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.
Badbury Rings is an Iron Age hill fort and Scheduled Monument in east Dorset, England. It was in the territory of the Durotriges. In the Roman era a temple was located immediately west of the fort, and there was a Romano-British town known as Vindocladia a short distance to the south-west.
Butser Hill is a hill and nature reserve in Hampshire, England. South-west of Petersfield, it is a 239.7-hectare (592-acre) biological and geological Site of Special Scientific Interest. It is a national nature reserve and a Special Area of Conservation. Part of it is a Geological Conservation Review site and an area of 84.8 hectares is Oxenbourne Down, which is designated a Local Nature Reserve. Part of it is a Scheduled Monument.
Beacon Hill is near the village of Burghclere and Watership Down, in north Hampshire. The hill's name is derived from the fact that it was one of many Beacon Hills in England and beyond. This hill was once the site of the most famous beacon in Hampshire. It is 261 metres high and has one of England's most well known hill forts on its slopes, visible from the main A34 road which passes close by. From there, outstanding views of the surrounding area and much of Hampshire may be obtained. The site is open to the public and managed by Hampshire County Council. It is an 80.7-hectare (199-acre) biological Site of Special Scientific Interest called Burghclere Beacon and a Nature Conservation Review site, Grade I.
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.
Old Winchester Hill is a 66.2-hectare (164-acre) biological Site of Special Scientific Interest in Hampshire. It is a Nature Conservation Review site, Grade I, and a national nature reserve. Part of it is a scheduled monument.
Fleam Dyke is a linear earthwork between Fulbourn and Balsham in Cambridgeshire, initiated at some timepoint between AD 330 and AD 510. It is three miles long and seven metres high from ditch to bank, and its ditch faces westwards, implying invading Saxons as its architects. Later, it formed a boundary of the late Anglo-Saxon administrative division of Flendish Hundred. At a prominent point, the earthwork runs beside Mutlow Hill, crowned by a 4000-year-old Bronze Age burial mound. The entire length is now a Scheduled Monument and a 7.8 hectare biological Site of Special Scientific Interest.
Caesar's Camp is an Iron Age hill fort around 2400 years old. It is located just in Crowthorne civil parish to the south of Bracknell in the English county of Berkshire. It falls within the Windsor Forest and is well wooded, although parts of the fort have now been cleared of some trees. The area is managed by the Forestry Commission but owned by Crown Estate, and is open and accessible to the public. The hill fort covers an area of about 17.2 acres and is surrounded by a mile-long ditch, making it one of the largest in southern England.
Mellor hill fort is a prehistoric site in North West England, that dates from the British Iron Age—about 800 BC to 100 AD. Situated on a hill in Mellor, Greater Manchester, on the western edge of the Peak District, the hill fort overlooks the Cheshire Plain. Although the settlement was founded during the Iron Age, evidence exists of activity on the site as far back as 8,000 BC; during the Bronze Age the hill may have been an area where funerary practices were performed. Artefacts such as a Bronze Age amber necklace indicate the site was high status and that its residents took part in long-distance trade. The settlement was occupied into the Roman period. After the site was abandoned, probably in the 4th century, it was forgotten until its rediscovery in the 1990s.
Black Ditches is an earthwork close to the village of Cavenham of Suffolk, and part of it is a biological Site of Special Scientific Interest (SSSI). The earthwork is 4.5 miles long between the River Lark at Lackford and the Icknield Way. It is described by the Suffolk Historic Environment Record as having no direct dating evidence but "by analogy with other linear earthworks in the region it is usually assumed to be post Roman".
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.
Bury Hill is the site of a former Iron Age hillfort about 1.5 miles (2.4 km) southwest of the centre of Andover, Hampshire. The site encloses about 22 acres (8.9 ha). There are evident two stages to the construction of the fort, the first is a low single rampart and ditch, to the north and west of the second, stronger double rampart and ditch earthworks, part of which overlies the earlier work. The banks and the ditch are apparently in good condition, although fairly heavily wooded. A footpath encircles the hill fort on the inner rampart, accessible from the northeast and southwest. The centre is left to grass and very secluded, but is not accessible to the general public. The site was used well into the Roman era and was used as a camp by King Canute in 1016, when he fought Edmund Ironside in the Battle of Andover.
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.
Norsebury Ring is the site of an Iron Age univallate hillfort located in Hampshire. Now mostly ploughed out to the South and east, some ditches and ramparts remain within a small copsed area to the North and west, which are surprisingly intact with a small outer ditch, then a bank, then another larger ditch followed by larger bank. However the trees and undergrowth hide the earthworks from immediate view.
Whitsbury Castle, or Whitsbury Castle Ditches, is the site of an Iron Age univallate hillfort located near the village of Whitsbury in Hampshire. The fort is roughly pear-shaped, located on a chalk outcrop, and covering approximately sixteen acres. The defenses comprise two large ramparts with outer ditches and an additional counter scarp bank on the northern half. The original entrance was at the southwestern corner but has been destroyed by the construction of a post-medieval manor house. The site has been in use throughout the ages, with excavation revealing mesolithic activity, an association with a Bronze Age ranch boundary, an Iron Age hillfort settlement, followed much later by Anglo-Saxon renovation and reuse of the defences. The site is privately owned but is flanked externally on all sides but east by public bridleways.
Woolbury, or Woolbury Ring, is the site of an Iron Age univallate hill fort on Stockbridge Down, Hampshire, England.
Bussock Camp is the site of an Iron Age bivallate hillfort located in Berkshire, England. It has a double bank and ditch to the south and east, with only a single bank remaining the north and western sides. The entrance is to the north of the site and is believed to be original, and the site encloses approximately 11 acres.
Battlesbury Camp is the site of an Iron Age bivallate hill fort on Battlesbury Hill near the town of Warminster in Wiltshire, South West England. Excavations and surveys at the site have uncovered various finds and archaeological evidence.
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.
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.
