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RAP00566.pdf ((56). quatre communes du Morbihan : carentoir)
  • of fieldwork, itself part of a larger, mul t i -di sci pl i nary study of the relationship between and settlement during the last two thousand years, took place from 21 March - 5 April and 6 -- 27 September in the communes of Ruffiac, Treal, St~Ni col as-du-Tertre , Carentoir, La
  • involved fieldwalking over large areas at wide intervais, as in 1982 85, in the four core communes; sampling in the communes surrounding the core? and excavation of parts of a field from which 'total' collection had previously been made. Two days (21-22 March) were spent in préparation
  • for the main season by two people. The team (consisting largely of past and présent students from the Universities of London, Reading, Durham and Sheffield) numbered twenty, including the directors, and worked for twelve days, from 23 March, with one day off. A smal 1 team, of the directors
  • and two others, returned on 28 April for three days in order to complète the excavations. Overall, 317 mandays were spent on this year's Easter seasons (303 by the main team), including travelling time and time off 5 255 (244) of thèse were working days. The weather was dreadful
  • worked flints were also collected, three from transect E, three from B, two from B and one from D. One possible platform and thirty lynchets were noted, of which fifteen were in Transect D. As in previous years there were considérable variations in the concentration of recovered
  • pottery, and the saine conventions are hereby used to distinguish between thems fields in which more than two neighbouring units each produced five or more sherds of the same broad period (or five or more fragments of building material) have been termed 'sites'; fields in which one
  • unit produced five or more sherds or fragments of building material, and two or more neighbouring units produced one to four, gr. two neighbouring units each produced five or more sherds or fragments, have been termed 'probable sites'; fields in which there were irregular
  • absorbing 42 working days. Two 6m squares were excavated (see fig. G), One, T3, was located on the highest part of the field, where surface prospection had identified both large amounts of pottery and concentrations of phosphates (Asti 11 and Davies 1983s 16, 18). The second, T4
  • . The first (T7) ran north west from T3 across a slight break in si ope, and the other two (T5 and T6) were eut in order to section the platform near T4 (see fig. C) . The-? sections were cleaned and drawn and features in the bottom of the trenches recorded. The two 6m squares were mai ni
  • , 67. table wares of fabrics 5 and 6, and 47. storage vessels of fabric S. Most of T4 was dug by hand in a similar way to T3 , but in the later stages a machine was used to remove some of the colluvium. Two im-wide trenches were also eut by machine. One (T5) , 22m long, extended
  • from T4, where three i nter-cutt i ng ditches were eut into the natural» It was only possible to section two of them in the time avail cible and the task of establishing the relationship between the three features was postponed until 1987» The sectioned ditches were bot h U-shaped
  • The 1986 Sept ember season involved sample excavation of parts of four fields (H145, K446, H80, A92) from which 'total ' collection had previously been made (fig. i). One day (5-6 Sept) was spent. in préparation for the main season by two people. The team (consisting of volunteers from
  • a wide range of places) numbered twenty-one, including the directors and Alan Lane, and worked for ei ghteen days, from 7 September , with two days off? Anne Gebhardt joined it for soil sampling for the second half of the season, and was assisted by a f ri end for the 1 ast week
  • . Overal 1 , 481 mandays were spent on the September season, including travelling time and time off§ 437 of thèse were working days. The weather was poor during the second week, with considérable rainfall, but only two complète days were lost in t 11 e field. \3> EBS 86 Fi g. 1 H
  • arable land-use and smal 1 enclosures (çl_os) , with two buildings and ? walled yards inside its western edge - since démoli shed. The site of thèse buildings i s presumably now marked by a remembrement mound near the junction of the two road s. Excavation strategy was the same
