39 EXCAVATIONS AT RADCLIFFE TOWER 1979-80 N Tyson Radcliffe Tower (Fig I) stands 140m W S W of Alluvial sand and gravel underlying the site prob- Radcliffe parish church (SD 796074) about 1.2km ably supported a ground-water gley soil on the east of the modern town centre, at a height of 68m floodplain, but the more freely-drained terrace OD. It occupies the first terrace above a flood- upon which the tower was built is a brown earth of plain in a loop of the River Irwell below its con- the Downholland association. Middle Coal Measure fluence with the River Roch. This loop takes the Trencherbone or Cannel Rock sandstone used in con- Irwell from the general southerly course which it struction would have been available locally. There follows from the Rossendale uplands to this point, are numerous coal seams in the locality, the near- westwards through a deep post-glacial gorge to Nob est being the Top Five Quarters mine which runs End. south west about 50m south of the tower. Whilst some reclamation has been carried out and more is planned, the valley at this point still bears the scars of industrial exploitation, although some relict woodland survives on the high south bank overlooking the floodplain. |n 1950 enigmatic timber structures were revealed by gravel digging near the confluence of the Roch and Irwell, and Mesolithic flints were reputedly found. Stone axes of Neolithic and Bronze Age date have been discovered, and a fine cast-flanged bronze axe was found in 1949 (Spencer 1950). More timber structures were excavated lower downstream in 1961 (Hallam 1961). During the Roman period gravel was probably quarried in the vicinity for the construction and maintainance of the Manchester-Ribchester road, which runs close by. Domesday Book records Radcliffe as being held by King Edward as part of the Royal Manor of Salford. After the Norman Conquest, the Baron de Mersey gave Radcliffe manor to Nicholas Fitz-Gilbert de Talbois who adopted the place name as his surname and thus founded the Radcliffe family. The family prospered during the medieval period, with branches in poss- ession of Ordsall Hall Salford, Smithills Hall Bolton and Baguley Hall Wythenshawe. In August 1403 James de Radcliffe was granted a licence to rebuild his manor house "... with walls of stone and lime, to enclose anew and within those walls erect a hall and towers ..." During the medieval period a park and fishponds could have been accommodated in fairly close Fig 1 Radcliffe Tower : site location proximity to the manor house. This is implied by an indenture of exchange dated 1338 between Richard such landscaping took place. de Radcliffe and William del Grenehurst, of tene- ments in Radcliffe called Gorill and le Light- The aims of the 1979 excavation were to establish birches within the 'New Park' (Irvine MSS 49). the nature and extent of surviving stratigraphy and locate an inferred enclosing wall. Discovery of an By 1518 the main line ceased with the death of John apparent moat or ditch section prompted further Radcliffe, when the manor passed to Robert work in 1980 to determine its direction. Radcliffe, subsequently first Earl of Sussex of the Radcliffe family. In 1561 Thomas Radcliffe, third THE EXCAVATION (Fig 2) Earl of Sussex, sold the manor to Richard Ashton of Middleton for 6000 marks (Hampson 1940). Six trenches (A-F) were excavated by hand, effec- tively sectioning the north-west corner of the site An illustration showing the hall with a ruined from the hall area to the modern north and west tower attached was drawn for Dr Whitaker in 1781, boundaries. Only plans and sections of trenches A, by which time its status had been reduced from C and F are reproduced here, with most 19th century manor house to farm. By the mid 19th century the features omitted from plans. A ground plan, four hall had been demolished leaving only the ruined external and four internal elevations of the tower, which remained in use as a farm building surviving Tower remains were also drawn (Tyson until after 1950 (Tyson 1985). 1985). CIRCUMSTANCES OF THE EXCAVATION Work was carried out in September 1979 and April 1980 by volunteers under the direction of Bury Gravel quarrying carried out more than thirty years Archaeological Group. Trenches were backfilled by ago on the flood plain of the river resulted in the machine after F.F25 had been covered with poly- formation of lagoons, which were subsequently thene. The site has since been levelled up and filled with industrial waste. As tipping was to grassed. Finds and the archive have been tempor- continue throughout the nineteen eighties, the site arily deposited with the Group secretary. owners proposed to landscape the tip entrance in 1980. Since this lay over the area of the main Acknowledgements