Location | Whitehorse Hill, between Swindon and Wantage. (SU299863) |
---|---|
Region | Oxfordshire England |
Coordinates | 51°34′30″N1°34′09″W / 51.5750587°N 1.5692032°W |
Type | Hillfort |
History | |
Periods | Iron Age |
Site notes | |
Excavation dates | 1995 |
Archaeologists | David Miles, Oxford Archaeological Unit |
Condition | substantial earthworks |
Public access | Yes |
Website | English Heritage |
Designated | 1882 [1] |
Reference no. | 1008412 [2] |
Uffington Castle is an early Iron Age (with underlying Bronze Age) univallate hillfort in Oxfordshire, England. It covers about 32,000 square metres and is surrounded by two earth banks separated by a ditch with an entrance in the western end. A second entrance in the eastern [3] end was apparently blocked up a few centuries after it was built. [4] The original defensive ditch was V-shaped with a small box rampart in front and a larger one behind it. Timber posts stood on the ramparts. Later the ditch was deepened and the extra material dumped on top of the ramparts to increase their size. A parapet wall of sarsen stones lined the top of the innermost rampart. It is very close to the Uffington White Horse on White Horse Hill.
Excavations have indicated that it was probably built in the 7th or 8th century BCE and continued to be occupied throughout the Iron Age. Isolated postholes were found inside the fort but no evidence of buildings. Pottery, loom weights and animal bone finds suggest some form of occupation however. The most activity appears to have been during the Roman period as the artefacts recovered from the upper fills of the ditch attest. The ramparts were remodelled to provide more entrances, and a shrine seems to have been built in the early 4th century CE. Two oblong mounds, one containing 46 Romano-British burials and one containing eight Saxon burials, lie nearby.
An ancient track passes by the northern entrance to the hillfort; it is known as The Ridgeway. It links to the Icknield Way at the Goring Gap, and passes close to Avebury before heading south across Salisbury Plain. It also passes very close to a Neolithic chambered long barrow, Waylands Smithy, about a mile to the west.
The hillfort is a Scheduled Monument, [2] and was included in the Ancient Monuments Protection Act 1882 as one of the first 68 sites in Britain and Ireland to receive legal protection. [1] Along with the Uffington White Horse on the slopes below the ramparts, it is in the care of English Heritage. [2]
The Ridgeway is a ridgeway or ancient trackway described as Britain's oldest road. The section clearly identified as an ancient trackway extends from Wiltshire along the chalk ridge of the Berkshire Downs to the River Thames at the Goring Gap, part of the Icknield Way which ran, not always on the ridge, from Salisbury Plain to East Anglia. The route was adapted and extended as a National Trail, created in 1972. The Ridgeway National Trail follows the ancient Ridgeway from Overton Hill, near Avebury, to Streatley, then follows footpaths and parts of the ancient Icknield Way through the Chiltern Hills to Ivinghoe Beacon in Buckinghamshire. The National Trail is 87 miles (140 km) long.
Maiden Castle is an Iron Age hillfort 1.6 mi (2.6 km) southwest of Dorchester, in the English county of Dorset. Hill forts were fortified hill-top settlements constructed across Britain during the Iron Age.
Liddington Castle, locally called Liddington Camp, is a late Bronze Age and early Iron Age univallate hillfort in Liddington parish in the English county of Wiltshire, and a scheduled monument.
Segsbury Camp or Segsbury Castle is an Iron Age hillfort on the crest of the Berkshire Downs, near the Ridgeway above Wantage, in the Vale of White Horse district of Oxfordshire, England. It is in Letcombe Regis civil parish and is also called Letcombe Castle.
Roundway Down and Covert is an area of sloping chalk grassland close to the hamlet of Roundway, near Devizes in Wiltshire, England. It is part of the North Wessex Downs Area of Outstanding Natural Beauty. At the summit of the slope are ancient earthworks, evidence of a Bronze Age human settlement and Iron Age hillfort.
Plainsfield Camp is a possible Iron Age earthwork on the Quantock Hills near Aisholt in Somerset, England.
Dowsborough Camp is an Iron Age hill fort on the Quantock Hills near Nether Stowey in Somerset, England. It has been designated as a Scheduled Monument. The fort and associated round barrow has been added to the Heritage at Risk Register due to vulnerability to vehicle damage and erosion.
Blacker's Hill is an Iron Age hill fort at Chilcompton, 4.5 kilometres (3 mi) south west of Radstock, Somerset, England. It has been designated as a Scheduled Ancient Monument.
Kenwalch's Castle is probably an Iron Age hill fort that may have been converted into a Roman fortress, near Penselwood, Somerset, England, 6.6 kilometres (4 mi) east south east of Bruton at grid reference ST747335. It is a Scheduled Ancient Monument. It is believed to be named after Cenwalh of Wessex.
Maiden Castle is an Iron Age hill fort, one of many fortified hill-top settlements constructed across Britain during the Iron Age, but one of only seven in the county of Cheshire in northern England. The hill fort was probably occupied from its construction in 600 BC until the Roman conquest of Britain in the 1st century AD. At this time the Cornovii tribe are recorded to have occupied parts of the surrounding area but, because they left no distinctive pottery or metalworking, their occupation has not been verified. Since then it has been quarried and used for military exercises. It is protected as a Scheduled Ancient Monument, and is owned by the National Trust. The hill fort is open to visitors, but unrestricted access to the site has resulted in it being classified as "at high risk" from erosion.