  • médiéval pottery to the rier t h classify the two fields as a 'site'. In March 1986 intensive surface collection was rnade from most of the two fields. The distribution of médiéval and post-medi eval pottery on K446 was of a 1 ow and even density, although there appeared to be more
  • of an arable lave been field, close to two small curtilages, which may abandoned earlier house plots. (The cadastral plan of Becul eu as a whole shows a great nurnber of thèse empty curtilages and suggests that the settlement of Becul eu had once been considerably larger.) The possible
  • the was necessary to establish the character of extended wh ère ver it cases (T26, T27) this was done by machine. features, and in two Features proved difficult to identify because they were often slight and because the natural subsoil and bedrock varied so much. In ail appr ox i matel y 52
  • clay subsoil (37), into which features had been eut. A small pit (35) was excavated in the south end of the trench, and a séries of uneven holes, interpreted as root holes (40) , were also found. The remaining features consisted of two irregular spreads of charcoal (39, 43), which
  • , and Subsoil and schiste I ay i mmed i ai t e 1 y b e (45) . At the eut into this natural s e v e r a 1 f e a t u r e s had been 35cm deep (44) , southern end a v shaped diteh, 60cm wide and produced two médiéval pottery sherds (fabric group 1). The most K446 prominent feature
RAP02884.pdf ((35). activités minières et métallurgiques en haute Bretagne. rapport de prospection thématique)
  • datants) ne permet pas d’établir avec précision la chronologie relative entre les deux sites. Le volume du ferrier décrit par les habitants locaux, encore en élévation au cours de leur jeunesse, est du même ordre de grandeur que celui de Pilleverte, ce qui porte à croire qu’un tonnage
  • chauffé. Un bloc gris-mauve et violacé de près de 400 g montre quant à lui, une très forte attirance à l’aimant sur un tiers de son volume (photo n°4). Sa forme quadrangulaire avec traces linéaires sur une face et sa couleur sont assez atypiques. Jusqu’ici les occurrences de gisements
  • de terrain plus approfondie réalisée en 2011 a permis de reconnaître l’emplacement du dépôt et d’observer sa nature (photos 8 à 12). Le volume résiduel se présente sous la forme d’un monticule allongé se déployant, à partir de la route départementale, le long du chemin transversal
  • , sur une longueur d’environ 6 m, pour une largeur de 3-4 m. Sa hauteur moyenne se situe au voisinage d’1 m. On peut estimer son volume à environ 15-20 m3. Après défrichement des fougères qui se sont développées dessus, il nous a été donné de constater que la masse était très
  • l’ordre de 1 ou 2 km. On peut noter aussi que le ferrier gallo-romain de La Sourcinière à Plesder, dont le volume pourrait être évalué à plusieurs centaines de mètres cubes d’après les témoignages de personnes l’ayant vu en élévation avant qu’il ne soit transformé en berge d’une pièce
  • scories écoulées. La partie accessible à la prospection occupe une surface visible, de l’ordre de 3 500 à 4 000 m², équivalente à un cercle de 70 m de diamètre, pour une hauteur proche de 2 m. Son volume peut donc être estimé au voisinage de 7 500 m3, pour la partie qui a pu être
  • des propriétaires de cet espace privé. 17 SITE : LA MONTAGNE / RUE DES FERRIÉRES COMMUNE : TEILLAY (35) Echantillon : 35 JUIGNÉ P12 S5 TENIER 2011 Radiocarbon Age 590±20 Calibration data set: intcal09.14c # Reimer et al. 2009 Two Sigma Ranges: [start:end] relative area One
RAP02332.pdf (PAIMPONT (35). le Bois Jacob. rapport de fouille programmée annuelle)
  • % probability) and the hollow bars represent two sigma statistics (95% probability). Marine carbonate samples that have been corrected for 13 C/ 12 C, have also been corrected for both global and local geographic reservoir effects (as published in Radiocarbon, Volume 35, Number 1, 1993
  • determinations are applied to convert BP results to calendar years. The short-term difference between the two is caused by fluctuations in the heliomagnetic modulation of the galactic cosmic radiation and, recently, large scale burning of fossil fuels and nuclear devices testing. Geomagnetic
