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.

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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.

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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.

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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.’

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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.

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

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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.

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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

Burning Moors

I took a walk onto Danby Low Moor to have a look around the old silica rock quarries. The quarries were active from the late nineteenth century until the mid twentieth century.

The stone was transported from the moor via an incline to a crushing plant in Castleton. The silica-rich stone was used in the manufacture of refractory bricks and foundry moulding sand.

Keepers across the moors were taking advantage of the light southerly winds, I could see the smoke from at least half a dozen moorland fires. As the day progressed more fires were lit. Smoke was blowing from the high moors into the Esk valley via Westerdale and Danby Dale.

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Looking eastwards along Eskdale , a low bar of smoke could be seen running along the coast where the light onshore winds met the stronger offshore wind, pushing the smoke northwards along the coastline

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The smoke from the northern moor tops gradually made its way to the escarpment edge and could be seen dropping down into the Tees valley and East Cleveland. If you were beneath the escarpment you probably wouldn’t notice the smoke, however, it was quite visible from above.

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The periodic burning of the moorlands is a controversial issue with arguments for and against, there is no doubt that it is a destructive process and can have a detrimental effect on the delicate ecosystems of the upland moors and bogs.

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What isn’t often discussed are the human health effects of these burnings. In an attempt to cut pollution and improve air quality, the government is currently legislating to reduce emmisions from all sectors of society but I can’t find any reference to the burning of moorland in the Government’s Clean Air Strategy

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In many ways, the grouse shooting industry seems to be untouched by the modern world. It occurs to me that with the current pandemic, many people are experiencing breathing difficulties, any increase in atmospheric pollutants is not a good thing, especially for those who live in the moorland dales.

Smoke is defined as the gaseous products of burning materials especially of organic origin made visible by the presence of small particles of carbon

It is unlawful to cause emission of smoke which is prejudicial to health or causes a nuisance. [Section 79 of the Environmental Protection Act 1990] The Heather & Grass Burning Code

Easington High Moor

Slack –  a shallow valley

Swang – a boggy or marshy area

Beck – a small stream

Rigg – a ridge

Bield – a sheep shelter

Easington High Moor, Roxby High Moor and Black Dike Moor form one of my favourite places on the North York Moors. They are an expanse of heather moorland, wetland and grassy moorland. It is difficult to say where one moor finishes and another starts, the boundaries are loosely defined by the Slacks and Riggs.

I follow the old peat road that runs beside the ancient barrow of Sail Howe. Beside the track are a couple of  large, unnamed, boundary stones.

Wooden shooting stands march along the edge of the slack. Heather has been machine- cut in a number areas of the moor such as the one above defining the boundary of an area of burning.  A days grouse shooting on the moor in August and September will set you back £23,250. This includes a mid morning snack and lunch f or a party of 8 guns. source

I pass one of the two Good Goose Thorne boundary stones that can be found on the moor. The beautifully mason-lettered stone stands beside it’s ancient predecessor.  The path leads me across a section of Black Dike Moor marked as Horse Flesh on the old OS maps. I then drop down to the stepping stones across Black Dike Slack and walk up onto Temple Beeld Hill.

Temple Beeld Hill, is barely a hill. On the higher ground is Temple Beeld itself. The North York Moors has many wonderful sites, what ever its origins, this one is definitely worth a visit.

Frank Elgee’s account and sketch plan of Temple Beeld

.. the most remarkable stones known to me occur on Temple Beald Hill on Black Dyke Moor, north of the village of Lealholm. Here, on a slight elevation between two boggy valleys, a quincunx arrangement of ancient menhirs has been converted into a cross- shaped beald or sheep shelter, shown on the annexed diagram. Originally, the site appears to have been occupied by five stones which are from four to five feet high ; those at C, D and in the centre, being thin and flat, and roughly shaped, whilst the two remaining stones at A and B are more regular and rectangular in form. High stone walls at a later period have been built between the ancient stones ; the wall from A to B is straight, and about thirty-five yards long ; and the wall from C to D decidedly curved and about twenty-two yards in length. This arrangement of the walls gives ample shelter to the moor sheep, and at one time the centre was partly roofed in — the timbers of an old thatch still lie in an irregular manner across the central angles. That the five stones are of pre-historic origin is highly probable, seeing that the central one has distinct cup-like markings at the top of the only side visible. The name Temple, too, is suggestive of some ancient circle of stones, for whatever purpose constructed. It may also be remarked that the four stones are not built into the ends of the walls, but stand off a few inches in distinct hollows in the ground. Temple Beald is the simplest type of stone circle upon the moors, where they are far from common.

Isn’t Quincunx a wonderful word?

In his 1987 book, Standing Stones and Earthworks on the North York Moors, Stanhope White describes how he surveyed Temple Beeld and sent the results to the Royal Observatory to ascertain whether the site had any astronomical alignments, none were found.

I’m sceptical regarding the Prehistoric origins of Temple Beeld as a monument. Three of the large standing may have been erected in prehistory but I suspect they may have been re-used and possibly relocated to create the sheep shelter around a central earth-fast stone. The cup-like marks that Elgee mentions appear to be the result of natural weathering. That said, I hope that one day someone proves me wrong because I love this place.

‘Noble ruins stand only where virgin stone is plentiful’

On my return I call in on the Nan Stone located on the edge of Hardale Slack above the Roxby Peat Holes.  The stone has its name carved into it, faded but still legible. As with the Good Goose Thorn, the stone stands beside an earth fast boulder. The older stone has a cross carved into it. I have seen this on other moorland stones, I have also seen these crosses explained as the ‘christianisation’ of an ancient pagan stone. I suspect that the explanation is far simpler and involves the marking of the stone to identify it as a boundary stone. I am planning to write a blog post soon exploring these boundary stones and their meaning.

These three moors are a place that I am constantly revisiting, over the years I have learned much about the North York Moors by walking their tracks and revisiting their sites. A first glance these Moors may appear to be a featureless places, set foot on them and you’ll soon learn that this is not the case.

Sources

The Moorlands of North-Eastern Yorkshire – Frank Elgee. 1912

Standing Stones and Earthworks on the North York Moors – Stanhope White. 1987