont a été effectué par les
RAP03814 (VANNES (56). Rue Saint Tropez. Rapport de fouille)
RAP03819 (SAINT-GLEN (22). La Touche ès Pritiaux : le site du premier âge du Fer. Rapport de FP 2019)
RAP03364.pdf (PLOUGASTEL-DAOULAS (29). Le Rocher de l'Impératrice. Rapport de FP 2014-2016)
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)
  • . precipitated ground water samples) . . 1 •• J "none" No laboratory pretreatments were applied. Spécial requests and pre-laboratory pretreatment usually accounts for this. bfcw t «»7M>, "àcid/alkali/acid/cellulose extraction" .«>iefc M&VJ-ÏH »iof»i s -a&ivuit* 8?* m-û\ * ■■ . ■• 'i
  • 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
  • corrections. Réservoir corrections for fresh water carbonates are usually unknown and are generally not accounted for in those calibrations. In the absence of measured ô 13/12C ratios, a typical value of -5 %> is assumed for freshwater carbonates. (Caveat: the corrélation curve for organic
RAP02005.pdf ((29). le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP03817 (QUIBERON (56). Beg er Vil : un habitat de chasseurs-cueilleurs maritimes de l'Holocène. Rapport de FP 2019)