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.
Anglo-Saxon architecture was a period in the history of architecture in England from the mid-5th century until the Norman Conquest of 1066. Anglo-Saxon secular buildings in Britain were generally simple, constructed mainly using timber with thatch for roofing. No universally accepted example survives above ground. Generally preferring not to settle within the old Roman cities, the Anglo-Saxons built small towns near their centres of agriculture, at fords in rivers or sited to serve as ports. In each town, a main hall was in the centre, provided with a central hearth.
Wooler is a small town in Northumberland, England. It lies on the edge of the Northumberland National Park, near the Cheviot Hills. It is a popular base for walkers and is referred to as the "Gateway to the Cheviots". As well as many shops and pubs, the town has a youth hostel, many hotels, and campsites. It lies on the St. Cuthbert's Way long-distance footpath between Melrose Abbey and Lindisfarne.
Oldbury Camp is the largest Iron Age hill fort in south-eastern England. It was built in the 1st century BC by Celtic British tribes on a hilltop west of Ightham, Kent, in a strategic location overlooking routes through the Kentish Weald. The fort comprises a bank and ditch enclosing an area of about 50 hectares, with entrances at the north-east and south ends. Wooden gates barred the entrances. Archaeological excavations carried out in the 1930s and 1980s found that the hill fort's interior had probably not been permanently occupied. It had been abandoned around 50 BC and the north-east gate had been burned down, possibly due to a Roman invasion. The wooded southern part of Oldbury Camp is now owned and managed by the National Trust and is open to the public.
The Cheviot is an extinct volcano and the highest summit in the Cheviot Hills and in the county of Northumberland. Located in the extreme north of England, it is a 1+1⁄4 miles walk from the Scottish border and, with a height of 2,674 feet above sea-level, is located on the northernmost few miles of the Pennine Way, before the descent into Kirk Yetholm.
St Cuthbert's Way is a 100-kilometre (62 mi) long-distance trail between the Scottish Borders town of Melrose and Lindisfarne off the coast of Northumberland, England. The walk is named after Cuthbert, a 7th-century saint, a native of the Borders who spent his life in the service of the church. The route links Melrose Abbey, where Cuthbert began his religious life, with his initial burial place on Holy Island. Cuthbert achieved the status of bishop, and was called a saint eleven years after his death, when his coffin was opened and his remains found to be perfectly preserved.
The River Glen is a seven mile long tributary of the River Till flowing through Northumberland, England. The College Burn and Bowmont Water, both flowing out of the Cheviot Hills, meet near Kirknewton to form the River Glen. The Glen flows past the small settlements of Yeavering, Lanton, Coupland, Akeld and Ewart, before joining the Till.
Akeld is a village and civil parish in Northumberland, England. It is situated around 2.7 miles (4.3 km) to the west of Wooler and 9.3 miles (15.0 km) from the border with Scotland at Coldstream. The village lies on the northern limit of Northumberland National Park and on the foot of the Cheviot Hills massif. It is overlooked by Akeld Hill and Harehope Hill to the south. In 2001 Akeld had a population of 82, increasing at the 2011 Census to 221, although this was partly due to the parish merging with that of Kirknewton. The burn which runs through the village and down to the Milfield Basin also bears the name Akeld.
Alnham is a hamlet and civil parish in Northumberland, England. It is about 14 miles (23 km) west of Alnwick, about 6 miles (9.7 km) from Scotland and is located on the south of a small tributary of the River Aln. The village stands on uneven ground, sloping from south to north, at the foot of the southern outliers of the Cheviot Hills. The River Aln flows eastward through the village from its source in the Cheviot Hills down to the coast. The layout of the village appears to have been dictated by the river. The estimated population taken at the 2011 Census was around 245.
The Grianan of Aileach, sometimes anglicised as Greenan Ely or Greenan Fort, is a hillfort atop the 244 metres (801 ft) high Greenan Mountain at Inishowen in County Donegal, Ireland. The main structure is a stone ringfort, thought to have been built by the Northern Uí Néill, in the sixth or seventh century CE; although there is evidence that the site had been in use before the fort was built. It has been identified as the seat of the Kingdom of Ailech and one of the royal sites of Gaelic Ireland. The wall is about 4.5 metres (15 ft) thick and 5 metres (16 ft) high. Inside it has three terraces, which are linked by steps, and two long passages within it. Originally, there would have been buildings inside the ringfort. Just outside it are the remains of a well and a tumulus.
Yeavering is a hamlet in the north-east corner of the civil parish of Kirknewton in the English county of Northumberland. It is located on the River Glen at the northern edge of the Cheviot Hills. It is noteworthy as the site of a large Anglo-Saxon period settlement that archaeologists have interpreted as being one of the seats of royal power held by the kings of Bernicia in the 7th century CE.
Humbleton Hill is a hill in Northumberland, England, about 1.5 miles (2.4 km) west of Wooler.
Castercliff is an Iron Age multivallate hillfort situated close to the towns of Nelson and Colne in Lancashire, Northern England.
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.
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.
The Cheviot Hills, or sometimes The Cheviots, are a range of uplands straddling the Anglo-Scottish border between Northumberland and the Scottish Borders. The English section is within the Northumberland National Park. The range includes The Cheviot, plus Hedgehope Hill to the east, Windy Gyle to the west, and Cushat Law and Bloodybush Edge to the south.
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.
Kilham is a hamlet and civil parish in the English county of Northumberland, located 8.0 miles (12.9 km) west of Wooler, 12.0 miles (19.3 km) east of Kelso, 17.0 miles (27.4 km) south west of Berwick-upon-Tweed and 38.9 miles (62.6 km) north west of Morpeth. It lies on the northern edge of the Northumberland National Park in Bowmont Valley Northumberland. The hamlet, which consists of a small group of agricultural dwellings, is overlooked by Kilham Hill and the northern limits of the Cheviot Hills. The parish had a population of 131 in 2001, and includes the hamlets of Howtel and Pawston, along with the former upland township of Coldsmouth and Thompson's Walls. falling to less than 100 at the 2011 Census. Details are now included in the parish of Branxton
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.
Castle Knowe, also known as Clinch Castle, is the site of an Iron Age hillfort in Northumberland, England, about 1 mile south-east of the village of Ingram. It is a scheduled monument.
Steep northern slopes of Yeavering Bell
View north-northeast from Yeavering Bell
North-east slope seen from near to White Law
Summit cairn
Summit
Summit
Hill fort
Sheepfold below Yeavering Bell