Burrough Hill is an Iron Age hillfort in Burrough on the Hill, 7 miles (11 km) south of Melton Mowbray in the English county of Leicestershire. Situated on a promontory about 210 metres (690 ft) above sea level, the site commands views over the surrounding countryside for miles around. There has been human activity in the area since at least the Mesolithic, and the hillfort was founded in the early Iron Age. In the medieval period, after the hillfort was abandoned, the hill was used as farmland. This ended in the 17th century when the parish the hill was in was enclosed. Traces of ridge and furrow show where the medieval fields were ploughed. Since the 1930s the site has been the subject of archaeological investigations and renewed excavations under the auspices of the University of Leicester began in 2010. Part of Burrough Hill Country Park and open to the public, the hillfort is protected as a Scheduled Ancient Monument.
Eddisbury hill fort, also known as Castle Ditch, is an Iron Age hill fort near Delamere, Cheshire, in northern England. Hill forts are fortified hill-top settlements constructed across Britain during the Iron Age. Eddisbury is the largest and most complex of the seven hill forts in the county of Cheshire. It was constructed before 200–100 BC and expanded in 1–50 AD. In the 1st century AD, the Romans slighted the site. It was reoccupied in the 6th–8th centuries AD, and an Anglo-Saxon burh was probably established at Eddisbury in 914. In the medieval and post-medieval periods quarrying and farming have damaged the site. Ownership is currently split between the Forestry Commission and a local farm. Eddisbury is protected as a Scheduled Ancient Monument.
Blewburton Hill is the site of an Iron Age hillfort located in Oxfordshire, in the southeast of England. It was a univallate hillfort. The area is mostly farmland with some small areas of wooded copse to the south and the northeast. The hill fort may have been occupied from the 4th century BC to the 1st century BC, and replaced a small settlement surrounded by a stockade, which is estimated to have been built in the 5th or 6th century BC.
Scratchbury Camp is the site of an Iron Age univallate hillfort on Scratchbury Hill, overlooking the Wylye valley about 1 km northeast of the village of Norton Bavant in Wiltshire, England. The fort covers an area of 37 acres (15 ha) and occupies the summit of the hill on the edge of Salisbury Plain, with its four-sided shape largely following the natural contours of the hill.
Chiselbury is the site of an Iron Age univallate hillfort in Wiltshire, England. The hillfort is sub-circular in plan, and encloses an area of approximately 10.5 acres (460,000 sq ft). It is defined by an earthen rampart up to 3.6 metres (12 ft) in height and an external ditch, up to a maximum of 1.6 metres (5.2 ft) in depth. A gap in the south-eastern side of the rampart, and a corresponding causeway across the ditch, is thought to be the original entrance and is associated with a small D-shaped embanked enclosure, which is apparently visible on aerial photographs. Although the enclosure has subsequently been degraded by ploughing, it is still apparent as a series of low earthworks.
Hillforts in Britain refers to the various hillforts within the island of Great Britain. Although the earliest such constructs fitting this description come from the Neolithic British Isles, with a few also dating to later Bronze Age Britain, British hillforts were primarily constructed during the British Iron Age. Some of these were apparently abandoned in the southern areas that were a part of Roman Britain, although at the same time, those areas of northern Britain that remained free from Roman occupation saw an increase in their construction. Some hillforts were reused in the Early Middle Ages, and in some rarer cases, into the Later Medieval period as well. By the early modern period, these had essentially all been abandoned, with many being excavated by archaeologists in the nineteenth century onward.
Cornish promontory forts, commonly known in Cornwall as cliff castles, are coastal equivalents of the hill forts and Cornish "rounds" found on Cornish hilltops and slopes. Similar coastal forts are found on the north–west European seaboard, in Normandy, Brittany and around the coastlines of the British Isles, especially in Wales, Scotland and Ireland. Many are known in southwest England, particularly in Cornwall and its neighbouring county, Devon. Two have been identified immediately west of Cornwall, in the Isles of Scilly.
Torberry Hill is an Iron Age hillfort in the county of West Sussex, in southern England. It is a Scheduled Ancient Monument, with a list entry identification number of 1015966. The hill fort is located within the parish of Harting, within the South Downs National Park. The hill includes the remains of an Early Iron Age univallate hill fort, a Middle Iron Age promontory fort and a post-medieval post mill. The hill is a chalk spur projecting northwards from the South Downs.
Beacon Hill, also known as Harting Beacon, is a hillfort on the South Downs, in the county of West Sussex in southern England. The hillfort is located in the parish of Elsted and Treyford, in Chichester District. It is a Scheduled Ancient Monument with a list entry identification number of 1015915. The hilltop enclosure is dated to the Late Bronze Age, from the 8th to 6th centuries BC. The hillfort defences were renewed during the Late Iron Age.
Chalbury Hillfort is an Iron Age hillfort about 1 mile (1.6 km) south-east of the village of Bincombe, in Dorset, England. It is a scheduled monument.