Panel aliases: Horseshoe Rock

Notes about name:

 
The name 'Lordenshaw' (also Lordinshaw) is not clear in its origin, but may come from heavy (Old French lourdin) ridge (Old English hou, which occurs as 'hoe', as in Prudhoe or Swinhoe, for example). The other meaning of 'shaw' is a wood. If the first derivation is correct it means that the ridge was unproductive, for 'heavy' was used as a term of complaint.

Current location: Countryside

Parish: Tosson CP, Alnwick, Northumberland, England   

Panel type:

• Burial Cairn

Legal status: Private

Nature of access: Open Access

Wheelchair access: Impossible

General notes:

 
North along the same ridge from West Lordenshaw (Birky Hill 1a-c), commanding views like the others across the Whitton Burn right through to the Cheviot Hills and the Coquet valley, with Simonside close by, is the ‘Horseshoe Rock', named many years ago. This outcrop block protrudes from a grass-covered cairn that may be a burial mound.

General introduction to Lordenshaw:

The sandstone promontory on which Lordenshaw stands is to the north east of the Simonside --Dove Crags range of hills. Its north west and south east flanks drop respectively to Whitton Dean, a tributary of the Coquet and to a narrow glaciated valley overlooked to the east by another outlying sandstone hill that rises to the same height as Lordenshaw. There is a rise to the hillfort from the south west, then the land slopes away to the north east, finger-like, to the Whitton Burn.

This raised, prominent extension of the Simonside Hills reaches 268m.OD, and is made up of outcrop Fell sandstone, with only a thin layer of acidic soil. There are patches of bright orange soil thrown up by rabbits, and a dark grey soil elsewhere.

The whole area has archaeology of many different periods, one of the most recent and most significant being the clearance of much of the land to the east for ‘improvement' for the growing of grain on a regular close-running rig and furrow system. This must have destroyed some surface archaeology, and may have resulted in some of the stone heaps that could also be prehistoric burial mounds.

Prominent on the hilltop is a ‘fort', a ditched Iron Age enclosure that has been re-used as a Romano-British settlement. The slope southwards to the modern road and car park has many field walls, some of cobble and soil construction, and others of vertically--set sandstones. Some of these walls cross one another, and represent different episodes in the use of the land.

The oldest features belong to the late Neolithic period, represented by cup and ring marked rocks over a wide area. The motifs vary from simple cups to more complex ringed cups and grooves, but there is a characteristic regional phenomenon of long grooves or channels that follow the slope of the outcrop sheets on the east side of the hill.

It is impossible to date outcrop markings, but in this area three possible early bronze age cairns have been built on marked outcrop rock, showing that the latter are either contemporary or earlier, and also showing that the sites were already of great importance in the landscape before the cairns were added.

All the marked rocks in situ are at prominent viewpoints, some commanding many miles of territory. A few cupped rocks in the hillfort allow the possibility that some marked surfaces may have been destroyed during its construction, and the medieval Deer Park wall may account for others being broken up and reused.
Modern quarrying has certainly taken its toll, especially on the north west, where masses of freestone have been removed, leaving holes in the ground like bomb craters, and the main block of rock art (2c) bears every sign of the quarrying process. Add to that a network of other walls, including those for sheilings (temporary herds' houses and gardens), and it is likely that we have lost a large proportion of rock art.
 

Motifs:  

Art description:

The motifs include a double groove enclosing many cups, some linked, and this groove becomes single, culminating in a cup and penannular. There are cups along the top in a line, and a linear groove. Different from all these are one, two and three--circled cups, two with grooves running from the cups and the other without. Other grooves roughly parallel, run to ground. There are at least two episodes in the marking of this rock, as the cups and rings were put there before the double groove.