Templeborough Roman Fort occupies a commanding position on the north bank of the River Don at Rotherham (OS grid SK 410 916), where the Magnesian Limestone ridge drops into the floodplain. Originally constructed in timber and earth in the mid–1st century AD, it was later rebuilt in stone and occupied—possibly intermittently—until the withdrawal of Roman authority in the early 5th century AD
Great Roe Wood (often simply called “Roe Wood”) sits on the Magnesian Limestone ridge that carries the Roman Rig between Sheffield and Doncaster, just northeast of the village of Woodhouse (OS grid SK 450 920). This ridge forms a natural corridor overlooking the Don valley, with shallow soils over limestone giving way to deeper alluvial gravels in the valley bottom.
Camp Green (often called “Danes Camp”) crowns a limestone-capped knoll immediately north-east of St Michael’s Church in Hathersage (OS grid SK 234 819). Perched above the Hope Valley, it commands wide views down the River Derwent corridor and sits at the transition between the Millstone Grit plateaux to the north and the lower limestone and sandstone vale to the south
This is an oval fort with an internal area of 2.5 acres. A bank, ditch and counterscarp bank are continuous around it except on the N side where ditch and counterscarp have been destroyed.
Scholes (or Scoles) Coppice Camp (sometimes called “Caesar’s Camp”) lies just north-west of Kimberworth in Rotherham, atop the same Magnesian Limestone ridge that carries the Roman Rig. Its grid reference is roughly SE 436 937, placing it only 200–300 m to the north of the Rig’s northern branch
The Roman Rig is a defensive dyke built to defend against attack from the south. It runs from Sheffield, past Templeborough and carries on almost to Doncaster. If this is a Brigantian dyke it would certainly add weight to Websters definition of the Roman border in the period.
Dryburn Henge lies on Alston Moor in Cumbria, within the North Pennines Area of Outstanding Natural Beauty. It occupies a strategic nodal point on the high moor, roughly at NY 760 430, where routes across the Pennine watershed converge. The surrounding terrain is underlain by Carboniferous Great Scar Limestone and interbedded Yoredale shales, with scattered fluvioglacial gravels in valley bottoms.
This mound is 22ft. in diam. and about 3ft high. It has been built upon a natural knoll which makes the barrow look larger than it is. Excavation showed that the mound has an earthy core with a rubble capping.
This unexcavated and undated barrow matches many of other Late Neolithic / Early Bronze-Age round barrows (c. 2400–1500 BC) dotted along the flanks of the Yorkshire Dales.
The Cleave dyke system is several Dykes which combine to create a boundary of between 9 and 18 kilometres running north south to the west of Thirsk.
