Rey Cross ii

OE stan ‘stone, stones’ is a very common pl. el. It is used alone as a pl. n. in STAINES, STEANE, STONE, where a Roman milestone or some prominant stone of another kindmay be referred to.

The Concise Oxford Dictionary of English Place Names. Eilert Ekwall. 1959

I recently took a trip over the Pennines to Cumbria. On the way home I stopped on Stainmore to have a look at Rey’s Cross. The Cross is located in a lay-by beside the A66. The A66 crosses the Pennines through the Stainmore Gap, a Pennine pass that was created by the flow of ice sheets during past glacial periods.

Historically, This part of Stainmore has always been important. The moor is rich in late Prehistoric remains. It was also the site of a large Roman marching camp, within the ruins of the camp is a wrecked prehistoric stone circle. Legend has it that the stone cross was raised as a memorial to Eric Bloodaxe, the last king of York, who was slain on the moor in 954.

Eric_Bloodaxe_coin_b

The cross, situated near the highest point of Stainmore, is close to an ancient county boundary, is a weathered shaft set into a substantial stone base and is thought to date to the early anglo saxon period. The name`Rey’ is thought to have been derived from the Old Norse element `hreyrr’ which can be taken to mean a heap of stones forming a boundary.

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One of the earliest references to the stone is from The Chronicle of Lanercost where it is call ” Rer Cros in Staynmor ” The chronicler states that it was set up as a boundary marker. The boundary was between the Westmoringas and the Northumbrians, the Glasgow diocesan border, before that it marked the border between the Cumbrians and the Northumbrians.

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The antiquarian William Camden tells us ” This stone was set up as a boundary between England and Scotland, when William (the Conqueror) first gave Cumberland to the Scots.”  Camden was incorrect, at the time of the Norman conquest much of Cumberland was already under Scot’s rule. The historic county of Cumberland was not established until 1177, however the stone could still have marked the boundary of the territory.

The A99 was widened in the early 1990’s so in 1990 the stone was moved from the south side of the road to its present site on the north side. An archaeological survey and excavation was undertaken as part of a wider archaeological project, sadly no burial was found beneath or around the stone.

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What fascinates me about this stone is that it marks a place that has been significant to the people of our islands for thousands of years. The people of the Neolithic period used this as route way between the east and west coasts. Later, the people bronze age erected a stone circle close to the site. Later still, the Romans heavily fortified road to guard the legions marching between Catterick and Penrith and it has remained the primary northern trans-pennine link ever since.  A hundred or so metres west of the stone is the modern east/west boundary between Cumbria and Durham and the route was also once the medieval border between Scotland and England. East meets west, north meets south all within sight of the weather-beaten old stone.

Gunnerkeld Stone Circle

Gunnerkeld – Sportsman’s Spring

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This beautiful concentric stone circle is situated a mile and a half north of Shap in Cumbria, an area rich in prehistoric monuments.

It is thought that the outer circle was erected during the Neolithic period. The circle is the same diameter as the famous stone circle at Castlerigg. Another similarity is the two large portal stones, a feature that can also be found at the Castlerigg circle. This leads to speculation that perhaps the two circles were erected by the same prehistoric architect.

The inner circle and a central cist were added during the Bronze Age, perhaps changing the use of the site from a place of ceremony and ritual to a sepulchral function, a place of the dead.

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Another remarkable aspect of this lovely stone ring is it’s proximity to the M6 southbound carriageway, which is just a stones throw away.  The soundtrack here is one of speeding traffic.

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Access to the site is via Gunnerwell Farm, this is private land, if you visit be sure to ask at the farmhouse, the farmer is very friendly. Also you need to cross a stream to access the field where the stones are located, wellies are advisable.

Sources

The Stone Circles of Cumbria – John Waterhouse 1985

Prehistoric Monuments of the Lake District – Tom Clare 2007

A Guide to the Stone Circles of Cumbria – Robert W.E. Farrah 2008

The Cammon Stone

Cammon Stone

The Cammon Stone from the Celtic ‘cam’ meaning bank stone. On its leaning side is a Hebrew inscription HALLELUJAH which was one the source of much controversy as it was thought to be Phoenician but can be compared to the Hebrew lettering on the Bransdale Mill inscription. It is most likely the work of Rev. W. Strickland a 19th century vicar of Ingleby.

Source – Old Roads & Pannierways in North Yorkshire. Raymond H. Hayes. NYMNP 1988

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 moorsOLYMPUS DIGITAL CAMERA

Tall solitary pines are also a rarity.

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Sunlight briefly breaks through, a moment of joy

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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.

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

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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

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

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

Leaving Eden – Moor Divock

 I’ve been exploring this moor for many years.