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
  • 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
  • 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
  • , and only two days were lost because of rain; however , the gênerai dryness meant that the ground was hard and made for very heavy working. EBS 88 B409 (Carentoir Zft 161) B409 lies on a west-facing si ope near the settlement of Le Eiois Guillaume, documentée! from the eighteenth
  • ' collection. Late IronAge/early Roman pottery was recovered (maximum 6 sherds per 5m square) and this tended to concentrate in two areas in the field. The much larger quanti ty of médiéval pottery (maximum 22 sherds per square) had a si mi 1 ar distribution, while the post— medi eval
  • charcoal (16) and smail 1 fragments of mudstone; this produced two smal 1 and abraded sherds of Iron-Age pottery (Fabric 86); the upper fill (15) had no finds. Another pit was also found in the north section (22: lm wide, 0.42m deep) whose fill (23) had no finds but more mudstone
  • . The range o-f pottery recovered -from the top two spits was very différent -from the lowest spit. In the first twenty centimètres 45 sherds were -found; médiéval pottery predominated (837.), -followed by post-medi eval (157.) and a single sherd o-f Roman pottery (27.) ; 52 -fragments o-f
  • large Roman settlement which lies 100m to the south east (see fig. 2). In sura , then , this 6m square produced évidence of an early agricultural phase, followed by two phases of Iron-Age activity, and then a later - perhaps mue h later - agricultural phase. Although there is a large
  • was not présent in such quanti ti es. Although the area excavated was so small, it is sufficient to reveal that this zone is of exceptional importance as a long-used settlement area - Iron Age, Roman nearby to the south east, two seigneurial sites hardby (Le Bois Guillaume and La Touche au
  • 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
  • , loosely compacted quart:-: pebble conglomerate and riverine gravel . The lower fill (17) had more stone (47.7kg) than the upper (16: 19.6kg): the différence may reflect two separate dumps of soil; the cleanness of the fillings, the comparât i vel y small number of finds and the lack
  • ring, three sherds of grey coarse ware, two sherds of fine cream ware and a body sherd of an Iron-Age fabric; only one small pièce of ceramic tile was found . Trenches 42, 43 and 44 After the cornpletion of T28 three lm-wide trenches were eut mechanically to try to establish
  • the same corner and was 4.5m long; T44 was eut north from the north-east corner of T28 for 4.4m (fig. 3). In T42 two ditches were located eut into the natural . One (24) was lm wide and about 0.2m deep and was fi lied with a loam (23) similar to the plough soil. The other (39) was much
  • to that of 10. The finds, though more plentiful, were similar in range: 14 sherds of grey coarse ware jars, 4 sherds of ter ra-ni qra -type pottery, 6 sherds of Iron-Age fabric and two pièces of ceramic tile were found. There was another ditch (11) in the south of the trench, eut
  • 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
  • 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
  • ) . At a later stage two further trenches were eut mechanically 30m either side of T39 (T40 to the south, T41 to the north). The sides of the trenches were cleaned by hand and recorded; the lowest part of the plough soil and features were excavated by hand. In one case T39 was extended (T46
  • 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
  • sherd of late Iron-Age/earl y Roman pottery (Fabric 15) and one sherd of vessel glasB. This had a light olive-green colour. Further down the slope, within 10m of pit 17, two ditches were located which had a similar character; both had shallow 'U' shaped profiles; and were apparently
RAP00565.pdf ((56). quatre communes du Morbihan : carentoir)
  • EAST BRITTANY SURVEY: QUST-VILAINE UATERSHED REPORT ON FIELDWORK IN MARCH-APRIL 1985 The fourth season in a programme of fieldwork, itself part of a larger, multi-discipl inary study of the rel ati onshi p between land-use and seulement during the last two thousand years, took
