The Grey Ditch, near Bradwell in the Peak District is a linear earthwork of post-Roman date. The dyke is built at right angles to the Batham Gate, a Roman road which runs between the Roman fort at Brough in Derbyshire (the Roman name was Navio ) and the Roman settlement at Buxton. When first recorded the length of the Grey Ditch was about 1.7 km long but it now has substantial gaps, caused by ploughing and by development. [1] It currently survives as four sections. The monument runs across the contours and runs along the division between the White Peak and the Dark Peak. The ditch lies on the side towards the northeast. The bank seems to have a single phase while the ditch showed evidence of up to five re-cuts. Importantly the bank lay over a plough soil, which contained sherds of Roman-British pottery. [2] B H O'Neil [3] suggested the Grey Ditch once went as far as the slopes of Mam Tor but there is no firm evidence for this. This area is the boundary between the Pecsaetna (people of the Peak district) and the kingdom of Mercia and the Grey Ditch could be a boundary marker between these groups but again there is no evidence for this.
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.
Arbor Low is a well-preserved Neolithic henge in the Derbyshire Peak District, England. It lies on a Carboniferous Limestone plateau known as the White Peak area. The monument consists of a stone circle surrounded by earthworks and a ditch.
Bokerley Dyke is a linear earthwork 5.75 kilometres (3.6 mi) long in Hampshire, between Woodyates and Martin. It is a Scheduled Monument. It is also spelt Bokerly Dyke.
Ringinglow is a village in the western section of Sheffield, England. It is on the western border of Ecclesall Ward, and although it is within the boundary of Sheffield, it is self-contained, being entirely surrounded by open countryside. The village now falls within the Fulwood ward of the City.
The Car Dyke was, and to a large extent still is, an 85-mile (137 km) long ditch which runs along the western edge of the Fens in eastern England. 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. There, the consensus begins to break down.
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.
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 and 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, sometimes a raised hedgerow and in other places is now no more than a cropmark, the ditch long since 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".
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.
Hazlebadge is a civil parish within the Derbyshire Dales district, in the county of Derbyshire, England. Largely rural, Hazlebadge's population is reported with the population of neighbouring parishes for a total of 427 residents in 2011. It is 143 miles (230 km) north west of London, 29 miles (47 km) north west of the county city of Derby, and 7 miles (11 km) east of the nearest market town of Chapel-en-le-Frith. Hazlebadge is wholly within the Peak District national park, and shares a border with the parishes of Abney and Abney Grange, Bradwell, Brough and Shatton, Great Hucklow as well as Little Hucklow. There are four listed buildings in Hazlebadge.
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.
Coordinates: 53°19′59.38″N1°44′54.76″W / 53.3331611°N 1.7485444°W