To search for any sites in the northern counties of England (previously known as Brigantia), click on the list of relevant counties, below. Please note that not all these english counties were truly in Brigantia, but they came close to its southern edges; and as parts of them tickle the edges of the southern Pennines, I thought they should be included. Hope that’s OK with everyone!
Takes a bitta finding this one! Take the B6265 road north out of Skipton, and about a mile along, turn left up the small road to Stirton village. But once on the level and the open countryside opens to your right, where there’s a notable bend in the road and a track goes up into the field, stop! Walk up past the closed fields and, where the open country starts, veer to the left track (not up the official footpath). Keep walking up here till you’re approaching the bend in the old walling; but veer into the grasses, right, about 50 yards before it. Good luck!
Archaeology & History
Very recently, Mr Paul Hornby called us to come and check a number of features he’d come across on a portion of open countryside not far from Skipton. At the very least it was gonna be a nice day out, ambling abaat and seeing some potentially new prehistoric sites — and we weren’t to be disappointed!
Close-up of cupsSingle cup-mark nearby
Although this site aint much to write home about, it is found close to a number of other recently rediscovered prehistoric features. Upon a fairly large stone a coupla hundred yards east of a supposed tumulus to the southern ridge of Sharp Haw, we find an arc of three cup-markings on the rock’s northeastern face, with a possible fourth cup along the same line (though I aint sure misself). And that’s it I’m afraid. Nowt else. (and I’ll try getting some better images when we’re next up there) Another stone nearby to the west has a near-perfect single cup-marking on its flat surface.
ACKNOWLEDGEMENTS:
Huge thanks to Paul Hornby for the use of his photos!
From the lovely village of Summerbridge (near Pateley Bridge), go up the steep Hartwith Bank road, going straight across at the crossroads for another few hundred yards, passing the old tombs of Graffa Plain on your right…and they’ll start appearing on your left-hand side (west). Do not go into the expensive National Trust car-park. Instead (if you’ve already gone too far), about 100 yards before the Car Park you’ll find a small dirt-track on your left a short distance away. But if you drive past the rip-off car park, another 100 yards on there’s another spot where you can easily park up on the right-hand side of the road. Then cross the road and follow y’ nose…
Archaeology & History
The OS grid reference given above is an approximation — for obvious reasons. This is a huge area that’s covered by Britain’s finest natural megalithic features, obviously sculptured by Nature Herself — though many are the historians who sought to give Druids the credit here. God knows how! The area over which these magnificent rock sentinels live covers some 60 acres and is some 1000 feet above sea level. The view from the hill around which the encircling parade of rocks guards is excellent, allowing our eyes to catch focus on the distant lands of Whernside, Simon’s Seat, York Minster, the Cleveland Hills and Kilburn’s white horse. It’s quite a view.
Easternmost Rocking StoneIdol Stone (Godfrey Higgins 1826)
But this tends to be overlooked when you first visit the place, as the rocks which surround and walk alongside you overwhelm with impressions not encountered before. To those with spirit, you’ll be bouncing and running all day here, clambering upon rocking stones, jumping between dodgy gorges that await falls, and just aching to climb pinnacles that deny you. But then, if you need the selfishness of silence, this arena will only grant such solace when the rains are about, or dense fog and low cloud keeps others from this haunting amphitheatre. And it’s not surprising… The mass of rocks contort into the most beautiful and curious simulacra, which would not have gone unnoticed, nor deemed unimportant in the sacred landscape of our ancestors…
Brimham Rocks have been written about since the 17th century, though they didn’t receive the serious attention of outsiders until the 19th, when numerous Victorian writers — from antiquarians and geologists, to archaeologists and Druids — got to hear about the place. And by the beginning of the 20th century, a veritable mass of articles had been written in journals and travelogues of all persuasions! These quiet Yorkshire Rocks had become truly famous!
Brimham Rocks (Walbran 1856)Old Woman and her consort
A lengthy essay was written in the distinguished archaeology journal of its time, Archaeologia, by northern historian Hayman Rooke (1787), who thought that some of the rocks here had been tampered with by the druids; with the legendary Cannon Rock in particular possessing oracular properties. The site as a whole was, he posited, a temple for Druids in ancient days. Certainly the place would have been deemed as sacred, whether by the druids or our more remote neolithic and Bronze Age ancestors.
Harry Speight & his mates, c.1890
In Harry Speight’s magnum opus, Nidderdale (1894), he described these rocky giants as best as he could, admitting as others before and since, that no mere words can convey the impression that only a personal encounter liberates, saying:
“The Brimham Rocks are among the greatest natural wonders of Yorkshire, and many have been the theories from time to time advanced as to the cause of their extraordinary aspects… The resemblances to natural and artificial objects are most striking. There we have the Elephant Rock, the Porpoise Head, the Dancing Bear (a very singular, naturally-shaped specimen), the Boat Rock, showing the bow and stern completely, etc. Then there is the great Idol Rock, a most mysterious-looking object, of almost incredible size and form. It is a perfectly detached block, fully twenty feet high, weathered along face joints into three roughly circular pieces, each from 40 to 50 feet in circumference, piled one above the other; the whole mass, weighing by estimation over 200 tons, being poised on a pyramid 3½ feet in diameter; the pivot itself supporting this immense column having a diameter of barely 12 inches.
