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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.
A hillfort is a type of earthworks 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.
Wansdyke is a series of early medieval defensive linear earthworks in the West Country of England, consisting of a ditch and a running embankment from the ditch spoil, with the ditching facing north.
Ringforts, ring forts or ring fortresses are circular fortified settlements that were mostly built during the Bronze Age up to about the year 1000. They are found in Northern Europe, especially in Ireland. There are also many in South Wales and in Cornwall, where they are called rounds. Ringforts come in many sizes and may be made of stone or earth. Earthen ringforts would have been marked by a circular rampart, often with a stakewall. Both stone and earthen ringforts would generally have had at least one building inside.
Roath is a district and community to the north-east of the city centre of Cardiff, capital of Wales. There is no community council for the area which is mostly covered by the Plasnewydd electoral ward, and stretches from Adamsdown in the south to Roath Park in the north.
Aidhne, also known as Uí Fhiachrach Aidhni, Mag nAidni, later Maigh Aidhne, was the territory of the Uí Fhiachrach Aidhni, a túath located in the south of what is now County Galway in the south of Connacht, Ireland.. Aidhne is coextensive with the present diocese of Kilmacduagh.
Dubh Artach is a remote skerry of basalt rock off the west coast of Scotland lying 18 miles (29 km) west of Colonsay and 15 miles (24 km) south-west of the Ross of Mull.
Grim's Ditch, Grim's Dyke or Grim's Bank is a name shared by a number of prehistoric bank and ditch earthworks. Enigmatic in both their naming and original function, examples are found across the chalk uplands of southern England.
Elmley Castle was a late 11th-century earthwork and timber castle which received stone additions in the 12th and possibly 13th centuries, located 0.5 miles (0.8 km) south of the village of Elmley Castle and 12 miles (19 km) southeast of the city of Worcester, in Worcestershire. Nothing but the earthworks survive.
Dorsey or Dorsy is a small village and townland between Belleeks and Cullyhanna in County Armagh, Northern Ireland. It has an estimated population of 130-160 people and includes about 30-35 houses.
Kirkmaiden is a parish in the Rinns of Galloway, the most southerly in Scotland; the present Church of Scotland parish has the same name as and is approximately coterminous with the original pre-Reformation parish.
The Black Pig's Dyke or Worm's Ditch is a series of discontinuous linear earthworks in southwest Ulster and northeast Connacht, Ireland. Remnants can be found in north County Leitrim, north County Longford, County Cavan, County Monaghan and County Fermanagh. Sometimes, the Dorsey enclosure in County Armagh and the Dane's Cast in County Down are considered to be part of the dyke.
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.
Gorley Hill is the site of a former Iron Age promontory hillfort located in Hampshire in the United Kingdom.
Scratchbury Camp is the site of an Iron Age univallate hillfort on Scratchbury Hill, overlooking the Wylye valley about 1km 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.
The Knockans is an Iron Age linear earthwork located in south-west Ireland, believed to be the site of the ancient Tailteann Games.
In archaeology, a linear earthwork is a long bank of earth, sometimes with a ditch alongside. There may also be a palisade along the top of the bank. Linear earthworks may have a ditch alongside which provides the source of earth for the bank and an extra obstacle. There may be a single ditch, a ditch on both sides or no ditch at all. Earthworks range in length from a few tens of metres to more than 80 km. Linear earthworks are also known as dykes, or "ranch boundaries".
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.