MD

The Kopstone, gatekeeper of the moor. Looking towards Shap with the Howgills in the distance. The low escarpment on the upper left of the picture is Knipe Scar with its  limestone stone circle, part of a chain of at least a dozen intervisible prehistoric monuments in the Lowther valley from Oddendale in the south to the Leacet circle in the north.

 

There is a loose alignment of monuments running across the moor, walking between this large pair of stones leads you towards the cairn circle known as Moor Divock 4

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MD4

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Stan Beckensall believes that the roughly circular area, below the arrow in the picture, is an eroded cup and ring motif. I have stared at this stone many times and in many lights, the eye of faith is required.

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Moving west, this embanked alignment of  large upright stones has previously been interpreted as the remains of a circle.

Autumnal colour

Continuing west, an avenue of small, paired stones leads you across the moor towards the White Raise Cairn

MD Arriving at White Raise the western landscape opens out,  the builders of the mound chose well when they selected this spot. The large white limestone block in the centre of the picture is thought to have served as a cover for the cist.

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The cist

White Raise illust

Onwards across the moor following the route of the Roman Road which deviates towards the circle indicating that this route existed long before the Romans arrived on our shores

OS Map Pub 1920

 When the Bronze Age people erected the monuments on the moor, the Cockpit may have already been regarded as an ancient monument.

 

MDThe Cockpit was probably the first stone circle I ever visited.

Cockpit

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Looking west across the moor from the Cockpit to White Raise and the Pennines beyond. Thinking about the journey home.

Sources

The Prehistoric Remains on Moordivock near Ullswater by M. Waistell Taylor. TCWAAS 001. 1886

The Stone Circles of Cumbria by John Waterhouse. Phillimore & Co. 1985

Map extract Reproduced with the permission of the National Library of Scotland

Into Eden – The Druidical Judgement Seat

DJS

Who could resist visiting a place with such a wonderful name?

I first visited this place in 2004, at that time very little was known about this strange oval earthwork. The site, on the margins of Brackenber Moor, has since been the subject of an Archaeological investigation by the Appleby Archaeological Group and North Pennines Archaeology.  They have concluded that the site, and a number of burial mounds located across the moor, are Bronze Age in date.

George Gill

On the ground there is very little to see. The surrounding moorland is a mix of rough pasture and a golf course. The site occupies a spit of land overlooking the George Ghyll. The ditch and bank are visible and there are a few lumps and bumps within the enclosure. What excites me about this place is the beautiful red sandstone crag and cave located on the edge of the Ghyll.

Standing Stone

Dropping down to the Ghyll just beyond a large standing stone

DJS

George Gill SandstoneAeolian (wind-blown) in origin, the Permian Penrith Sandstone Formation formed approximately 272 to 299 million years ago in a desert environment

George Gill Cave

The main cave could easily house two or three people comfortably. There are many birds nests in the niches in and around the main cave.

Roman Fell

The 5th hole looks towards Roman Fell.

Parasol Mushroom

Dykes on the Tabular Hills

The linear dykes of the Tabular Hills of north east Yorkshire are the third largest group in Britain both in area and the number of dykes.

The Scamridge Dykes are the most famous of the North Yorkshire Dykes, they run six abreast in a large curve for almost three kilometers from the scarp edge of Troutsdale south to the head of Kirkdale.  Their scale can only really be appreciated from the air. The dykes are thought to be prehistoric in origin, they most probably define prehistoric territorial boundariesDykes

The Cockmoor Dykes also run south from the Troutsdale scarp where as six large dykes. As they run south to Wydale they are joined by another fourteen smaller parallel dykes.  The six large dykes are thought to be prehistoric and the additional dykes are thought to be burrowing mounds connected with the large-scale rabbit warrening industry of the eighteenth and nineteenth centuries.

Cockmoor

My friend Chris Corner and I took a trip down to the Tabular Hills to have a look at these mighty earthworks. We started by trying to find an embanked pit alignment at Givendale but found nothing apart from dense conifer woodland, debris and deep forestry plough ruts. We moved east to Cockmoor.

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The multiple small dykes at Cockmoor, probably the result of commercial rabbit warrening.

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One of three round barrows on the margins of the Cockmoor Dykes. The other two barrows have been destroyed by agricultural activities.

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The rabbits have all gone. Tiny spoil heaps in the sides of the dyke, probably caused by burrowing miner bees.

One of the six large Cockmoor Dykes running down to the scarp edge overlooking Troutsdale.

A Penny Bun & Oysters

The Scamridge Dykes form a dense mixed woodland corridor across the large open fields.

 We dropped down into Troutsdale and come across this beautiful abandoned building. Chris informs me that it is a school house built in 1870

Map

Sources

Linear Earthworks of the Tabular Hills, North East Yorkshire. D.A Spratt 1989

MAGIC

Historic England

Google Earth

 

A walk to the Source of the Ure

I wrote this account of a walk I took to the source of the River Ure in 2005. It was first posted on Julian Cope’s The Modern Antiquarian website.