“East of the guide’s house are the famous Rocking Stones, consisting of a group of four rocks, which were discovered to be movable in the year 1786. The two on the west side weighing approximately 50 and 25 tons, require but little force to vibrate, while those on the east side, though much smaller are not so well poised and do not move readily. Each of the larger stones has a basin-like cavity on the top, and a kind of knee-hole open to the north, said to be the work of Druids. Close to the Rocking Stones are the appropriately-named Oyster-shell Rock, and the Hippopotamus’ Head. Turning now some thirty yards north of the Idol Rock we ascend Mount Delectable, where is the agreeable Courting or Kissing Chair, happily at not too close quarters with the above Hippopotamus’ Head and Boar’s Snout. The Chair consists of a single seat, but why it should be so called, I had better leave the amorous lover to solve. West of these is the more sober Druid’s Reading Desk, with its church-like lectern on a stout stone base. The we come to the Lover’s Leap, a gigantic and abrupt face of beetling crag, weathered to the west, and rising to a height of 60 to 70 feet, with three immense fragments balanced in a very remarkable manner at the summit. The rock is in tow principal sections, and an iron hand-rail has been fixed across the chasm to enable visitors to look down from the top. Further south are the Frog and Tortoise Rocks, the latter presenting from one point of view a capital resemblance to a tortoise creeping up the face of the crag towards the imaged frog. A little below this is a good imitation of a cannon, projecting from the edge of the cliff. In addition to these singular resemblances there are many others which the guide points out, such as the Yoke of Oxen, Mushroom Rocks, Druid’s Oven, Dog’s Head, Telescope, and the curiously perforated Cannon Rock, etc.”
In a later work, Speight (1906) also mentioned the existence of a Druid’s Circle some 300 yards west of the main natural temples, but this site appears to have been destroyed. Thankfully the large standing stone on Hartwith Moor, a mile to the south, can still be found upright…
Folklore
Idol Stone (Hargrove 1809)
In folklore, there’s little surprise this place was held by just about every 18th and 19th century historian as a ‘druidic site.’ But more interesting – in the light of Paul Devereux’s (2001) work on acoustic archaeology – is what Edmund Bogg (c.1895) said of these huge contorted stones:
“In bygone days these immense stones were supposed to be the habitation of spirits. The echo given from the rocks was said to be the voice of the spirit who dwelt there, and which the people named the Son of the Rocks. From a conversation we had with the peasantry not far from here, it seems the ancient superstition had not yet fully disappeared.”
This is precisely the notion of spirit given to rocky places elsewhere in the world, where the very echo was perceived as the ‘voice of the rocks’. Meditate on it a bit, in situ. (a fine summary of this notion and its implications — which has crept into archaeology of late — can be found in Paul Devereux’s work, Stone Age Soundtracks)
One of Brimham’s southwestern rocks was known as the Noon Stone when Mr Rooke (1787) came here. There are many stones with this name scattering Yorkshire and other northern counties, each with the same mythic background: that the sun casts a shadow from it at midday to indicate the time of day. Of this Noon Stone Mr Hooke also told us that,
“On Midsummer Eve fires are lighted on the side. Its situation is apposite for this purpose, being on the edge of a hill, commanding an extensive view. This custom is of the most remote antiquity.”
On the very southern edge of Brimham’s Rocks (some might say beyond their real border) is the Beacon Rock — and it is aptly named: as in the year 1887 on the day of Queen Victoria’s Jubilee, a great beacon fire was lit here, signalling to others in the distance. Its title however, pre-dates Victoria’s Jubilee, though we don’t know how far back in time it goes…
…to be continued…
References:
Bogg, Edmund, From Eden Vale to the Plains of York, James Miles: Leeds c.1895.
Devereux, Paul, Stone Age Soundtracks: The Acoustic Archaeology of Ancient Sites, Vega: London 2001.
Grainge, William, The History and Topography of Harrogate and the Forest of Knaresborough, John Russell Smith: London 1871.
Harrison, William, A Descriptive Account of Brimham Rocks in the West Riding of Yorkshire, A. Johnson: Ripon 1846.
Michell, John, The Earth Spirit: Its Ways, Shrines and Mysteries, Thames & Hudson: London 1975.
Michell, John, Simulacra, Thames & Hudson: London 1979.
Rooke, Hayman, “Some Account of the Brimham Rocks in Yorkshire,” in Archaeologia journal, volume 8, 1787.
Speight, Harry, Nidderdale and the Garden of the Nidd, Elliot Stock: London 1894.
Speight, Harry, Upper Nidderdale, with the Forest of Knaresborough, Elliot Stock: London 1906.
Walbran, John Richard, A Guide to Ripon, Fountains Abbey, Harrogate, Bolton Abbey, etc, Johnson: Ripon 1856.