  • ; the main team (consisting largely of past and présent students from the Universities of London and Reading) numbered twenty-two, including the directors; it worked for twel ve days, from 24 March, and had one day off; nine people (including one director) remained for an additional week
  • to concentrate upon the excavation. Overall , 434 mandays were spent on this year's season, including travelling time and time off; 364 of thèse were working days. Two of the main team spent most of their time assisting in a survey of standing buildings already in hand when the season started
  • and two adjacent transects in Carentoir (F and C), which had been inadequately covered in 1983 because of the height of the crop, were rewalked; F included the cadastral and modem village of Carentoir (see fig. 1). Except for a small area in the north of C, and for fields previously
  • , but sixteen worked flints were recovered, three from transect L, three from C and ten from F, and also a stone axe, the stone of which has yet to be identified (F117). Two possible areas of ridge and furrow were noted, along with fourteen lynchets and eight (mostly substantial) old banks
  • . As in previous years there were considérable variations in the concentration of recovered material, and the same conventions are hereby used to distinguish between them: fields in which more than two neighbouring units each produced five or more sherds of the same broad period (or five
  • or more fragments of building material) have been termed 'sites 1 ; fields in which one unit produced five or more sherds or fragments of building material, and two or more neighbouring units produced one to four, or two neighbouring units each produced five or more sherds or fragments
  • fragments of brick and tile (6.58g). The assemblage included five worked flints, one pièce of haematite and two pièces of tegul a. Although black/grey and grey/green schiste were présent ail over the field, and looked like natural , red/yellow schi ste was distributed in a pattern
  • ) and 6.36 fragments of brick and tile (115.57g). The assemblage included second-century central Gaulish Samian and rims of third/fourth-century types; thirty-eight pièces of tegul a and twenty-nine of imbrex; three pièces of haematite (310g) and two worked flints. Magnetic susceptibil
  • the same alignaient as the lynchet. The ditch was fi 1 1 ed with a homogeneous silty loam which contained two sherds of médiéval pottery and two pièces of (? médiéval) tile. The fill of the ditch was indistinguishable from the overlying thick 1 ayer of loam, which constituted the main
  • 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 récognition of characteristic seventeenthand 1 ate nineteenth-century types. It is clear that some settlements have a prépondérance of one or other of the two common types of building - the single cell , with ground floor hall and storage loft above, and the long-house, combining byre
  • as coniferous) can hardly be more than two hundred years old. In such ways surface scatters, in association with other évidence, are beginning to suggest precisely localisable changes in land-use, especially during the 1 ast millenium. This year also saw a major attack on the problem
  • introduced into the field bounded by the lynchets and eut by Trench 1, need some further investigation. The next season Next year will see two main seasons of fieldwork: fieldwalking and small excavation from 22 March - 5 April 1986 and three weeks of excavation during September
  • of the quai ity of préservation of sites; two 25m squares within the field have already been prospected using a f 1 uxgate gradiometer in order to assist choice of areas for excavation. Thereafter further sites from which 'total' collection has been made will be investigated in small areas
RAP00567.pdf ((56). quatre communes du Morbihan : carentoir)
  • EAST BRITTANY SURVEY 1987 PU EAST BRITTANY SURVEY - OUST/VILAINE WATERSHED EASTER 1987 The seventh season in a programme of fieldwork, itself part of a larger, mul ti -di sci pl i nary study of the relationship between 1 and-use and settlement during the last two thousand
