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
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.
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.
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.
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.
Jun 16
Over the last five years Iron-Age specialists have been re-examining what British hillforts were really for. The question is no longer just “fortress or farm?” but whether many of them were built first and foremost as places of gathering, display and ritual.
Bishopdale lies within the northern limb of the Askrigg Block, its underlying bedrock dominated by Carboniferous limestones with intermittent shales and sandstones of the Yoredale Series. The Great Scar Limestone, a thick, massive unit formed around 330 million years ago in a shallow tropical sea, underpins the dale’s steeper scarps and cliff lines, while the thinner-bedded limestones and intervening mudstones of the Yoredale Group create the characteristic terraced flanks on which many of Bishopdale’s field systems are laid out
The Kilburn White Horse is a large chalk hill figure cut into the limestone of Roulston Scar, the steep escarpment that defines the western edge of the Hambleton Hills in North Yorkshire. Carved in November 1857 and measuring roughly 97 by 67 metres, it was conceived not as an ancient relic but as a deliberate Victorian creation
The Hill Figures of the British Isles Hill figures are large geoglyphs cut into Britain’s chalk and limestone hillsides, their bright-white forms visible for miles across the landscape. They range from abstract Bronze‐Age symbols to concrete horses and even regimental badges of the 20th century, each marking different moments when local communities, landowners or military …
Castle dykes it is a small class one henge, 90m across, perched on the high ground up in the North Yorkshire dales. The bank survives up to 1.5 m high in places, and the ditch up to 3 m deep. Early 20th-century reports (1908) noted its intact form, and recent LiDAR-based surveys have confirmed its classic henge profile with minimal later disturbance.
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