hall, west wing and courtyard, it was considered essential to determine the archaeological potential Special thanks are due to the people who took part of the site so that this might be respected when in the excavation and to Stephen Moorhouse for his CHURCH STREET EAST " EOT 4SO 3795440750 1 2kn C-COAL MEASURES T-RIVER TERRACE J SG-SAND4 GRAVEL BC-BOULOER CLAY SURVEYED: BURY ARCHAEOLOGICAL GROUP DRAWN: MARK FLETCHER 1982 Fig 2 Radcliffe Tower : site plan report on the aludel. Grateful thanks are due to THE FEATURES the site owners Wimpey Waste Management for per- mission to excavate, and to the Planning Department of Greater Manchester Council and Bury Metro A full list of contexts in trenches A, C and F is Lottery for financial help. Valuable help was also given in Appendix 2, but the principal features on provided by Radcliffe Local History Society and the site were as follows: Bury Metro Leisure Services Department. Phase I a Ditch (Fig 3) SUMMARY OF MAIN PHASES Crossing the centraland southern half of trench C Since the medieval and early post-medieval phases a ditch or pit 7m wide by 1.5m deep had been dug cannot be reliably dated at this stage by finds, into the natural gravel. The sides sloped to a their chronology is based on the interpretation of flat base, 1.6m wide, which was covered to a depth the stone pitching laid down as part of a rebuild- of 450mm by a very dark greyish-brown organic silt ing phase in c 1403. The following sequence may be (19). Above this a dark brown clayey silt (18) tentatively suggested: formed a layer up to 800mm deep extending to within 2.6m of the north end of the trench. This second- Phase 1 a (medieval) rubble foundation and ditch ary silting was sealed across the centre of the or pit associated with ditch by a layer of dark brown silt containing earlier structure. charcoal and burnt clay (13), the. ends of which were truncated by later intrusions. Finally^ Phase I b(AD 1403) major rebuilding, extension overlying the layer of burnt material were several of courtyard and construc- lumps of roughstone up to 400mm square, including a tion of enclosing wall. single unweathered'sandstone ashlar 700mm long by 300mm-broad. These were levelled off wjth.dark' Phase ir a (c 1500-1730) construction of west wing; reddish-grey sandstone pitching (10)'iri a .layer up modification of enclosing to 250mm thick, thinning laterally and situated wall and later ditch fill-, across the centre-of the trench in a formation up ing. to 4m wide. The originql'exten't of this 'stone pitching could not be determined owing to distur- Phase II b(cl730-!840) construction of farm build- bance by 19th century foundations. A small pif . ings; demolition of hall (F|4) in the west section was sealed by' post-'' and certain farm buildings; medieval consolidation. construction..of .Tower Street cottages. Fig 3 Radcliffe Tower : trench C plan (top) and section (bottom) 42 Phase I a Foundation (Fig 4) formation I-2m wide, within Im of its west end. In the adjacent trench D at the same level were a few Situated approximately 7m inside the phase I ditch scattered fragments of sandstone, probably spread and projecting 1.3m from the south section of from B. Both areas had suffered extensive damage trench F, was an unrnortared sandstone rubble from !9tn century cottage foundations and floors. foundation (F25), 2.3m wide by 200mm deep. It Evidence of stone pitching was found in trench C rested on a gravel surface (21) sloping slightly to and has been described above. Extensive distur- the west, where the foundation depth increased to bance was caused in trench E by cellaring, but 400mm and where some perimeter blocks were up to vestiges of the feature survived as a layer of 600 mm long. The north edge of this feature was compact reddish-brown clay with small sandstone partly overlain by burnt clay, probably associated pieces, extending 1.4m from the south end to a with a hearth of phase II a, and it was cut diag- maximum thickness of 120mm. It was also present in onally by an old service trench. Patchy evidence a 2m wide formation across the trench 3m from its of sandstone pitching, as in trench C, also north end, albeit cut by a drain and service occurred. trench. Similarly in trench F, reddish-brown clay with sandstone fragments formed a patchy layer (7) Phase I b Enclosing wall (Fig 5) up to 100mm thick throughout, and was overlaid by slight remains of the west wing foundations A section of unmortared sandstone rubble wall described below. A dump of sandstone pieces, with foundation (F25) crossed trench A at right angles, occasional lumps of roughstone 300mm square, filled with its face 2.4m from the south end of the a depression 3.5m long by at least 1.2m wide in the trench, overlooking a shallow ditch.