Escaping the mad parade

Walking from Farndale up towards Rudland Rigg, we followed the track up the side of Monket Bank. The track climbs up through the old jet workings and quarries along the moor edge.

In the 14th century this route was known as Monckgate and linked Bransdale with Farndale. The track was used as a Church or Corpse Road with coffins being carried over the rigg to Cockan Kirk in Bransdale.

The road across the rigg is now known as Westside Road, in the past, it was known as Waingate, running from Kirkbymoorside Market Place in the south to Battersby Bank in the north.

We cut out across the moor towards Ousegill Head and the Three Howes. Flint tools had been found by the gamekeepers for a number of years so in September 1973 Raymond Hayes and others excavated the area. His small excavation yielded over 800 flints from an area of 3.50 x 3.0m. The site was interpreted as ‘A temporary camping site in a forest clearing, probably being occupied by hunters following red deer or other game.’

Whilst at the Three Howes we saw a Red Kite being harassed by an anxious Curlew. Once the Kite had rid itself of its tormentor it flew directly over us, a joyful moment, this was my first sighting of a Kite on the moors.

We walked back across the old peat workings and rejoined the track, moving on to the waymarker at Cockam Cross and then onto our final goal, the Cammon Stone.

The Cammon Stone is a prehistoric standing stone that sits just beside the main track. The stone is about a metre and a half tall and leans towards the west. I have been visiting this stone on and off for at least two decades, my perception is that the lean of the stone has increased over the years but I may be wrong, I hope I am. The southern views from the stone look down along Bransdale, the axis of the stone is also aligned in this direction, which is probably no coincidence.

There are a number of faded letters carved onto the western face of the stone, in the past, antiquarians had speculated as to whether these letters were Phoenician in origin. They are actually Hebrew and spell out the word halleluiah. They are thought to be the work of the Reverend W Strickland, Vicar of Ingleby. Strickland is thought to be responsible for carving a number of inscriptions in this area.

There is a second stone, a large flat slab. No one knows whether this slab ever stood upright. There is no obvious weathering patterns to indicate that it might have been upstanding but I guess that question could only ever be answered by an archaeological investigation.

We picked our way along a track that ran from the moortop into Farndale and joined the daleside road at Spout House. If you are a fan of stone walls and troughs, you will love this road, it has massive walls with stone-lined gutters and numerous multiple carved stone troughs. The stonemasons and wallers were once kept busy in this area.

Also on this road is the Duffin Stone, a massive boulder that has tumbled down from the escarpment side and is embedded into the verge of the narrow lane. The stone bears the scars of contact with many vehicles.

Etymology

Waingate – OE Waen Way – Waggon Road

Monket – The ‘Mun(e)k(e)’ spellings suggest ‘monks’, but in the absence of monastic associations one might suspect an earlier ‘Mened-cet’ (Welsh Mynydd-coed) – ‘forest hill’. Here one might compare ‘Monket House’ in north-east Yorkshire.

Cammon Stone – Cam Maen – Bank Stone.

Rudland – OE hrycg ON hyrggr ‘ridge’.

Sources

Old Roads & Pannierways in North East Yorkshire. R. H. Hayes.1988. The North York Moors National Park.

Yorkshire Archaeological Journal. Vol.67. 1995. The Yorkshire Archaeological Society.

The Consise Oxford Dictionary of English Place-Names. Eilert Ekwall. 1974. Oxford.

Horn Ridge Dyke

In common with most people I feel as though many aspects of my life have been on hold for the past 12 months. My list of places to visit gets longer and longer. Now that lockdown is easing I seem to have a mental log-jam of what to do and what to see.

I have been planning on visiting the Cross Dyke of Horn Ridge for quite some time as it is one of the few local dykes that I haven’t visited. Once again, it was a chance online conversation with a friend that spurred me into action.

The sun was shining, the forecast was giving out wintery showers, this was perfect for me, half decent weather and less chance of meeting anyone on the moor-top.

I drove down to Farndale and walked up the keepers track that runs up the side of Monket House Crags. The track is not too steep and takes you through an area covered in spoil heaps from the 19th century jet workings. When I started walking the sun was shining, within a few minutes a wintery squall blew in from the north leaving a dusting of snow on the hillside. The squall was intense but short-lived, this became the pattern for the rest of the day.

I followed the track south along the gentle rise of Horn Ridge. From the high point the land begins to gently slope down to the south, the eye is drawn along the valley of the River Dove to the dale end with the moorland above Hutton Le Hole and the Vale of Pickering in the far distance.

As you walk down towards the very obvious earthwork you become very aware that you are on a narrowing promontory of moorland , the fertile dale on either side, hemmed in by the dark domineering presence of Rudland Rigg to the West and Blakey Ridge to the East. As you near the Dyke you can see through the central gap to a fairly level area with the barrow beyond, the effect is quite striking.

The Dyke itself runs the full width of the upland, terminating where the land drops off at either end. Its total length is approximately 300m.

Approaching it from the north it appears to be quite an impressive earthwork fronted by a deep ditch that has been dug along its whole length. When viewed from the south it appears less imposing.

A section of the Dyke was excavated by Raymond H. Hayes. He was unable to find any evidence that might give a date to the earthwork. He observed that with the ditch ‘its builders did not cut the rock as in Iron Age or Roman ditches.’

There are a couple of stone settings within the dyke on the south side but these look relatively recent, a modern shelter or grouse butt and a trap built by keepers to catch small mammals. These moors are not a friendly place for any creature that vaguely threatens the grouse population. Last year 5 dead Buzzards were discovered hidden beneath a rock just 3km north of the Dyke.

Walking south towards the barrow, a squall blows through and the views are lost.

The barrow is a sad sight. It’s quite large, approx 10-15m diameter. It’s hard to fully gauge the dimensions due to it’s in a terrible state of repair of the structure. The scheduling entry for the monument mentions ‘a central excavation hollow around 4m by 2m, with a second 1m diameter pit in its west side.’ The keepers have also recently built a trap into one of the holes in the mound.

I took wander over to the western edge of the ridge. There are reports of cairns and hut circles in this area. I was just starting to spot them when it started to snow quite heavily. My mind turned to driving home and having to tackle the steep bank from the dale bottom up to Blakey Ridge. Under normal circumstances I wouldn’t mind being trapped in Farndale but with the current conditions i.e. the Feversham Arms being closed, I decided that the western edge of Horn Ridge was one for another day and turned for home.

Sources

Google Earth

Heritage Gateway

A History of Helmsley Rievaulx and District. 1963. Editor – J McDonnell

The brides of place: cross ridge boundaries reviewed. – Blaise Vyner. In Moorland Monuments CBA Research Report 101. 1995