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.
The River Plym is a river in Devon, England. It runs from Dartmoor in the centre of the county southwest to meet the River Meavy, then south towards Plymouth Sound. The river is popular with canoeists, and the Plym Valley Railway runs alongside a section of the river.
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.
South Hams is a local government district on the south coast of Devon, England. Services divide between those provided by its own Council headquartered in Totnes, and those provided by Devon County Council headquartered in the city of Exeter.
Hambledon Hill is a prehistoric hill fort in Dorset, England, situated in the Blackmore Vale five miles northwest of Blandford Forum. The hill itself is a chalk outcrop, on the southwestern corner of Cranborne Chase, separated from the Dorset Downs by the River Stour. It is owned by the National Trust.
Plympton is a suburb of the city of Plymouth in Devon, England. It is in origin an ancient stannary town. It was an important trading centre for locally mined tin, and a seaport before the River Plym silted up and trade moved down river to Plymouth and was the seat of Plympton Priory the most significant local landholder for many centuries.
Small Down Knoll, or Small Down Camp, is a Bronze Age hill fort near Evercreech in Somerset, England. The hill is on the southern edge of the Mendip Hills, and rises to 222 m (728 ft).
Worlebury Hill is the name given to an upland area lying between the flatlands of Weston-super-Mare and the Kewstoke area of North Somerset, England. Worlebury Hill's rises from sea level to its highest point of 109 metres (358 ft), and the western end of the hill forms a peninsula, jutting out into the Bristol Channel, between Weston Bay and Sand Bay. A toll road follows the coast around the hill from Sand Bay in the north to the now derelict Birnbeck Pier in the west, although tolls are not currently collected on the road. Worlebury Golf Club is situated on the Hill and the area is known for being one of the wealthiest areas in the county of Somerset.
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.
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.
Bury Camp is the site of an Iron Age multivallate hillfort in Wiltshire, England. It occupies a triangular promontory of Colerne Down at the southern edge of the Cotswold Hills between two spurs of a river valley. The enclosed area of approximately 9.2ha is surrounded by a ditch 4m wide and up to 1m deep, and an outer rampart up to 1.5m high on the east and northwestern sides and up to 2m high on the southwestern side, across the neck of the promontory.
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.
Worlebury Camp is the site of an Iron Age hillfort on Worlebury Hill, north of Weston-super-Mare in Somerset, England. The fort was well defended with a numerous walls, embankments and ditches around the site. Several large triangular platforms have been uncovered around the sides of the fort, lower down on the hillside. Nearly one hundred storage pits of various sizes were cut into the bedrock, and many of these had human remains, coins, and other artefacts in them. During the 19th and 20th centuries the fort suffered damage and was threatened with complete destruction on multiple occasions. Now, the site is a designated Scheduled monument. it falls within the Weston Woods Local Nature Reserve which was declared to Natural England by North Somerset Council in 2005.
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.
Membury Camp, or Membury Fort, is the site of an Iron Age hill fort located on the borders of Wiltshire and Berkshire,. The site encompasses 14 acres, and is situated in the south-western corner of a small plateau. The circular earthworks are completely shrouded in trees and inside the walls it is mostly arable farmland. To the northeast, in the Berkshire segment, the camp is totally wooded by a small copse, Walls Copse, which covers a quarter of the site. To the north and east the adjoining ground is flat, but to the south and west it falls away steeply, providing a natural defence. The camp consists of a single ditch with banks on either side and encloses and area measuring 390m by 490m. A gap in the east with inturning flanks is probably an original entrance though it is mutilated and overgrown. Other gaps in the banks appear to be more modern. A possible hut circle is visible as a cropmark situated at the south end of the hill fort. The east side of the earthwork has been partly destroyed by the construction of a wartime airfield, RAF Membury. The site has not been excavated but a number of prehistoric finds have been found in the vicinity. It is a scheduled ancient monument no. 228970 There have been several collections of pottery found, in 1977, 1980 and 1987 Other significant finds have also included for flint artefacts from the mesolithic era, and flint tools from the neolithic era, prior to the Iron Age.
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.
Dudsbury Camp is one of a series of Iron Age earthworks in Dorset, starting from Hambledon Hill, and including Hod Hill, Spetisbury Rings, Buzbury Rings, Badbury Rings and Dudsbury Camp. The Iron Age port at Hengistbury Head forms a final Iron Age monument in this small chain of sites. The fort is located near the village of West Parley.
Plymbridge Woods is a woodland in Plympton, Devon, England managed by The National Trust. The woods are named after the historic Plymbridge, a Grade II listed bridge over the River Plym. Drake's Trail passes through the woods providing a cycling and walking route. There is a range of wildlife, birds and flora.
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.