Take the road up to Brimham Rocks from Summerbridge; crossing the little crossroads, then keep your eyes peeled for the singular farmhouse on your right. Just beyond this, on your right, you’ll notice some small moorland opens up and reaches gently down the slope for some distance. Go along the footpath for 100 yards or so, then into the heather to your right, for 60 yards or so (as if you walking towards the farmhouse and small crags). This is where the following sites could be found. (when we visited Brimham recently, unfortunately sunfall stopped us having a proper wander here, so the status of the site/s remains unknown to us)
Archaeology & History
This little-known and possibly destroyed prehistoric site — less than a mile north of Standing Stone Hill and just a coupla hundred yards south of the legendary Brimham Rocks — has been described by several antiquarians from the early 19th century onwards. It’s an intriguing place, deserving of much greater antiquarian attention. Ely Hargrove (1809) appears to be the first who mentions prehistoric tombs here, though his sense of direction implies another site (unless he just got that part of it wrong?). Along with “several small tumuli or carns” near another section of Brimham Rocks themselves, he told there to be,
“Several large tumuli; one of which about 80 yards west of the great Cannon, measures 150 feet in circumference. It is worth remarking that the place where most of these tumuli are found is, at this day, called Graffa Plain, i.e., the Plain of Graves.”
These ‘tumuli’ were again mentioned briefly in passing by one ‘D.N.H.’ in the Gentleman’s Magazine of November 1823. The great Knaresborough historian William Grainge also described cairns here. They were then highlighted on the very first Ordnance Survey of the region in the 1850s and shown as “Supposed tumuli.” Eventually, at the turn of the 20th Century, they were explored at the behest of the local land-owner by Mr L.A. Armstrong. His description of what they found here is intriguing and well worth reproducing in full:
“By permission of the Right Hon. Lord Grantley, I was enabled to make a careful examination of two of the ancient burial mounds of ‘ Graff a Plain,’ Brimham Moor, on Tuesday, August 4th, 1908.
“Mound No. 1, of circular form, and about 12′ o” in diameter, is situated about 150 yards north-west of the first large group of rocks, upon the south-eastern boundary of the moor, and about 50 yards south-east of the trackway leading to ‘ Riva Hill Farm,’ and it occupies the summit of a slight hillock, upon a comparatively level portion of the heath, which rises rapidly to the south of it in a bold sweep, terminating in the outstanding rocks of Graffa Crags and Brimham Beacon.
“The entire absence of any heather upon the mound, and the profusion of bright green bilberry plants which covered it and at the same time rendered its outline more noticeable, told plainly of a different character of subsoil from that of the surrounding moor ; but prominent as the mound appeared, its actual elevation was deceptive, being barely two feet above the natural level, and the uneven character of the upper surface suggested previous disturbance to be more than probable. A few attempts to pierce the crown, however, proved it to be a cairn, constructed of large stones, and accounted for the prolific growth of the rock-loving bilberry which overspread it, as well as for the uneven character of the surface.
“The thick green covering was carefully stripped off in lengths and placed on one side, and the few inches of vegetable earth removed, revealing the cairn in an almost perfect state, formed of a series of large stones placed methodically in concentric rings, each stone slightly inclined towards the centre, and the whole mass interlocked together by their own weight. Large stones were placed around the outside forming the enclosing circle, which is almost invariably found in the case of earth-built tumuli, and a few of these had been visible before the covering was stripped.
“The construction of the cairn rendered it necessary to remove the stones from the outer ring first, and to work gradually towards the centre where the burial, if such existed, might be expected to lie. This proved no easy task, as the stones were so tightly wedged, and had each apparently been specially selected for the purpose. Almost without exception, they were about a foot in diameter, oblong or oval in form, and three to five inches in thickness, with flat surfaces and rounded edges. No marks of tools were visible on any, but all alike were either water-worn, or had been especially rubbed to their present form. The stone itself was the Millstone Grit of the surrounding moor, but fragments of stone of the form composing the cairn are not now to be found thereon readily, although a careful search might reveal such. Personally I am inclined to think that they have been transported from a considerable distance; that great care has been exercised in their selection is indisputable.
“When nearing the inner radius of the cairn, small fragments of charcoal were noticeable, but they were by no means in large quantities. There was also a layer of fine grey sand an inch or two in depth, which had apparently been spread over the natural surface of the ground, and the stones bedded therein. Sand of this kind is abundant in the vicinity of the rocks upon the moor.
“In the centre, large pieces of stone were piled around a rough circle of about 3′ 6” extreme diameter, and within these, large and small stones, all of the form previously noticed, were laid more or less upon their flat surfaces, and amongst them the grey sand and charcoal were very evident; pieces of the latter up to an inch square, being found.
“Upon the gradual removal of this central mass of stones, the presence of the unmistakable black ‘barrow earth’ became evident in a slight layer, perhaps an inch or an inch and a half in thickness, and spread over the whole area within the inner ring, the bottom of which had been paved with large flat stones. Amongst this earth very slight traces of a greyish white paste-like substance were”] visible, probably the decomposed remains of the bones after calcination. The deposit was carefully gathered together. Its removal bared the large stones forming the bottom of the grave, and these proved to be two in number, the largest being about 2′ o” across, and of a somewhat angular form ; strikingly different to those composing the cairn itself, for the edges were rough fractures, not rounded in any way. Apparently the surface soil had been removed from the ground upon which the cairn was built, for the upper face of the two stones forming the bottom was level with the natural ground surface adjoining, so far as could be ascertained, and these had apparently been laid down for the reception of the deposited remains.
