A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roman period. The fortification usually follows the contours of a hill and consists of one or more lines of earthworks, with stockades or defensive walls, and external ditches. Hillforts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC, and were used in many Celtic areas of central and western Europe until the Roman conquest.
Maiden Castle is an Iron Age hill fort 1.6 miles (2.6 km) south west of Dorchester, in the English county of Dorset. Hill forts were fortified hill-top settlements constructed across Britain during the Iron Age.
Uffington Castle is an early Iron 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 end was apparently blocked up a few centuries after it was built. 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.
Danebury is an Iron Age hill fort in Hampshire, England, about 19 kilometres (12 mi) north-west of Winchester. The site, covering 5 hectares, was excavated by Barry Cunliffe in the 1970s. Danebury is considered a type-site for hill forts, and was important in developing the understanding of hill forts, as very few others have been so intensively excavated.
Dunkery Beacon at the summit of Dunkery Hill is the highest point on Exmoor and in Somerset, England. It is also the highest point in southern England outside of Dartmoor.
Chanctonbury Ring is a prehistoric hill fort atop Chanctonbury Hill on the South Downs, on the border of the civil parishes of Washington and Wiston in the English county of West Sussex. A ridgeway, now part of the South Downs Way, runs along the hill. It forms part of an ensemble of associated historical features created over a span of more than 2,000 years, including round barrows dating from the Bronze Age to the Saxon periods and dykes dating from the Iron Age and Roman periods.
Wincobank is an Iron Age hill fort near Wincobank in Sheffield, England.
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.
Buckland Rings is the site of an Iron Age hill fort in the town of Lymington, Hampshire. Today, the mounds and dykes around the outside which once constituted its defences are still clearly visible, although the outer bank lies under the road on the west side, and on the south-east it is nearly ploughed-out. Excavations of the inner and middle ramparts in 1935 revealed that they were of wall-and-fill construction, retained at the front by upright timber beams and walls of cut and laid turf. The entrance, which lies on the east side, was also excavated revealing a long entrance passage and the postholes for a pair of stout gateposts. The site was bought by Hampshire County Council in 1989 to ensure its preservation, and it is open to the public from the A337 road onto which part of it faces.
Ladle Hill is a 10.5-hectare (26-acre) biological Site of Special Scientific Interest west of Kingsclere in Hampshire. It is also a Scheduled 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 1km 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 located in Wiltshire. 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 southeastern 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.
Ffridd Faldwyn is an Iron Age hillfort in northern Powys, in the former county of Montgomeryshire, It is sited on a prominent hill west of Montgomery, close to but higher than Montgomery Castle, overlooking the River Severn. It is one of the largest hill-forts in Wales.
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.
Caesar's Camp is an Iron Age hill fort straddling the border of the counties of Surrey and Hampshire in southern England. The fort straddles the borough of Waverley in Surrey and the borough of Rushmoor and the district of Hart, both in Hampshire. Caesar's Camp is a Scheduled Ancient Monument with a list entry identification number of 1007895. It lies approximately 3 kilometres (1.9 mi) north of the town of Farnham, and a similar distance west of Aldershot. The hillfort lies entirely within the Bourley and Long Valley Site of Special Scientific Interest. Caesar's Camp is a multivallate hillfort, a fort with multiple defensive rings, occupying an irregular promontory, with an entrance on the south side. The site has been much disturbed by military activity, especially at the southeast corner. The remains of the hillfort are considered to be of national importance.
Warbstow Bury is an Iron Age hillfort about 0.5 miles (0.80 km) west of the village of Warbstow, in Cornwall, England. It is a scheduled monument.
Bury Walls is an Iron Age hillfort about 1 mile (1.6 km) south-east of Weston-under-Redcastle, in Shropshire, England. It is a scheduled monument.
Hollingbury Castle, also known as Hollingbury Camp and Hollingbury Hillfort, is an Iron Age hillfort on the northern edge of Brighton, in East Sussex, England. It is adjacent to Hollingbury Park Golf Course.
Maiden Bower is an Iron Age hillfort near Dunstable in Bedfordshire, England. The site, which also has traces of a Neolithic causewayed enclosure, is a scheduled monument.
