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.
Old Oswestry is a large early Iron Age hill fort in the Welsh Marches near Oswestry in north west Shropshire, England. The earthworks, which remain one of the best preserved hill forts in the UK, have been described as "The Stonehenge of the Iron Age Period". After the hill fort was abandoned, it was incorporated into Wat's Dyke by the Mercians during the Early Medieval period.
Danebury is an Iron Age hillfort 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 hillforts, and was important in developing the understanding of hillforts, as very few others have been so intensively excavated.
Devil's Dyke or Devil's Ditch is a linear earthen barrier, thought to be of Anglo-Saxon origin, in eastern Cambridgeshire and Suffolk. It runs for 11 kilometres (6.8 mi) in an almost straight line from Reach to Woodditton, with a 10-metre-high (33 ft) ditch and bank system facing southwestwards, blocking the open chalkland between the marshy fens to the north and the formerly wooded hills to the south. It is a Scheduled Monument, a biological Site of Special Scientific Interest and a Special Area of Conservation.
Grim's Ditch, Grim's Dyke or Grim's Bank is a name shared by a number of prehistoric bank and ditch linear earthworks across England. They are of different dates and may have had different functions.
Stonea Camp is an Iron Age multivallate hill fort located at Stonea near March in the Cambridgeshire Fens. Situated on a gravel bank just 2 metres above sea-level, it is the lowest hill fort in Britain. Around 500 BC, when fortification is thought to have begun at this site, this "hill" would have provided a significant area of habitable land amidst the flooded marshes of the fens. The site exhibits at least two phases of development over several hundred years of settlement, with a D-shaped set of earth banks surrounded by a larger, more formal set of banks and ditches.
Warham is a village and civil parish in the English county of Norfolk. It is situated about 5 km (3.1 mi) inland from the north Norfolk coast, 5 km (3.1 mi) south-east of the town of Wells-next-the-Sea and 50 km (31 mi) north-west of the city of Norwich.
Dolebury Warren is a 90.6-hectare (224-acre) biological Site of Special Scientific Interest (SSSI) and ancient monument near the villages of Churchill and Rowberrow in North Somerset, part of South West England. It is owned by the National Trust, who acquired the freehold in 1983, and managed by the Avon Wildlife Trust.
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.
Castle Neroche is a Norman motte-and-bailey castle on the site of an earlier hill fort in the parish of Curland, near Staple Fitzpaine, Somerset, England. It is a Scheduled Ancient Monument.
Thetford Castle is a medieval motte and bailey castle in the market town of Thetford in the Breckland area of Norfolk, England. The first castle in Thetford, a probable 11th-century Norman ringwork called Red Castle, was replaced in the 12th century by a much larger motte and bailey castle on the other side of the town. This new castle was largely destroyed in 1173 by Henry II, although the huge motte, the second largest man-made mound in England, remained intact. The motte, recognised as a scheduled monument, now forms part of a local park, and the remains are known variously as Castle Hill, Castle Mound and Military Parade.
Embury Beacon is the site of an Iron Age promontory fort on the west of the Hartland Peninsula, north of Bude and west of Clovelly, in north Devon. The fort has almost entirely been lost to coastal erosion, but a fraction of the eastern ramparts still exist at approximately 150 metres (490 ft) above Sea Level. It is part of the National Trust property of Bideford Bay and Hartland, which also includes two other hill forts at Windbury Head and Bucks Mills earthworks. The site's name suggests it was the location of a beacon, possibly during the Elizabethan period, but there is no archaeological evidence of this.
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.
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.
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.
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 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.
Holkham Camp, or Holkham Fort, is an Iron Age fort in Norfolk, England, about 1 mile (1.6 km) north-west of the village of Holkham. It is a scheduled monument.
Cockthorpe Common, Stiffkey is a 7.1-hectare (18-acre) biological Site of Special Scientific Interest east of Wells-next-the-Sea in Norfolk, England. It is in the Norfolk Coast Area of Outstanding Natural Beauty.
Stiffkey Valley is a 44.4-hectare (110-acre) biological Site of Special Scientific Interest east of Wells-next-the-Sea in Norfolk, England. It is in the Norfolk Coast Area of Outstanding Natural Beauty.
Wells Chalk Pit is a 4-hectare (9.9-acre) biological and geological Site of Special Scientific Interest on the eastern outskirts of Wells-next-the-Sea in Norfolk, England. It is a Geological Conservation Review site, and it is in the Norfolk Coast Area of Outstanding Natural Beauty.
