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.
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
Tor Dyke appears to have been attributed to Venutius which dates it of the period AD 52 – 70. The presence of a legionary size marching camp a few miles to the southwest at Malham certainly indicates an active role in the Roman advance of AD 70. However, given the lack of published research so far a clear picture has yet to emerge.
Jun 27
A gazetteer of probable prehistoric mounds, cairns and boundary earthworks in Coverdale. It is not complete and is still being researched.
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.
Jun 15
On every late-Victorian and early-20th-century OS sheet the surveyors marked any conspicuous heap of stones they could not instantly classify as a tumulus, beacon, trig-point or boundary stone with the catch-all term “Pile of Stones.”
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
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