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.

Some moorland stones

I took a trip over to Glaisdale to visit one on my favourite North York Moors standing stones. This rarely visited, tall, beautiful stone is one of a pair of upright stones located on Glaisdale Swang

Swang – a boggy stretch of land.

When I arrive at the stone I’m confronted by an anxious pheasant hen who starts running in circles around me, a tactic designed to distract me while her brood of chicks scatter for the shelter of the nearby heather.

I can see another stone on the moor edge in the distance, I know that this will probably be a guide stone but probably isn’t good enough, I head for the higher ground. The ground is marshy, so I zig zag my way up the narrowing valley following the lush green carpet of bilberry which tends to grow on the better drained ground. Curlews and lapwings rise in alarm and noisily track my progress as I move from one birds territory to another. Towards the top of the swang, a large hare breaks cover.

As I move onto the high moor guide stones mark the track. Many of these stones date to the 18th century, others may possibly be far older. On October 2nd, 1711, the Justices sitting at Northallerton ordered that guide posts should be erected throughout the North Riding.

A solitary pine tree on the moor top, its branches indicate the direction of the prevailing winds.

Walking across across the high moor towards Glaisdale I encounter a couple of low standing stones one of which is close to a low mound. These stones are not on the track and are too small to be guide stones. Another group of large stones look as through they were once standing but it is difficult to say much more about them.

This guide stone was carved and erected by Thomas Harwood about 1735. Harwood erected four other similar stones on Glaisdale Rigg. The stone appears to be housed in an old cross base. It is possible to make out the inscriptions on the north and east faces, they read Gisbrogh Road and Whitby Road. The other two faces are illegible, Stanhope White writes that the south face reads Glaisdale Road TH.

Walking over to the edge of Glaisdale I find this beautiful orthostatic wall, a real joy. About a century ago many of the original field walls across the moor and dales were rebuilt by professional wallers, this wall may be a survivor of an earlier age.

In his book, Some Reminiscences & Folk Lore of Danby Parish & District, Joseph Ford writes of Stone-Rearing Days. These were occasions when a farmers neighbours gathered together to build walls around newly-enclosed fields. Ford thinks that this tradition may stretch as far back in time to the original settlers of the moorland dales.

D. A. Spratt YAJ 60 1988

Etymology

Glaisdale – YN [Glasedale 12 Guisb. Glasedal 1223, Glasdale 1228 FF] ‘The valley of R Glas’

OW gleis, Welsh glais ‘stream’

Glas is a British river-name derived from the Welsh glas ‘blue, green, grey’

Sources

Yorkshire Wit, Character, Folklore & Customs. R Blakeborough. W Rapp & Sons Ltd. 1911

The North York Moors. An Introduction by Stanhope White. The Dalesman Publishing Co. 1979

Some Reminiscences & Folk Lore of Danby Parish & District. Joseph Ford. M.T.D. Rigg Publications. 1990

The Concise Oxford Dictionary of English Placenames. E Ekwall. 1974

Orthostatic Field Walls on the North York Moors. D.A. Spratt. Yorkshire Archaeological Journal No. 60 1988

Near Moor

Wandering Red Way onto Near Moor

Near Moor is a moor on the western margins of the Cleveland Hills. The moor is at its highest in the north-east where it meets the wooded escarpment edge of the Cleveland hills, it then slopes gently southwards towards Crabdale. Near moor is bounded by Far Moor To the East, Pamperdale Moor to the South and the valley of Scarth Nick and Scarth Wood Moor to the west.

The moor is managed for grouse shooting. The vegetation of the moor is predominantly heather with patches of moorland grasses and sedges.

The rocks here are mainly Jurassic Sandstones, formed 170 million years ago in shallow estuaries and deltas. To the north, below the escarpment edge, there are many old jet workings. Blocks of ‘White Flint’ can be found on the moor-top.

Both Near Moor and the adjacent Scarth Wood Moor were used by our ancient ancestors, there are the remains of ancient walls, enclosures, trackways and cairns dotted across both moors.

There are a number of cup-marked rocks on the moor, all are very weathered and barely recognisable.