  • , Reading, Cardiff and York) numbered twenty-two, ' including the directors, and worked for twel ve deiys, from 22 March, with one day off. Six people went in advance, and worked for one day beforehand. Overall, 330 mandays were spent on this year ' s season, including travelling time
  • (752 ha.), and 14.67. of the portion of Transect R walked (197 ha.): see fig. 2. Two sets of cropmarks, one platform and two areas of ridge and furrow were noted in M, together with forty-one lynchets; four and three lynchets, respect i vel y , were noted in P and R. 32.82kg
  • of pottery, 161.72kg of man-made building material, 23 from thèse flints and 611.72g of haematite were recovered transects , together with two worked pièces of quartz (from M). This breaks down, by transect, as follows: Brick/tile kg 18. 49 P M 121 . 77 21 . 46 R Pre-Rom. Pottery 1 . 47
  • there were considérable variations in the concentration of recovered pottery, and the usual conventions are hereby used to distinguish between them: fields in which more than two neighbouring units each produced five or more sherds of the same broad period (or five or more fragments
  • of building material) have been termed 'sites'; fields in which one unit produced five or more sherds or fragments of building material, and two or more neighbouring units produced one to four, or. two neighbouring units each produced five or more sherds or fragments, have been termed
  • two groups of 'blank' fields south east and south west of Comblessac. Together thèse zones suggest that the settlement of Comblessac and its immediately dépendent arable may have been rather small, much smaller than the centres in the core communes: it is notable that a tile
  • further. This is not the place -For comprehensi ve considération o -F contrasts between the core communes and the transects sampling the surrounding area o-F the Oust/Vilaine watershed. However , it may be useful to make one or two observations about the material, prior to sustained
  • was found near Le Boschet, Château de la Boulaye, 'Château Gaillard' (ail in M) and near le Mur (R) . There are, however, two cases of such material being found near (apparently) non-seigneurial settlements 300m from Comblessac in R and 100m from La Rigaudiere, 1km south of Pipriac, in M
  • and nearby M509, M516, M542) , and as in the core the quantities of Roman pottery were very small. Thèse tile scatters were sometimes surprisingly extensive, being évident over a distance of 300, and sometimes even 600m. In two cases fields were walked in the vicinity of already known
RAP03077.pdf ((22)(35). paléométallurgies du fer en haute-Bretagne de la protohistoire à la période industrielle. rapport de pt 2014)
  • ferrier dans lequel apparaissent des scories et quelques fragment d’argile cuite orange (photo n°4). Compte tenu des quantités très importantes de scories et sédiment reconnues, il s’agit d’un site de production massive, dont le volume d’origine atteignait et dépassait même
  • la fin du bas moyen-âge (mentions historiques jusqu’au 15e siècle). Compte tenu du volume du ferrier, il remonterait probablement au moyen-âge central ou au bas moyen-âge, mais dans l’état actuel de la question seule une datation C14 permettrait de s’en assurer. Bien que démantelé
RAP03438 (BADEN (56). Rue du Lannic : installation funéraire à l’âge du Bronze et occupation domestique de la Tène au début de l’époque romaine. Rapport de fouille)
  • . In the 1.400 m2 of excaveted area, a funerary complex composed of three graves constructed in stone cist witness of a long funerary occupation. Two of them are preserved in the base of a cairn. Despite the lack of bones and contemporary artifacts, these two graves provides radiocarbon
  • niveau marin est due à une augmentation du volume des océans suite à la fonte des calottes glaciaires (eustasie), et aux réajustements isostatiques de la lithosphère, qui sont ainsi les principaux agents d'évolution du niveau marin à l'Holocène (Stéphan et al., 2013 ; Stéphan et
RAP03300.pdf (RANNEE (35). La Chaussée. Rapport de fouille)
  • the to Bronze and Middle Ages (La Sallerie), two domestic occupation sites dating to the transition between the Bronze and Iron ages (Les Rimbaudières et La Pinelière), a rural habitation dating to the late Iron Age (La Chaussée) and a roman road (La Grande Bécannière). An excavation