“As there was every reason to believe that some portion of the ashes might have been placed in an urn, efforts were made to raise the stones above mentioned in hopes of a discovery. This was by no means easy, but by care and perseverance, it was at last accomplished, but only to meet with disappointment. Immediately beneath was a slight layer of ashes upon the natural ground surface, which latter showed very evident signs of fire, the bright yellow sand composing the substratum being calcined to a dark red colour for quite 2” in depth. This sand was very stiff and compact. The most diligent search failed to reveal any trace of a hole or other disturbance at any point, or of any implements which might have accompanied the body, either upon the surface or amidst the cairn.
“One stone found amidst those immediately covering the deposit, was remarkable because entirely different from all the remainder composing the cairn, and appeared to have been shaped with some definite object in view. It was a fragment of hard sandstone, in the form of a truncated pyramid, the sides and top being roughly fractured to shape, but the base was quite smooth, and bore marks of friction. The base measured 6″ x 5″, and the height about 4½”. This might have been used as a crushing and grinding stone for grain, or for rubbing purposes, but careful search failed to reveal its companion slab. With this exception, nothing was found that could be considered as having been fashioned for use, and there was nothing to throw any light upon the probable period of the cairn’s erection.
“The second tumulus examined is situated about 100 yards south-west of the first. It was of rather irregular shape, and appeared to have been somewhat disturbed, but the original diameter had probably been about 9′ o”. Upon examination, it also proved to be of the cairn type, and apparently similar to that previously opened, but it had been disturbed throughout at some distant period, and no trace of the deposit could be found, although the yellow sand forming the subtratum was noticeable, calcined over the whole area as before. There were also traces of charcoal. It is remarkable that amidst the smaller stones of this cairn another ‘ rubbing stone ‘ was found, almost identical with that in the former one, and similarly, this proved to be the only ‘ find ‘ of any description bearing certain traces of man’s handiwork.
“Although somewhat disappointing not to be able to assign the erection of these cairns to any definite period, yet their examination proves valuable for two reasons. First it places beyond any question the nature of the mounds scattered over this portion of Brimham Moor, which is known by the name of ‘ Graffa Plain,’ a name which the late Mr. William Grange translates as ‘ the place of graves ‘ — significant in itself, though he at the same time casts a doubt upon the formation of the mounds in question being anything other than natural. The identity of the grave mounds being established, they prove that a settlement of primitive man of no small magnitude must have been located somewhere in the vicinity.”
The word ‘graffa’ seems to be the plural for ‘graff’, which the english dialect magus, Joseph Wright (1900), convincingly assures us to derive from the old english, “græf, a grave, trench.” This seems confirmed by the common finding of ‘graff’ in regional dialects from Yorkshire, Lancashire and other northern counties, where it relates specifically to ‘graves.’ A variation on the word, as cited above, finds ‘graff’ occasionally relating to “a ditch or trench; a channel, cutting; a hole, pit or hollow.” The usually helpful A.H. Smith (1961-63) was curiously silent on this place-name; but local historians Grainge, Walbran and others tell us that Graffa Plain is simply “the plain of the graves.”
I know of no other accounts that have explored this site. Does anyone have any further information about this place?
References:
Armstrong, A. Leslie, “Two Ancient Burial Cairns on Brimham Moor, Yorkshire,” in The Naturalist, March 1909.
Hargrove, Ely, The History of the Castle, Town and Forest of Knaresborough, Hargrove & Sons: Knaresborough 1809.
Smith, William, “Yorkshire Place-Names,” in W. Smith’s Old Yorkshire – volume 1 (Longmans, Green & Co.: London 1881).
Wright, Joseph (ed.), English Dialect Dictionary – volume 2, Henry Frowde: London 1900.
The site has been known about for nearly 150 years, albeit mistakenly as a series of prehistoric barrows that William Greenwell (1877) told were “near the division between the parishes of Rudston and Burton Agnes” near the crest of the hill. He further told the place to be,
“Two long mounds, almost parallel, their northern end gradually losing themselves in the surface-level, but connected together at the southern end by another long mound.”
South end of Cursus A (after D.P. Dymond)Early photo of Cursus A (after J.K.St Joseph)
Then in 1958 when C. & E. Grantham of Driffield did the first modern excavation here across a section of the western ditch, they found that the long embankment went on much further than ever previously anticipated, for more than half-a-mile downhill in the direction of Rudston village. It wasn’t a long barrow or tombs of any sort, they found! Then in 1961 when Dr. J.K. St. Joseph did aerial survey work over the area, he and his colleagues established that this monument consisted of extensive parallel ditches stretching for at least 1½ miles towards and past the eastern side of Rudston village. It’s nature as a cursus monument was rediscovered after several thousand years in the wilderness… (on St. Joseph’s survey, two other cursus monuments were also found in the vicinity, being Rudston Cursus B and Cursus C) Readers will hopefully forgive me for quoting at some length Mr Dymond’s (1966) article on the site (with minimal editing!):
“The southern end of the cursus lies in the western angle of two roads, Woldgate and Burton Agnes Balk. In plan it is square with rounded corners and consists of a bank with outer ditch. Although the bank has been ploughed for many years, it still remains substantial; it stands up to 4 feet high from the outside and 1-2 feet wide from the inside. The east and west banks decline in height northwards and are now at their greatest height where they join the southern end. The profile of each bank is smooth and rounded and merges on the outside with the broad shallow depression of the silted-up ditch. The south bank is now 170 feet long overall, and spread to a width of 60-80 feet. It stands higher at both ends than in the middle. This fact was noted by Greenwell, who also recorded that at the southwest angle “there was the appearance of a round barrow raised upon the surface of the long mound.” There is no surface evidence today to suggest a secondary round barrow, and to some extent at least the greater height at the angles is probably due to the concentration of upcast inside a fairly sharp corner.
