The Shaugh Moor project is concerned with an area of moorland in south Dartmoor north-east and north respectively of the villages of Shaugh Prior and Wotter (fig. 1). The physical threat to the evidence for settlement and land-use caused by the operations of the China Clay industry involved the Central Excavation Unit of the Department of the Environment from 1976 in a programme of survey, excavation and environmental studies related to the settlements, land boundaries, burial mounds and ceremonial structures that are to be found on this piece of moorland. The background to the project and its preliminary research strategy have been outlined in Paper I (Wainwright et al. 1979) and this publication describes the investigation of a stone-walled enclosure surrounding houses and other structures that was totally excavated in 1977 and 1978. Subsequent papers will describe the related archaeological and scientific investigations into the past environment and land-use of this block of moorland and its adjacent region.
Viewed from the south Devon littoral with its series of good harbours the dark bulk of Dartmoor is clearly visible across the flat coastal plain. It is the largest of the five granite masses that provide a spine to the south-west English peninsula (Dartmoor, Bodmin Moor, Hensbarrow, Carnmenellis and Penwith) that were formed by the consolidation of molten material. The 500 square kilometres of the Moor form an undulating upland up to 600 m OD on the north-east side, where the greatest elevations occur. In the southern parts of the Moor the rolling tableland is 300 m to 420 m high—modern cultivation tends to cease at the 300 m contour, that is broken by numerous upland valleys and the eroded remains of tors. Today this expanse of moorland is bleak and treeless except in river valleys at the rim of the granite escarpment, although patches of contorted oak woodland survive at Piles' Wood on the River Erme, Wistman's Wood on the West Dart and Black Tor Beare on the West Okement. Pollen analyses have shown, however, that up to a height of about 360 m Dartmoor was probably covered by a deciduous forest dominated by oak that was gradually eroded by climatic trends and human activity (e.g. Simmons, 1969). It is from this central mass that the rivers of south Devon diverge. The wide upland valleys of the Tavy, Plym, Yealm, Erme, Avon and Dart plunge through characteristic deep wooded gorges near the southern granite escarpment into the South Hams and around this border modern settlement—numerous villages and a few towns are situated.
The third phase of the Shaugh Moor Project comprised survey and excavation work on the Saddlesborough Main reave and Wotter Common (fig. 1). Following the decision of the china clay companies not to develop the area immediately around Saddlesborough (Area Y), Watts, Blake and Bearne & Co Ltd and English China Clays Ltd embarked upon a joint tipping programme which will eventually destroy the terminal reave east of Saddlesborough and most of the monuments on Wotter Common (fig. 2).The area to the north of Saddlesborough was surveyed in 1976 and limited excavation was undertaken early in 1977 (Site 10, Wainwright et al 1979). An enclosure, 1 km to the north-east of Site 10, was totally excavated in 1977 and 1978 (Site 15, Wainwright and Smith 1980). In 1979 and 1980 the area threatened by the quarry extensions was surveyed and a programme of limited excavation was undertaken on the Saddlesborough Main reave and Wotter Common (Site 208).
Winklebury Camp (SU61355290), an Iron Age 'plateau fort’, now of some 7.6 hectares (19 acres), is situated in the parish of Basingstoke, approximately 1 mile north-west of the town centre of Basingstoke, (fig. 1), though it is now surrounded by housing estates. It occupies a hill of Upper Chalk which has been isolated from the main mass of the North Hampshire Downs by two dry river valleys, one trending south-east, the other north-east. Both are tributary to the R. Loddon. The hill rises to a maximum height of 126 m a.s.l., near the projected line of the western rampart and slopes off gradually to north and south, and more steeply to the south-east. About half a mile to the south of the fort, a tributary of the R. Loddon, now culverted, would have provided the nearest source of water.Winklebury Camp has suffered from gradual encroachment by the surrounding housing estates, losing the ditch and rampart face to the north and east, and ditch, rampart and a small part of the interior, to the west. Only to the south does any of the bank and ditch survive. In the south-west corner of the fort, in an area protected by the remains of a small copse, a 90 m length of eroded rampart remains to an approximate height of 2 m. There is no ditch fronting this rampart now, but immediately east of the end of the stretch of rampart is the only remaining length of ditch. This extends for some 200 m along the remainder of the south side of the fort, averaging 2 m deep and 5 m wide. It rises in the south-east corner at a causeway, beyond which is another short stretch of ditch which is rapidly lost in house gardens. This causeway is faced by rampart, but there are indications, for example a slight change in the direction of the rampart at this point, that this is in fact a blocked entrance.
For five years from 1976 to 1980 the archaeology and environment of a block of landscape centred around Shaugh Moor on south-west Dartmoor were analysed prior to the destruction of some of the evidence by china clay working. The investigations began in 1976 with a survey of the field monuments and the initiation of soil, vegetation, small mammal and phosphate studies in addition to the search for peat deposits of sufficient antiquity. From 1977 the programme was determined by the encroachment of the quarries and other works, so that early in that year a group of cairns were excavated (site 10) and subsequently the first of two seasons work on a walled enclosure (site 15) was initiated. The excavation of the enclosure was completed in 1978 and in that year it was also necessary to undertake a small investigation near the northern edge of the project area on the Trowlesworthy cross-dyke (site 202) and near its southern edge on Wotter Playground (site 201). Settlements and field systems were surveyed and excavated on Wotter Common in 1979 and these investigations were completed in 1980 when the Saddlesborough Reave, which crosses the centre of the project area from east to west was also surveyed in detail and sampled by excavation.More field work could have been undertaken on threatened areas and indeed a limited operation was undertaken in 1981 on the Saddlesborough Reave to confirm some points of detail. Instead, it was thought best to conclude the project after five years, to complete the publication of the results and to allow mature consideration of these so as to generate a new set of questions.At an early stage the decision was taken to publish the work as a series of annual reports in theseProceedingsrather than as a single monograph. The first report (Wainwrightet al.1979) set out the simple research design for the project and contained accounts of the 1976 survey and of the excavation of the cairn group.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
hi@scite.ai
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.