Maiden Castle is an Iron Age hill fort 1.6 mi (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.
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.
The Trundle is an Iron Age hillfort on St Roche's Hill about 4 miles (6 km) north of Chichester, West Sussex, England, built on the site of a causewayed enclosure, a form of early Neolithic earthwork found in northwestern Europe. Causewayed enclosures were built in England from shortly before 3700 BC until at least 3500 BC; they are characterized by the full or partial enclosure of an area with ditches that are interrupted by gaps, or causeways. Their purpose is not known; they may have been settlements, meeting places, or ritual sites. Hillforts were built as early as 1000 BC, in the Late Bronze Age, and continued to be built through the Iron Age until shortly before the Roman occupation. A chapel dedicated to St Roche was built on the hill around the end of the 14th century; it was in ruins by 1570. A windmill and a beacon were subsequently built on the hill. The site was occasionally used as a meeting place in the post-medieval period.
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.
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 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.
Cholesbury Camp is a large and well-preserved Iron Age hill fort on the northern edge of the village of Cholesbury in Buckinghamshire, England. It is roughly oval-shaped and covers an area, including ramparts, of 15 acres (6.1 ha), and measures approximately 310 m (1,020 ft) north-east to south-west by 230 m (750 ft) north-west to south-east. The interior is a fairly level plateau which has been in agricultural use since the medieval period. The hill fort is now a scheduled ancient monument.
Bratton Castle is a bivallate Iron Age built hill fort on Bratton Down, at the western edge of the Salisbury Plain escarpment. The hill fort comprises two circuits of ditch and bank which together enclose a pentagonal area of 9.3 hectares.
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.
Trevelgue Head, also known as Porth Island, is a headland north-east of Newquay, Cornwall, England, next to Porth at the eastern end of Newquay Bay.
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.
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.
Thundersbarrow Hill is an archaeological site in West Sussex, England. It is on a chalk ridge, aligned north-west to south-east, on the South Downs north of Shoreham-by-Sea.
South Weald Camp was a hillfort based in South Weald, Brentwood, Essex, England. Roughly circular in plan, the fort covered 2.8 hectares, with a suggested construction date in the late Iron Age, from the 1st century BC to the 1st century AD. The location is associated in this period with the Catuvellauni and the Trinovantes.
Wor Barrow is a Neolithic long barrow on Cranborne Chase, about 1 mile (1.6 km) east of Sixpenny Handley in Dorset, England. It is a scheduled monument.
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.