The River Ure rises in the Pennines and then heads east into Wensleydale, it then flows out of Wensleydale into the Vale of York. South of York the Ure is joined by the much smaller Ouse Gill Beck and the river’s name becomes the River Ouse, I’ve never figured that one out. The river then flows south east and merges with the Trent to form the River Humber, which then flows out into the North Sea. What is significant about the Ure is its association with a number of nationally important prehistoric sites.

The Ure flows through Wensleydale, a Yorkshire Dale that has been occupied since at least the Late Upper Palaeolithic period. As the Ure flows through Yorkshire it is associated with at least 2 cursus, 7 henges, a stone row, numerous cairns, barrows, rock art sites, burned mounds and an assortment other prehistoric sites.

It is quite possible that during the Neolithic period, the River Ure was one of the ‘lines of communication’ between the Wolds culture of East Yorkshire and the Neolithic peoples of Cumbria. Evidence for this communication can be seen in the large numbers of Group VI stone axe blades found in East Yorkshire. The greatest concentration of Group VI axe blades occurs around the Humber estuary.

group vi

These axe blades all originated from the Great Langdale Axe production areas in Cumbria. Reciprocally there has been a significant amount of flint from the East Yorkshire coast found on a number of Cumbrian sites. There are also various other correlations between the prehistoric monument types and pottery found in both East Yorkshire and Cumbria but I’ll not detail them here in this brief summary.

Neolithic_stone_axe_with_handle_ehenside_tarn_british_museumLangdale Axe Image Credit

Archaeologist Jan Harding speculates that the name ‘Ure’ derives from the Celtic word Isura, meaning ‘Holy One’. The source of the Ure captured my imagination mainly because of its location and proximity to the source of another great river that features in the prehistory of the North of England, the River Eden.

The Ure and the Eden rise within two kilometers of each other on the western edge of the Pennines. At their closest point, the two rivers pass within less than four hundred metres of each other. This means that it is theoretically possible to travel from the North Sea to the Irish Sea only walking on dry land for less than four hundred paces. I’m not suggesting that this was actually the case, where the rivers are at their closest they are merely becks. All I’m saying is that it is theoretically possible that our ancestors may have used the course of these two great rivers as a guide, a navigable route, between the east and west coasts of Britain.

Ure Head 3

Field notes

“In November days,
When vapours rolling down the valleys made
A lonely scene more lonesome”

Influence of Natural Objects by William Wordsworth

I drove down to the site via Brough and Kirby Stephen and then along the Mallerstang Valley. I parked the car in a convenient lay-by and took the footpath to How Beck Bridge and then on up to Green Bridge.

With the Howgill Fells forming one side of Mallerstang and the Pennines forming the other it is easy to see why Mallerstang probably receives more than its fair share of rain. On the day I went it was raining on and off all day, the becks were full to the brim, almost every rocky ledge on the fell had been transformed into a beautiful waterfall with the ground completely saturated. In other words, a typical upland Pennine scene.  They say that the sheep around these parts have webbed feet.

Ure Head 2
I left the path at How Bridge and followed the beck upstream. Its rough walking on the fells and involves a fair bit of bog-trotting and beck jumping, the peat on the moor side had been cut at regular intervals, presumably to aid drainage, so it was possible to follow the tracks of the vehicle that performed the peat cutting for much of the journey.
There is very little wildlife to be seen on these upland fells, a few ravens and the odd small bird, I guess the ground is too waterlogged for rabbits, but it is far from a silent wilderness, there is the sound of running water everywhere. The hike to the summit is one of those frustrating walks that presents you with two false summits to breach before you reach the fell top.
The Ure finally disappears into a flat bog on the summit of Lunds Fell. I was hoping that the source of the river would be a discernible feature such as spring but this wasn’t the case, the beck just petered out into a featureless boggy plain.

Ure Head
I sat and had a cup of coffee at the modern cairn on top of the fell, to the north I could see the Pillar marking the source of the Eden . I was just about to set off walking to the pillar when a storm blew across from Wild Boar Fell and I found myself in cloud. Not being familiar with the area, and not wanting to blunder into a bog I decided that I would call it a day and return home. I would leave the Eden for another day. As I’ve said before, it’s always nice to have something to come back for.
All in all I guess the source of the Ure is definitely ‘one for the enthusiast’ but if you want to get the general feel of the place you can drive along the Mallerstang valley and stop somewhere around SD778963. At this point, you’ll be straddling the county border, east meets west, watching the Eden flowing north into Cumbria and the Ure flowing south into Yorkshire.