  • a rural habitation dating between the second century BC and the first century AD. Excavations at La Chaussée provide data documenting the western edge of this site. The La Chaussée site is characterized by a series of parallel east-west ditches that cross the study area ; the two
  • between this two northern ditches, there is little evidence demonstrating the structuring and modification of the site. Indeed, the majority of the observed stratigraphic relationships are primarily modern / contemporary ditches that cut the earlier late Iron Age structures
RAP02283.pdf (BAUD (56). Kervin. un camp militaire romain ? dfs de diagnostic)
  • comprise a single rampart and one or two ditches. A single gâte is usual, tvuo gâtes being rare. Internai buildings consist of small barracks and sheds... It seems likely that the fortlets themselves tuere relieved from main garrisons and that permanent duties tuere not required
RAP03553 (PLERIN (22). Centre Hélio-Marin : bâtiments associés à la pars rustica de la villa gallo-romaine de Port-Aurel. Rapport de diagnostic)
  • plans Vérane Brisotto Inrap Spécialiste lithique Étude du mobilier lithique Marina Biron, Inrap Spécialiste ,conservation du mobilier métallique Stabilisation et nettoyage du mobilier métallique Brice Ephrem, Ausonius Ichtyologue Tamisage et étude ichtyologique Véronique
  • CRAVO et Véronique Matterne pour l’étude carpologique et à Brice Ephrem (Ausonius) pour l’icthyofaune. La stabilisation et la restauration du mobilier métallique ont été confiées à Marina Biron (Inrap). Enfin, une étude sur la présence de pêcherie le long de la Pointe du Roselier
RAP03801 (Corpus des signes gravés néolithiques, Art rupestre néolithique en Armorique. Rapport PCR.)
  • les intentions du programme 1.3. Principes Nous devons nécessairement passer par une étape d’enregistrement des surfaces et donc des volumes, en mettant en œuvre des techniques éprouvées mais cependant récentes qui permettent des levés numériques 2D/3D des gravures et des levés 3D
  • /photogrammétrie et lasergrammetrie selon les cas, afin de restituer la morphologie tridimensionnelle des supports, volumes dans lesquels seront rapportés les signes gravés levés par… photographies compilées sous éclairages tournants obliques (réels ou virtuels), voire, dans certains cas
RAP02921.pdf (TORCÉ (35). Mauzé. rapport de fouille préventive)
RAP03345.pdf (QUIBERON (56). Beg-er-Vil : Un habitat du Mésolithique sur le littoral du Morbihan. Rapport de FP)
  • préliminaires .............................................................................. 70 3 Campagne 2016 2. La gestion technologique des volumes des nucleus : comparaison des systèmes techniques de Beg-er-Vil (Quiberon, Morbihan) et de Beg-an-Dorchenn (Plomeur, Finistère
  • pièces cotées (années 2012 à 2015) par Diana Nukushina (Thèse de doctorat de l’Université de Lisbonne et Rennes 1) • Etude de la série lithique 2014 par Gaëlle-Anne Denat et développement d’une méthode d’étude des volumes débités (Master 1 de l’Université de Rennes 2). • Etude
  • a fallu l’imbiber d’eau douce cette fois (pour ne pas altérer les analyses chimiques, ni faire d’auréoles de sel), presque en permanence. Le tamisage à sec des sédiments a également été réalisé systématiquement, qui permettait de réduire les volumes des trois-quarts à la moitié
RAP03240.pdf (PLOUEZOC'H (29). Grand cairn de Barnenez : nouvelles approches, nouveaux résultats, nouvelles perspectives. Rapport de FP 2015)
  • a été réalisée des parties accessibles précisément du tumulus nord de Barnenez. Seuls de la table pour pouvoir découper des sections sur la table de couverture et ses abords sont acces- celle-ci et avoir un volume précis . Le profil du sibles actuellement. bloc est en biseau
  • occi- d’érosion sont présentes sur la face supérieure pri- dentale ne peut pas être estimée. Seule un dolmen vilégiant une extraction sur estran. Le volume don- a pu être observé, malheureusement son état ne né par le modèle 3D est de 2,65 m3 donnant un permet pas de savoir
  • une superposition des un effet de marnage et difficilement franchissables deux volumes pourrait être un argument supplé- notamment au niveau du littoral de par leur lar- mentaire. Une autre possibilité est d’impacter des geur. Le paysage autour du monument était donc voies de