Icknield Street or Ryknild Street is a Roman road in England, with a route roughly south-west to north-east. It runs from the Fosse Way at Bourton on the Water in Gloucestershire to Templeborough in South Yorkshire. It passes through Alcester, Studley, Redditch, Metchley Fort, Birmingham, Sutton Coldfield, Lichfield, Burton upon Trent and Derby.
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.
Bokerley Dyke, Bokerly Dyke, Bokerley Ditch, is a linear earthwork 5.75 kilometres (3.6 mi) long in Hampshire, between Woodyates and Martin. It is a Scheduled Monument.
The Car Dyke was, and to a large extent still is, a long ditch which runs along the western edge of the Fens in eastern England for a distance of over 57 miles (92 km). It is generally accepted as being of Roman age and, for many centuries, to have been taken as marking the western edge of the Fens. The name derives from carr, a fourteenth-century word for marsh or drained land.
Devil's Dyke is the remains of a prehistoric defensive ditch which lies at the east side of the village of Wheathampstead, Hertfordshire, England. It is protected as a Scheduled Monument. It is generally agreed to have been part of the defences of an Iron Age settlement belonging to the Catuvellauni tribe of Ancient Britain. It has possible associations with Julius Caesar's second invasion of Britain
Grim's Ditch, Grim's Dyke or Grim's Bank is a name shared by a number of prehistoric bank and ditch linear earthworks across England. They are of different dates and may have had different functions.
The Pecsætan, also called Peaklanders or Peakrills in modern English, were an Anglo-Saxon tribe who inhabited the central and northern parts of the Peak District area in England.
Hob Hurst's House is a Bronze Age barrow on Beeley Moor near Bakewell in Derbyshire. It is unique in that instead of the normal round shape, Hob Hurst's barrow is rectangular. Originally made with 13 stones, only five remain today.
Stanton Moor is a small upland area in the Derbyshire Peak District of central northern England, lying between Matlock and Bakewell near the villages of Birchover and Stanton-in-Peak. It is known for its megaliths – particularly the Nine Ladies stone circle – and for its natural, wind-eroded sandstone pillars. The Peak District Boundary Walk runs across the moor.
Bradwell is a village and civil parish in the Derbyshire Peak District of England. The population of the civil parish taken at the 2011 Census was 1,416. It lies south of the main body of the Hope Valley but is usually included among its settlements.
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.
The Bull Ring is a Class II henge that was built in the late Neolithic period near Dove Holes in Derbyshire, England.
The Aberford Dykes are a series of archaeological monuments located around the valley of the Cock Beck, where it runs just north of the village of Aberford on the border between North and West Yorkshire, England.
Batham Gate is the medieval name for a Roman road in Derbyshire, England, which ran south-west from Templebrough on the River Don in South Yorkshire to Brough-on-Noe and the spa town of Buxton in Derbyshire. Gate means "road" in northern English dialects; the name therefore means "road to the bath town".
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".
Buckland Rings is the site of an Iron Age hill fort in the town of Lymington, Hampshire. Today, the mounds and dykes around the outside which once constituted its defences are still clearly visible, although the outer bank lies under the road on the west side, and on the south-east it is nearly ploughed-out. Excavations of the inner and middle ramparts in 1935 revealed that they were of wall-and-fill construction, retained at the front by upright timber beams and walls of cut and laid turf. The entrance, which lies on the east side, was also excavated revealing a long entrance passage and the postholes for a pair of stout gateposts. The site was bought by Hampshire County Council in 1989 to ensure its preservation, and it is open to the public from the A337 road onto which part of it faces.
A cross dyke or cross-dyke is a linear earthwork believed to be a prehistoric land boundary that usually measures between 0.2 and 1 kilometre in length. A typical cross dyke consists of one or more ditches running in parallel with one or more raised banks. Univallate cross dykes typically have a flat-bottomed ditch while the ditches of multivallate cross dykes possess a V-shaped cross-section. A defining characteristic of a cross dyke is that it cuts across the width of an upland ridge or the neck of an upland spur. Cross dykes generally occur at altitudes over 150 metres (490 ft) above mean sea level.
Harthill Moor is a small upland area in the Derbyshire Peak District of central and northern England, lying between Matlock and Bakewell near the villages of Birchover and Elton. The moor is within the southern portion of Harthill civil parish. Its highest point is 272 metres (892 ft) above sea level. The River Bradford flows along the northern edge of the moor past Youlgreave and into the River Lathkill at Alport. Harthill Moor is a rich prehistoric landscape with several protected Scheduled Ancient Monuments.
Bradwell Moor is a moorland hill above the village of Bradwell, Derbyshire in the Peak District. The summit is 471 metres (1,545 ft) above sea level.
Scot’s Dyke, also known as the Scots Dyke or the Scots Dike, is a linear earthwork in the district of Richmondshire in the county of North Yorkshire, England. It is about fourteen kilometres long and runs from the river Swale to the river Tees.