“The south arm of the ditch has been largely destroyed by a chalk-pit, but the southeast turn is quite clear on air-photographs. There is no suggestion on the ground or from the air that the cursus had ever extended further to the south.
“The cursus begins its descent in a due northerly direction, and loses its eastern side for approximately 600 feet under the enclosure road, Burton Agnes Balk. The ditch can be traced intermittently on the western and eastern verges. It then swings gently NNW around the head of a small slack draining northwest. Thus far the cursus is traceable on the ground. The ditches are the most consistent feature, showing as broad shallow depressions 20-40 feet wide and 70-80 yards apart, which when in fallow attract a dark coarse vegetation (particularly thistles and nettles. The banks inside the ditches are sometimes visible in relief though considerably spread. Where the banks have been almost entirely ploughed out, a chalk spread usually marks their position.
“There is a suggestion on the ground that the banks and ditches may have been separated by berms, particularly on the east side near the square end. This appears to be confirmed by the silting of the ditch in the excavated section…
“Proceeding further downhill in the direction of Rudston village, the cursus quite suddenly swings north-NNE, finally crosses Burton Agnes Balk, and passes to the west of Pits Plantation. On the west of the road both banks and ditches are still visible in relief, and the ditches produce a firm crop-mark. East of the road no surface traces are discernible, and only the eastern ditch shows intermittently as a crop-mark.
“For ½-mile across the floor of the Great Wold Valley, there is no trace of the cursus. The area has been ploughed since medieval times, and there is in addition a considerable Romano-British settlement. It is worth noting that in this length, the cursus must have crossed the stream of the Gypsey Race, surely a fact of some importance in any discussion of the function of cursuses.
“Two parallel ditches c.60 yards apart, visible on air photographs in a field immediately north of the modern Rudston-Bridlington road, seem to represent the continuation of the cursus. The ditches travel for approximately 300 yards and end at the Bridlington Gate Plantation. There are no surface traces in the field, but a depression in the plantation may represent the eastern ditch. This depression is crossed obliquely by the remains of a low bank and ditch running along the length of the plantation WSW and ENE. This latter (part) is probably part of the supposedly Iron Age entrenchment system, and has certainly been used as a road from Rudston to Bridlington, as the name of the plantation implies.
“The northern end of the cursus cannot be traced. Possibilities are that the end was in the plantation and has been destroyed by the later earthwork, or that the cursus proceeded NNE for an unknown distance. If the latter hypothesis is accepted, the western ditch must be under the Argam Dykes, a double entrenchment which appears to terminate at the northern side of the plantation, and the eastern ditch is indistinguishable from ploughing lines to which it is parallel…
“Cursus A has its southern end at a height of 254 feet OD, on the forward face of a long chalk ridge running WSW and ENE. From this point the course of the cursus is visible, except for that part west of Pits Plantation. The last known part in Bridlington Gate Plantation, 1½ miles off, is clearly visible. Seen against the contours of the area, the cursus has one end resting on a high ridge, crosses a broad valley, and climbs at least in part, the far side. It appears to pass approximately 300 yards east of the monolith in Rudston churchyard.”
Line of Rudston A
The presence of this and three other cursus monuments close by (Rudston B, C and D) indicates that the region was an exceptionally important one in the cosmology of our prehistoric ancestors. Four of these giant linear cursus monuments occur in relative proximity, and there was an excess of ancient tombs and, of course, we have the largest standing stone in the British Isles stood in the middle of it all. A full multidisciplinary analysis of the antiquities in this region is long overdue. To our ancestors, the mythic terrain and emergent monuments hereby related to each other symbiotically, as both primary aspects (natural) and epiphenomena (man-made) of terra mater: a relationship well known to students of comparative religion and anthropology who understand the socio-organic animistic relationship of landscape, tribal groups and monuments.
References:
Dymond, D.P., “Ritual Monuments at Rudston, E. Yorkshire, England,” in Proceedings of the Prehistoric Society, volume 32, 1966.
Eliade, Mircea, The Sacred and the Profane, Harvest: New York 1959.
Greenwell, William, British Barrows, Clarendon Press: Oxford 1877.
Hedges, John & Buckley, David G., The Springfield Cursus and the Cursus Problem, Essex County Council 1981.
Nicholson, John, Beacons of East Yorkshire, A. Brown & Sons: Hull 1887.
Pennick, Nigel & Devereux, Paul, Lines on the Landscape, Hale: London 1989.