There are the remains of quarries on the margins of the moor, local stone masons also used the prehistoric walls as a source of stone.

On the Grit

Moors

Are a stage

for the performance of heaven.

The audience is incidental.

A chess-world of top-heavy Kings and Queens

Circling in stilted majesty

tremble the bog-cotton

Under the sweep of their robes.

Ted Hughes

Pretty much at the top of my post-lockdown visit list was a trip to visit Jenny Twigg and her Daughter Tibb and the Sypeland Crags in Upper Nidderdale. Following a minor navigational blunder, nothing new for me, I met up with Mr. Chappell and Mr. Vasey and we set off across Fountains Earth Moor.

Travel almost anywhere in the Pennines and their foothills, you’ll see crags and cliffs defining the upper slopes of the Pennine Dales and hilltops. These outcrops are generally composed of either sandstones or limestone. Millstone Grit is a generic term for a number of Pennine sandstones. Both the sandstones and the limestone were deposited over 300 million years ago during the Carboniferous Period.

At first, with some spread of warm shallow seas, limestone formed, the Carboniferous or Mountain Limestone that was to be built into some of the most solid and respectable piles in England, buttresses of its pride and self confidence. The work of silting up these Carboniferous seas was completed by deposits brought from the northern continent of Atlantis, then hot, mountainous and swept by monsoons. A large river with tributaries drawn from territories stretching from the north of Scotland to Norway poured out its coarse sediments across north-eastern England. So were Norwegian pebbles brought to Yorkshire and held in the Millstone Grits that were laid down as the deltas of this northern river.

Jacquetta Hawkes.

The Pennine limestones are massive and dense and form great scars where they outcrop along the scarp edges of the hills. Limestone can be weathered chemically, the weakly acidic rains and rivers of the uplands gradually dissolves the limestone to form the deep gorges and caves and the iconic limestone pavements of the Karst landscapes of the Pennine Uplands.

When Millstone Grits outcrop on the scarp edges they tend to form crags and cliffs. These sandstones are resistant to chemical weathering so are eroded by wind and ice. the weather is able to erode the weaker beds within the sandstones and sculpt the rocks into strange shapes. There are many of these sculpted outcrops along the Pennine edges and tops, almost all were formed during the last Ice Age, the most well known being Brimham Rocks which is now owned by the National Trust and has been a popular tourist attraction for many generations.

Sypeland Crags are little known and somewhat off the tourist beat and track, this was evident by the lack of ancient or modern graffitti on the rocks. The rock type here is the Lower Brimham Grit, a course grained sandstone. There are only 3 named rocks on the moor, Jenny Twigg and her Daughter Tibb and a massive boulder called Tib’s tent.

The origin of the Twigg and Tibb names is not known and there are very few literary references to the stones. I first read about them in Guy Ragland Phillips book, Brigantia – A Mysteriography. Phillips quotes a passage from William Grainges 1863 book, Nidderdale.

..is a large group of naked rocks, some of them of enormous bulk, called Sypeland Crags; they are of the course millstone grit, like those of Brimham, the grotesque grandeur of which they imitate, though on a smaller scale. Two of them a short distance from the main group are tall upright pillers and at a distance have the appearance of giantesses in broad bonnets, from which resemblance they have recieved the names of Jenny Twigg and her Daughter Tibb,

William Grainge

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The folklore of the area says that Jenny Twigg and Tibb were the keepers of a drovers inn on the side of Dead Man’s Hill. They are said to have robbed and murdered three drovers and buried their decapitated bodies. When the bodies of the men were discovered Jenny and Tibb were found guilty of murder and hanged. Another tale says that they were witches who were turned to stone, a familiar tale at number of megalithic sites. The tale of the witches being turned to stone is very similar to tales in Scandinavian folklore where are number of large rock features are thought to have been giant trolls, of both sexes, who were instantly petrified when the suns rays fell upon them.

