Offa's Dyke is a large linear earthwork that roughly follows the border between England and Wales. The structure is named after Offa, the Anglo-Saxon king of Mercia from AD 757 until 796, who is traditionally believed to have ordered its construction. Although its precise original purpose is debated, it delineated the border between Anglian Mercia and the Welsh kingdom of Powys.
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.
Liddington Castle, locally called Liddington Camp, is a late Bronze Age and early Iron Age univallate hillfort in Liddington parish in the English county of Wiltshire, and a scheduled monument.
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.
Trendle Ring is a late prehistoric earthwork on the Quantock Hills near Bicknoller in Somerset, England. It is a Scheduled Monument. In 2013 it was added to the Heritage at Risk Register due to vulnerability to plant growth.
Wat's Dyke is a 40-mile (64 km) linear earthwork running through the northern Welsh Marches from Basingwerk Abbey on the River Dee estuary, passing east of Oswestry and on to Maesbury in Shropshire, England. It runs generally parallel to Offa's Dyke, sometimes within a few yards but never more than three miles (5 km) away. It now appears insignificant and is visible in some places as a raised hedgerow and in others no more than a cropmark. The ditch has long since been filled in and the bank ploughed away, but originally it was a considerable construction, considered to be strategically more sophisticated than Offa's Dyke. The date of construction is disputed, ranging from sub-Roman to the early ninth century.
Nordy Bank is an Iron Age hill fort on Brown Clee Hill in the Shropshire Hills Area of Outstanding Natural Beauty in South Shropshire, England.
Maiden Castle is an Iron Age hill fort, one of many fortified hill-top settlements constructed across Britain during the Iron Age, but one of only seven in the county of Cheshire in northern England. The hill fort was probably occupied from its construction in 600 BC until the Roman conquest of Britain in the 1st century AD. At this time the Cornovii tribe are recorded to have occupied parts of the surrounding area but, because they left no distinctive pottery or metalworking, their occupation has not been verified. Since then it has been quarried and used for military exercises. It is protected as a Scheduled Ancient Monument, and is owned by the National Trust. The hill fort is open to visitors, but unrestricted access to the site has resulted in it being classified as "at high risk" from erosion.
Burrough Hill is an Iron Age hillfort in Burrough on the Hill, 7 miles (11 km) south of Melton Mowbray in the English county of Leicestershire. Situated on a promontory about 210 metres (690 ft) above sea level, the site commands views over the surrounding countryside for miles around. There has been human activity in the area since at least the Mesolithic, and the hillfort was founded in the early Iron Age. In the medieval period, after the hillfort was abandoned, the hill was used as farmland. This ended in the 17th century when the parish the hill was in was enclosed. Traces of ridge and furrow show where the medieval fields were ploughed. Since the 1930s the site has been the subject of archaeological investigations and renewed excavations under the auspices of the University of Leicester began in 2010. Part of Burrough Hill Country Park and open to the public, the hillfort is protected as a Scheduled Ancient Monument.
Kelsborrow Castle is an Iron Age hill fort in Cheshire, northern England. Hill forts were fortified hill-top settlements constructed across Britain during the Iron Age. It is one of only seven hill forts in the county of Cheshire and was probably in use for only a short time. In the 19th century, a bronze palstave was recovered from the site. It is protected as a Scheduled Ancient Monument.
Eddisbury hill fort, also known as Castle Ditch, is an Iron Age hill fort near Delamere, Cheshire, in northern England. Hill forts are fortified hill-top settlements constructed across Britain during the Iron Age. Eddisbury is the largest and most complex of the seven hill forts in the county of Cheshire. It was constructed before 200–100 BC and expanded in 1–50 AD. In the 1st century AD, the Romans slighted the site. It was reoccupied in the 6th–8th centuries AD, and an Anglo-Saxon burh was probably established at Eddisbury in 914. In the medieval and post-medieval periods quarrying and farming have damaged the site. Ownership is currently split between the Forestry Commission and a local farm. Eddisbury is protected as a Scheduled Ancient Monument.
Oakmere hill fort is an Iron Age hill fort, one of many large fortified settlements constructed across Britain during the Iron Age, but one of only seven in the county of Cheshire in northern England. It is protected as a Scheduled Ancient Monument. Despite being a low-lying site, Oakmere is still considered a hill fort.
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 in Wiltshire, England. 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 south-eastern 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.
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.
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.
Ffridd Faldwyn is an Iron Age hillfort in northern Powys, in the former county of Montgomeryshire, It is sited on a prominent hill west of Montgomery, close to but higher than Montgomery Castle, overlooking the River Severn. It is one of the largest hill-forts in Wales.
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.
William Jones Varley, FSA (1904–1976) was a British geographer and archaeologist, particularly known for his excavations of English Iron Age hillforts, including Maiden Castle and Eddisbury hillfort in Cheshire, Old Oswestry hillfort in Shropshire, and Castle Hill in West Yorkshire. He was also a pioneer of geographical research and education in colonial Ghana where he worked from 1947 to 1956, and was involved in historical conservation there.
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.