One of the four (known) cursus monuments around Rudston: this one stretches between the Ordnance Survey coordinates TA 081669 near Kilham Grange on the southwestern edge of Rudston, then heads northeast towards the village itself at TA 094675. Described briefly in D.P.Dymond’s essay on (mainly) Cursus A, he said how Cursus B was part of,
Early ground-plan (after D.P. Dymond)Early photo of Rudston B (after J.K.St Joseph)
“a large complex of crop marks. The largest feature is the squared, tapering end of Cursus B, which can be traced for 700 yards in a north-easterly direction. No surface remains seem to survive in an area intensively ploughed, except for a swelling under a hedge on the line of the south-eastern bank (at TA 0834 6703). West of the square end and partly overlying it, are several small rectangular enclosures, which are probably part of a later (?Romano-British) settlement and field-system. Also in this tangle of crop-marks there are four roughly circular shapes, which may well be barrow circles associated with the end of the cursus. On certain barrow just south of the end of the cursus has an inner ring of pits. Where the cursus is lat visible to the north-east, it is headed roughly for the monolith ¾-mile away. The width of Cursus B is approximately 90 yards between ditch centres. It has its square end on the forward slope of a ridge (like Cursus A) at a height of 180 feet OD, and descends towards the village, which is visible from the end, through a shallow valley.”
Dymond’s note about the alignment feature of this cursus, towards the gigantic Rudston monolith, was one echoed in the Hedges & Buckley (1981) survey. They noted:
“At Rudston, the B cursus extended eastwards aligns upon the Rudston monolith in Rudston churchyard. Destruction of standing stones elsewhere may have removed similar associations between the stones and cursuses.”
This alignment feature was also confirmed by cognitive archaeologist and alignment specialist, Paul Devereux (Pennick & Devereux 1989) in his survey of cursus monuments.
Typical of these fascinating antiquities, nothing of any worth has been found along the length of the cursus that can give us any clues to its nature and function. However, the presence of this and three others close by indicates that the region was an exceptionally important one in the cosmology of our prehistoric ancestors. Four of these giant linear cursus monuments occur in relative proximity, and there was an excess of ancient tombs and, of course, we have the largest standing stone in the British Isles stood in the middle of it all. A full multidisciplinary analysis of the antiquities in this region is long overdue. To our ancestors, the mythic terrain and emergent monuments hereby related to each other symbiotically, as both primary aspects (natural) and epiphenomena (man-made) of terra mater: a phenomenon long known to comparative religious students and anthropologists exploring the animistic natural relationship of landscape, tribal groups and monuments.
References:
Dymond, D.P., “Ritual Monuments at Rudston, E. Yorkshire, England,” in Proceedings of the Prehistoric Society, volume 32, 1966.
Eliade, Mircea, The Sacred and the Profane, Harvest: New York 1959.
Hedges, John & Buckley, David G., The Springfield Cursus and the Cursus Problem, Essex County Council 1981.
Pennick, Nigel & Devereux, Paul, Lines on the Landscape, Hale: London 1989.
Follow the same directions to find the Blackheath Circle, but instead of turning onto the golf course, keep going up the steep road until you reach the T-junction at the top; then turn left and go along the road for about 200 yards, past the second track on the left, keeping your eyes peeled across the small moorland to your left where you can see the rocks rising up. Walk along the footpath towards them. You can’t really miss the place!
Archaeology & History
The Bride at sunset – the fallen Groom to her left
If you’re a heathen or geologist and you aint seen this place, check it out – you won’t be disappointed! First mentioned in 1491, this has always been a place of some repute. Its legendary companion, the ‘Groom’, lays resting on the Earth after being felled sometime in the 17th century.
F.A. Leyland’s 1860s drawing
A beautiful, remarkable and powerful site of obvious veneration. First described in local deeds as early as 1491, there are a great number of severely weathered boulders all round here, many like frozen rock giants haunting a magickal landscape. The modern lore ascribes the stones to be dedicated to Bride, goddess of the Brigantian people. And like Her legendary triple-aspect, we find here in the landscape a triple aspect to the outcrops themselves: to the west are the Bride Stones; to the east, the Little Bride Stones; with the Great Bride Stones as the central group, surveying everything around here.
At the main complex is what is singularly known as the Bride itself: a great smooth upright pillar of stone fourteen feet tall and nine feet wide at the top, yet only about two feet wide near its base, seemingly defying natural law. Watson (1775) described, next to the Bride herself, “stood another large stone, called the Groom…(which) has been thrown down by the country people” – probably under order of the Church. Crossland (1902) told how the Bride also acquired the title, “T’ Bottle Neck,” because of the stone’s simulacrum of an upturned bottle.
The Bride & her Groom (laid on the earth)The ‘head’ or top of the Bride Stone
Scattered across the tops of the many rocks hereby are many “druid basins” as Harland and Wilkinson (1882) described them. Many of these are simply basins eroded over the millenia by the natural elements of wind and rain. It is possible that some of these basins were carved out by human hands, but it’s nigh on impossible to say for sure those that were and those that were not. If we could find a ring around at least one of them, it would help — but in all our searches all round here, we’ve yet to locate one complete cup-and-ring. So we must remain sceptical.
On the mundane etymological side of things, the excellent tract by F.A. Leyland (c.1867) suggested the Bride Stones actually had nothing to do with any goddess or heathenism, but derived simply from,
“the Anglo-Saxon adjective Βñáð, signifying broad, large, vast — hence the name of the three groups known as the Bride Stones. The name of The Groom, conferred on the prostrate remains, appears to have been suggested by the fanciful definition of the Saxon Brád, as given by (Watson).”
However, the modern place-name authority A.H. Smith (1963:3:174) says very simply that the name derives from “bryd, a bride.”
