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
Category: Brigantia
Great Roe Wood (Roe Wood) Enclosure – Woodhouse
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.
Dryburn Henge, Cumbria
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.
Black Dike – Coverdale
Black Dike is the diminutive counterpart to the great Tor Dike, rising from its western arm and climbing to the watershed between Great and Little Whernside. Beginning at roughly SD 988 756—where Tor Dike cleaves the limestone scarp—the Black Dike pursues a steep, sinuous course uphill for nearly 0.6 km, finally spilling onto the ridge crest at about 675 m above sea level