Mam Tor is a 517 m (1,696 ft) hill near Castleton in the High Peak of Derbyshire, England. Its name means "mother hill", so called because frequent landslips on its eastern face have resulted in a multitude of "mini-hills" beneath it. These landslips, which are caused by unstable lower layers of shale, also give the hill its alternative name of Shivering Mountain.
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.
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.
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.
Dolebury Warren is a 90.6 hectares 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.
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.
Dundon Hill Hillfort is an Iron Age hillfort in Compton Dundon, Somerset, England. It has been designated as a Scheduled Ancient Monument. South east of the site is a Bronze Age bowl barrow which, it has been suggested, was later modified as a Norman Motte, known as Dundon Beacon.
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.
The Aston Valley Barrow Cemetery, or Ashton Valley Barrow Cemetery, is a group of Bronze Age bowl barrow and bell barrow tumuli on the south facing edge of Codford Down on the west side of the valley of the Chitterne Brook, within the civil parish of Codford, in Wiltshire, England. There were originally ten bowl barrows and a single bell barrow, but some of these have now been ploughed out: only the bell barrow and five bowl barrows survive. The site is a scheduled monument.
Taunton Deane was a local government district with borough status in Somerset, England. It merged with West Somerset to form Somerset West and Taunton on 1 April 2019. Its council was based in Taunton. The district was formed on 1 April 1974, under the Local Government Act 1972, by a merger of the Municipal Borough of Taunton, Wellington Urban District, Taunton Rural District, and Wellington Rural District. Taunton Deane was granted borough status in 1975, enabling the mayoralty of Taunton to be continued, when other districts did not have mayors. The district was given the name of an alternate form of the Taunton Deane Hundred.
Mendip is a local government district of Somerset in England. The Mendip district covers a largely rural area of 285 square miles (738 km2) ranging from the Mendip Hills through on to the Somerset Levels. It has a population of approximately 110,000. The administrative centre of the district is Shepton Mallet but the largest town is Frome.
There are over 670 scheduled monuments in the ceremonial county of Somerset in South West England. The county consists of a non-metropolitan county, administered by Somerset Council. The two administratively independent unitary authorities, which were established on 1 April 1996 following the breakup of the county of Avon, are North Somerset and Bath and North East Somerset. These unitary authorities include areas that were once part of Somerset before the creation of Avon in 1974.
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.
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.
The Wye Valley is the limestone valley of the River Wye in the White Peak of Derbyshire, England. The source of the River Wye is west of Buxton on Axe Edge Moor. One main channel runs underground through Poole's Cavern. The river flows though Buxton Pavilion Gardens and then along a culvert under the town centre. After leaving the flat area of central Buxton, the Wye Valley becomes distinct as a gorge running east for 10 miles (16 km) before the valley broadens at Ashford-in-the Water.