A “rude stone” was described in one tract as being a short distance below this great rock outcrop; it was turned into a cross by the local christian fanatics and moved a few hundred yards west, to a site that is now shown on modern OS-maps as the Mount Cross.
Folklore
Although local history records are silent over the ritual nature of these outcrops, tradition and folklore cited by the antiquarian Reverend John Watson (1775) tell them as a place of pagan worship. People were said to have married here, although whether such lore evolved from a misrepresentation of the title, Bride, is unsure. In the present day though there have been a number of people who have married here in recent years.
If the Brigantian goddess was venerated here, the date of the most active festivities would have been February 1-2, or Old Wives Feast day as it was known in the north. The modern witches Janet and Stewart Farrar, who wrote extensively about this deity (1987), said of Bride: “one is really speaking of the primordial Celtic Great Mother Herself,” i.e., the Earth Mother.
Telling of further lore, Watson said that weddings performed here in ages past stuck to an age-old tradition:
“during the ceremony, the groom stood by one of these pillars, and the bride by the other, the priests having their stations by the adjoining stones, the largest perhaps being appropriated to the arch-druid.”
New Age author Monica Sjoo felt the place “to have a special and uncanny power.” This almost understates the place: it is truly primal and possesses the virtues of strength, energy, birth and solace.
References:
Bennett, Paul, The Old Stones of Elmet, Capall Bann: Milverton 2001.
Crossland, Charles, “Place-Names in the Parish of Halifax in Relation to Surrounding Natural Features,” in Halifax Naturalist, volume 7, 1902.
Farrar, Janet & Stewart, The Witches’ Goddess, Hale: London 1987.
Harland, John & Wilkinson, T.T., Lancashire Folklore, John Heywood: Manchester 1882.
Leyland, F.A., The History and Antiquities of the Parish of Halifax, by the Reverend John Watson, M.A., R.Leyland: Halifax n.d. (c.1867).
Smith, A.H., The Place-Names of the West Riding of Yorkshire – volume 3, Cambridge University Press 1963.
Watson, John, The History and Antiquities of the Parish of Halifax, T. Lowndes: London 1775.
If you follow the directions to reach the Churn Milk Joan stone, then continue onto the moor following the same directions to find the Miller’s Grave, once you’ve reach this you’ll see a large rounded boulder a couple of hundred yards away on your left, to the northwest. That’s Robin Hood’s Penny Stone!
Archaeology & History
Robin Hood’s Pennystone, Midgley Moor
In terms of this site’s archaeology, it has none to write home about in official records (other than a few flints found nearby), but there’s more to this place than meets the eye. A large rounded boulder sat upon the moorland plain with a large Nature-worn bowl on its top, the site is some 112 yards (102m) northwest of the little-known, but impressive Miller’s Grave prehistoric cairn (close to being a midsummer/midwinter line). North and south of the rock are small lines of prehistoric walling — though their context is difficult to assess. The Greenwood Stone and Greenwood B stone can be found about 200 yards west.
Folklore
A singular footpath once led up to this old boulder, atop of which – in its large ‘bowl’ – vinegar used to be poured. In this, coins were left by local people who suffered the plague and in return food was left for them. And of course it is said that Robin Hood frequented the place in bygone times.
References:
Bennett, Paul, The Old Stones of Elmet, Capall Bann: Milverton 2001.
Robert, Andy, “Our Last Meeting,” in NEM 37, 1989.
Robert, Andy, Ghosts and Legends of Yorkshire, Jarrold: Sheffield 1992.
Get right to the top of the valley, past the end of the tree-line where the moor opens up ahead of you. Keep going till you reach the farmhouse on the left (there are usually sheepdogs outside, barking their heads off!). Take the track on the right, making sure y’ close the gate (the farmer here is infamous – so please shut the gate!). Cross the yummy stream at the bottom & double-back on y’self. If or when y’ reach the derelict house (an old shooting house), drop down the small valley, over the stream and stick to the bottom edge of the slope. (if y’ don’t reach the house, just cross the stream and keep to the contours) Keep walking for about 200 yards, keeping your eyes peeled for some uprights!
Archaeology & History
As with the Turvin Stone a half-mile southwest of here, this too is a very peculiar site. ‘Peculiar’ inasmuch as no-one really seems to be able to make head or tails what the place actually was. As you’re approaching the place, it looks like some decent ‘four-poster’ stone circle is ahead of you; but once you reach the place there are a veritable number of other earthfast rocks and tumbled stones all round, making your initial appraisal of the place suddenly grind to a halt! Added to this is the oddity of finding the standing stones on a considerable geological slope, unlike most other megalithic sites in the region (and elsewhere for that matter!).
The tallest standing stone
The tallest, easternmost of the three stones (SD 99547 21992) is more than five-feet tall and is lower down the slope than the other uprights here. Almost ‘surrounded’ by some denuded stone enclave (a large robbed cairn perhaps?), this is the most visually impressive of the stones here. Up the slope from here 15 yards (13.56m) away is what may, or may not, be a simple earthfast boulder (at SD 99535 21999): but it’s upright, about 3 feet tall, and due to proximity gives the impression that it was part of whatever monument this site once was. Due west of the tallest standing stone nearly 20 yards (17.6m) away, is a more rounded stone of ‘female’ character, less than 4 feet tall (at SD 99528 21993). That’s the general gist of the place.
