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Auteur
ASTILL Grenville [X]
Type d'opération
Département
56 [X]
Date (Année)
1988 [X]

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RAP00568.pdf ((56). quatre communes du Morbihan : carentoir)
  • (56). quatre communes du Morbihan : carentoir
  • 56
  • (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
  • ; the cadastral work allows total reconstruction of the early rà neteenth- century ] andscape and is of parti cul ar value for the fieldwork programme (Asti 11 and Davies 1982, 1983, 1984, 1985, 1986, 1987)." The 1988 season involved sample excavation of parts of seven fields (B409, A92, A31
  • five-day planning trips by two in September 1987 and April 1988. The team, consisting of volunteers from a wide range of places, numbered twenty-six, including the directors, one finds assistant and three supervisors; it worked for f i ve weeks from 28 August, with four days off
  • . Anne G'ebhardt joined it for a day for soi 1 sampling and Tony Stevenson for two days for pollen sampling. Overall, 938 mandays were spent on the 1988 season, including travelling time and time off; 787 of thèse were working days. The weather was idéal for much of the season
  • material was obtained from T29 (as was reflected by the results D -f the total collection) but more Roman pottery was found. Time ran ont and the sites had to be backfilled at the point, when ditches were recognised (Asti 13. and Davies 1987, 118-21). In 1988 the excavation was resumed
  • (30 and 57); they did not eut each other. The fill (56) of pit 57 had 1 sherd of a Roman grey coarseware (Fabric 216); that. of pit 30 (29) produced no finds. There? were no features in the trench for a long section of the slope, some 26m, and then there was a further group of pits
  • holes were excavated, most within the southern part of T32 and T38 (48, 54, 58, 56, 42: with fills 53, 55, 59, 57 and 43). Al I the features of this timber phase were shallow (0.1-0. 2m deep) and appear to have been truncated; this may have happened in the course of ploughing