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RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • , at least during the médiéval period (Astill and Davies 1984a: 20). A116 lies to the north of Ruffiac, between Coetion and Le Vivier. It is located in a small damp valley bottom, on a north-facing si ope, at 70m. At least one platform can be seen. To the north of the field, in the lowest
  • part of the valley, is an area of permanent pasture in which there is a prominent bank and a possible platform (see fig. 2). The bank runs diagonally across the valley bottom. 130m to the west of this bank, at the bottom of the south-facing slope of the valley, is a pronounced
  • conditions prevailed on another three. Excavation therefore had to be more limited than was intended. The excavation strategy was similar to that used by Martin Bell to sample lynchets and valley bottoms in the south of England (Bell 1977; 1983). A 2m-wide trench, 14m long, was eut across
  • of the 18 mètre squares) was dug. Soil samples for micromorphol ogical and pollen analysis were taken in columns from the sections, using purpose-made meta! containers. Small test holes were also eut by machine at every 15m to the north of Trench 1 (up the side of the south-facing valley
  • the archaeol ogical potential of small -scale work on field boundaries in this area. The ditch in Trench 1 is likely to be an earlier field boundary, perhaps marking the division between cultivable 1 and and the wet areas of the valley bottom. In Trench 2 the bank may have marked
  • the boundary between plough land and meadow and could also have acted as a kind of flood barrier; the shallowness of the loam deposit would argue for a shorter period of ploughing in the lower northern slope of the valley (the area immediately behind this bank). The absence of brick
  • , 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
RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • valley. Near the top of the slope and near the valley bottom are two breaks of slope which follow the contours and could therefore be lynchets or river terraces (fig. tf.) . The ancien cadastre shows this area to have been arable in the early nineteenth century. The two fields A31
  • been joined to A79. This new field, A31/79, therefore includes the area where the material had concentrated, as also part of the ridge and the whole valley side. In 1987 it was griddE*d in 5m squares for 'total collection. Relatively large quanti ti es of Roman pottery (1—3 sherds
  • ) were recovered from a few squares distributed throughout the field (21 out of 1383 squares). Brick and tile concentrated in the central area of the field, straddling the earthwork on the valley slope (fig. 5); thèse squares produced a maximum of 9 pièces each (0.5kg). The médiéval
  • to have been dug parai lel to one another, but they were not. equi distant (13.8m between 51 and 53; 11.7m between 53 and 55). Trench 39 T39 was lB3m long; it stretched from the ridge to the bottom of the valley slope and sectioned the two earthworks. The depth of the plough soil
  • at the bottom of the valley slope. The part of T39 which was on the ridge produced one shallow feature only, perhaps the base of a pit (65: 0.6m wide, 0.1m deep), whose fill (9) produced no finds. Between the brow of the ridge and upper part of the slope (between 30 and 60m from the south
RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • of Augan commune centre, Here there was a marked change in topography - as the and in modem land management — as we moved also in the bedroc north 5 it was with steeper rnuch higher hi 1 1 s and some north/south valleys; but farms (and often fiel ds and houses) were biqger
  • of this deposit in T5 and T6 made it clear that the platform earthwork was a lynchet, similar in character to the? lynchet sectioned in 1985 on the other si de of the valley. Around the crest of the lynchet a slight change in the colour and texture of the 1 owest colluvium (T5, context 4) may
  • was found on the surfaice (see Table 3),, Identification of the lynchet by T4, T5 and T6 confirma the 1985 resuit s suggested by T2? the lower si opes of the valley had been in arable use in the médiéval period but had been turned over to meadow by the nineteenth century, perhaps
  • 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
  • working days were spent on site and the average size of the team was six. Trench 25 This was the most westerly trench and was 39m long. The depth of plough soil varied from 36cm at the south, uphill, end to 1.10m lower down the valley side. The plough soil (1, 36) overlay the natural
  • was a ragged v-shaped ditch, 1.3m wide and 40cm deep (46), which followed the slope down the valley side -for at 1 east 90m; subsidiary machine eut s (T26, T27) located the ditch on the saine alignment and f ai 1 ed to produce évidence of a tujrn. Both ditches contai ned small quanti ti es
RAP01961.pdf (bassin occidental de la Vilaine et centre Bretagne. rapport de prospection inventaire)
  • Systems in Flanders. The intégration of aerial photography and GIS in the Potenza Valley Survey (Italy) ADABweb - Base de données archéologiques sur l'inlranet du pays fédéral allemand Niedersachsen (Basse-Saxe) Vlapping the Médiéval agricultural traces with help of GIS and aerial
  • . SanchezPalencia & A. Orejas T. Driver High peaks, deep valleys: Triumphs and challenges in surveying upland Wales from the air 10,30-11,00 N. Andrikopoulou-Strack Protecting the archaeological héritage by using aerial photographs - Chances and limits of an archaeological method 11,00
  • Meyer Archaeological Research using Satellite Remote Sensing Techniques (Corona) in the Valleys of Shirwan and Chardawal, Iran M. Doneus & G. Scharrer Archaeological Feedback of the Aerial Archaeological Interprétation of an Early Médiéval Graveyard in Frohsdorf, Lower Austria. W
RAP02259.pdf (CHÂTEAUBOURG et DOMAGNÉ (35). parc d'activités de la Goultière. tranches 1 et 2. mise en évidence d'une occupation du paysage du néolithique à l'époque gallo-romaine. dfs de diagnostic)
RAP03661 (HOEDIC (56). Les derniers chasseurs-cueilleurs côtiers d'Europe atlantique et la mort : étude interdisciplinaire de la nécropole mésolithique de Hoedic)
RAP03548 (DINEAULT, PLOMODIERN, ROSNOEN (29). Prospection diachronique Basse vallée de l'Aulne. Rapport de PD 2017)
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)
RAP03316.pdf (PLOUHINEC (29). Ménez-Dregan 1 : des Prénéandertaliens aux Néandertaliens à l'extrême ouest de l'Europe. Rapport de FP)
RAP01557.pdf (PLOULEC'H (22). le Yaudet. rapport final de synthèse de fouille programmée 1996-1998)
RAP02029.pdf (l'âge du bronze en centre Bretagne. rapport de prospection thématique)
RAP03284.pdf (éléments pour une nouvelle approche de l'âge du Bronze en Bretagne ; le cadre chronologique et les formes de l'habitat. Rapport de PCR 2015)
RAP02005.pdf ((29). le mésolithique en Bretagne. rapport de projet collectif de recherches)
RAP02143.pdf (LILLEMER (35). une enceinte du néolithique moyen à Lillemer. rapport final de synthèse de fouille programmée 2003-2005 et de prospection thématique)
RAP01982.pdf ((29). les sites mésolithiques en Finistère : chronologie et stratigraphie. rapport de prospection thématique avec sondage)