Nov 23
Boltby is a very important ancient site IMO. A gold “hair braid”, was found there, linking it to the Amesbury Archer, buried with two similar hair braids. This also provides a link to the founding of Stonehenge, which helps set a potential scene for a possible “zeitgeist”, of the day.
Swaledale occupies the long, sinuous valley carved by the River Swale on its 45-kilometre descent from Nine Standards Rigg (662 m) on the Pennine watershed to Richmond in lower Teesdale. The dale narrows between rough gritstone scarps near Keld, broadens to a patchwork of hay-meadows around Muker and Gunnerside, then opens into a tree-fringed flood-plain west of Reeth before the river cuts through the Carboniferous escarpment to meet the Vale of Mowbray.
This head is one of thirteen “Celtic”, or archaic heads that are located within the interior of the church. Twelve of those heads, including this one, are located in four rows of three, which run down either side of the churches arched columns. The thirteenth head is located in the bell tower.
The stats for this Neolithic monument are astounding: 200m across, once a great circle of earthen banks and deep ditches. Today, almost lost: 5,000 years of plough and neglect have flattened the banks and filled the ditches, and Cana Henge is now nothing but a smoothly undulating grassy field on the moor overlooking Ripon.
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.
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
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