If you visit here you’ll notice another smaller upright a short distance further down the slope in the green, less than three feet tall And there’s possibly another one of similar stature more than 200 yards SSE. But what is this place? Is it prehistoric? Was it built in the Dark Ages? Medieval times? Does anyone have a clue!?
References:
Bennett, Paul, The Old Stones of Elmet, Capall Bann: Milverton 2001.
Burl, Aubrey, Four Posters: Bronze Age Stone Circles of Western Europe, BAR 195: Oxford 1988.
From Mytholmroyd, take the Cragg Vale road (B6138) up and up and up, until you get past the tree-level and the hills open up on either side of you. Take note of the farmhouse on the right-hand side of the road a half-mile on and park where you can. Walk down the track by the farmhouse (known as Washfold Road) and cross the stream at the bottom. OK – from here walk straight up the hill in front of you! (not along the footpath) In less than 100 yards it levels out and you’re onto the moorland proper. From here walk straight west for about 400 yards. If you deviate a little, don’t worry. You’ll see this small upright stone as you’re getting closer, seemingly in line with several other rocks, almost giving the impression you’ve come across a stone row. Good luck!
Archaeology & History
The slim upright
This small squat standing stone is just over three feet tall (1m), about 10 inches thick and 3½-feet across. Leaning at an angle into the ground, this broad but thin monolith has sunk some distance into the moorland peat.
It was located on February 15, 2011, in the company of Dave Hazell (pacemaker in tow!) on our first sojourn of the year. It hasn’t been mentioned in any previous surveys and aint in anyway what you’d call impressive. Nearby are the early remains of old walling north, east and west of here (one of them being a small enclosure of some type), for which I can again find no other references. What looks distinctly like the remains of a large cairn isn’t far away either. However, it may be that some of the remains up here are medieval in nature and it would be of benefit if someone who specializes in remains from that period could have a look here. The equally curious Turley Holes standing stones can be seen a half-mile northeast of here.
Best way here is, from Mytholmroyd go up the Cragg Vale road for a coupla miles, then turn right and heading down, then up, towards Withens Clough reservoir. Once there, walk onto the moor to your left (south) until you’re on the ridge above you. Keep walking until y’ see the rocky cairn-like creatures stood in isolation on a flat moorland plain.
Archaeology & History
Two Lads – on a dark, rainy, windy day
Truly weird spot this one, but I love it! Seemingly miles from anywhere, it’s one helluva walk to most folk, but utterly worthwhile when your arrive. On a clear day you can see for miles and the landscape is adorable! On a cloudy rainy day, the feel of the place changes if you take care to stay with the site, saturated, meditating (as no other people ever turn up when She’s like that – so you and the place get the best from each other!).
The site comprises of two boulders, each crowned with a cairn of stones. The westernmost one of the two (SD 98392 22111) is intriguing as it has, carved upon the rock beneath the stone cairn on the northwestern edge of the stone, what looks like a singular cup-marking, plus a large water-worn bowl on its northern edge, and a very distinct deeply-cut cross-base, several inches deep, near the northeastern corner of the rock. This cross-base seems slightly more rectangular in form than square; although the large covering of stones makes an accurate ascription difficult. If this cross-base and cup-markings are authentic, we would have here a clear example of the christianization of a previously heathen site.
A cursory examination of the easternmost of the Two Lads (SD 98397 22117) doesn’t indicate any artificial workings on the rock surface.
Two Lads on 1853 OS-map
Although the two ‘cairns’ on top of these two rocks are not prehistoric in nature, about 20 yards behind the Two Lads (south) may once have been the severely denuded remains of a once large prehistoric cairn. Although the position in the landscape is perfect for such a construction, this is somewhat tentative, it’s gotta be said! Further examinations are obviously necessary here.
The studious A.H. Smith (1961-63) believes that a field-name record from 1624, describing some ‘Lad Stones’ in the parish of Heptonstall relates to this site. We know with certainty however, that this site was first illustrated on Greenwood’s 1771 map of Yorkshire, then highlighted on more recent 19th century Ordnance Survey maps as ‘cairns.’
Folklore
Drawing of the Lads in 1877
The creation myth behind this place is that two lads were walking over the moor in midwinter and got caught in a blizzard. Losing all sense of visibility they tried to shelter from the wind and snow by hiding behind these rocks, but perished. Sometime later their bodies were found and the curious “cairn” of rocks were mounted onto the boulders to mark where they’d died. This is a folktale we find at many other old stone remains on the hilltops of northern England and Scotland.
The Two Lads seems to be very close to a midwinter alignment (or izzit a lunar standstill line?), linking it with the huge Rudstoop Standing Stone and, eventually, Robin Hood’s Penny Stone on Midgley Moor – which might be the root of the folktale. (i.e. midwinter, snow, death) Any archaeoastronomy buffs out there wanna check this one out? Then we can confirm or dismiss it.
References:
Anonymous, “The ‘Two Lads’, Withens Moor,” in Todmorden & Hebden Bridge Historical Almanack, T. Dawson: Todmorden 1877.
Bennett, Paul, The Old Stones of Elmet, Capall Bann: Milverton 2001.
Smith, A.H., The Place-Names of the West Riding of Yorkshire, Cambridge University Press 1961-63.