Ragland Phillips book doesn’t mention the murders and there appears to be no official records of the trial and execution of the women. He does mention the summit of Dead Man’s Hill, telling us that three headless bodies were found at a point where three tracks diverge into Wharfedale, Coverdale and Nidderdale. He goes on to say that it is also the point where three walls meet at a ‘peculiar’ structure known as Jenny’s Gate. It strikes me that the burial of three headless bodies at the point where three important tracks meet, if true, sounds more ritualistic than anything else.

Jenny Twigg has a hole running through the stone, the hole is large enough to pass your arm through. In some parts of our islands there was a tradition that any oath or vow sworn, including marriage, and shook upon through a holed stone, was ‘sealed in stone’ and never to be broken

There are a number of beautiful weather-sculpted rocks along the edge of the crags.

Some of the rocks have been undercut by the elements, one has been walled-in to form a rock shelter. Others have small pools of peat-stained water at their base and on the top surface of one large rock there are a number of large basins, the most I’ve ever seen.

Pereidolia – The Kiss

Tibbs Tent and light snow

This is a grouse moor, the butts are well kept, there is a maintained shooting house and there is grit left out for the birds, over the course of our day we only saw one grouse on the moor. We left for home watching squalls drifting over the distant Vale of York.

Etymology

Sypelands – Sibberlands 1609

Nidd – British river name. Root Nei – to be brilliant. Nedd/Neath – Wales, Nita – Germany, Nidar – Scandanavia

Sources

Moors. Remains of Elmet – Ted Hughes 1979

A Land – Jacquetta Hawkes 1978

Brigantia, A Mysteriography – Guy Ragland Phillips 1976

Map Image reproduced with the permission of the National Library of Scotland 

The Consise Oxford Dictionary of Place Names – Eilert Ekwall. 1974 edition

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

Stone

Crossing the muddy, cattle-churned field from the Hutton Road, there are various earthworks visible in the low winter sun. This was once the site of a Medieval leper hospital overlain by a nineteenth century tramway, built to transport ironstone from the local mines.

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I follow the path uphill, the woodland sits in the winter shadow of the escarpment. I stumble up the steep, muddy track to the lichen-splattered, table-top outcrop, the Hanging Stone.

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Many visitors have left their mark on the outcrop.

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Out of the shadows, walking from Ryston Nab along Ryston Bank, warmed by the low winter sun. A line of prehistoric barrows follows the scarp edge, the ancestors watch over Bousdale. An intake wall, now in ruins, has been built across the barrows, the tumbled wall stones contain fossils. There were once other cairns here, marked on the early maps, erased by the forester’s plough.

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I leave the footpath and follow a line of boundary stones across Hutton and Newton Moors. The stones follow a low ridge and have been erected on top of prehistoric mounds. The mounds are most likely Bronze Age in date, all have been disturbed by excavation. The boundary stones date from the mid-eighteenth to early nineteenth centuries and mark the parish boundaries between Newton, Pinchinthorpe, Hutton Lowcross, Guisborough and Great Ayton.

Ryston: rhiw – Welsh ‘hill, ascent’

Roseberry Topping – Othensberg 1119

Chasing the Solstice Sun

On an overcast Solstice day, I go looking for one of Frank Elgees prehistoric settlement sites in the Commondale Beck valley

Limekilns are few and far between on the northern moors

Tall solitary pines are also a rarity.

Sunlight briefly breaks through, a moment of joy

The sound of the train fills the valley

The settlement site sits on a terrace overlooking the Commondale Beck. Elgee found other sites on located on the same terrace on both sides of the river.

An old hollow way leads to one of the many rocky outcrops on the valley side, a quarry for field walls and butts.

Clouds are moving rapidly westwards across the moors, I catch a glimpse of the sun.

An alignment of grouse butts runs across the moor, tops covered with fresh turfs.

The moor is sodden, there is a possible alignment of standing stones on the moor top

I return to the road, blue skies can be seen through a break in the clouds above the Kildale Gap, I head west.

On the edge of the escarpment I encounter the sun, I drink tea and bask in its warmth.

A Chambered Cairn

I took a walk today onto Great Ayton Moor to visit the Chambered Cairn. There is an excellent account of the Monument by Mike Haigh on the Northern Earth website here