From Blubberhouses church by the crossroads, walk up the slope (south) as if you’re going to Askwith, for 100 yards or so, taking the track and footpath past the Manor House and onto the moor. Once you hit the moorland proper, take the footpath that bears left going down into heather and keep going till you hit the dead straight Roman Road path running west onto Blubberhouses Moor. Go on here for nearly a mile until you hit the stream and nearby Eagle Stone boulder. Walk upstream from here, on its eastern (right-hand) side for 100 yards, then walk up onto the level moor, scattered with rushes. Keep up here, heading towards the upright cairn open the skyline to the north. Once here, walk 80 yards (73m) WNW and you’ll note a number of flat stones embedded in the heather around you. You’re damn close!
Archaeology & History
Off-path and takes some finding and will all-but disappear when the heather grows back, so this one’s probably only for the purists amongst you. But I like it anyway! This is one of at least seven newly-discovered cup-marked stones hereby, including the nearby ‘Owl Stone’ with it’s big eyes! There are just two cup-marks on the flat surface: one an archetypal large cup 3 inches across and a half-inch deep; the other, a small faint cup less than 2 inches wide and very shallow which is easily missed if you pay little attention. On the photo here, the fainter cup is slightly above right of the centre. The carving appears to be on the far eastern edges of the Slade Cairnfield. Other undiscovered remains are likely to be found here.
Follow the directions to reach the Lippersley Pike cup-marked stone, then keep walking westwards, but go up the slope immediately on your right (north) and walk upwards along the path to the notable stone structure at the top-end of the ridge a coupla hundred yards ahead. Once there, you’re standing on it!
Archaeology & History
Lippersley Pike & shooter’s butt
A little known site with some excellent 360° views all round, reaching as far west as Pendle Hill, north past Simon’s Seat, and east onto the far reaches of the North York Moors. The landscape here is truly superb! And humans have been here since, it would seem, mesolithic periods at least, if Cowling’s finds are owt to go by! For although he described the much denuded tomb that we can still see under the herbage and recently-built shelter, there was also, “on the northern slope…a small occupation immediately below the summit on the northern side.” We found remains of it on our visit here the other day. But of the tomb itself — which Mr Cowling thought was neolithic in age — he wrote:
“The highest point of Lippersley Pike, on Denton Moor, is crowned by a stone cairn 1083 feet above sea level, and overlooks, on the northern side, a small site which appears to have been occupied by the ‘Broad Blade’ people, for there occur several pieces of patinated flint, along with scrapers and worked blades.”
Aerial view of Lippersley Pike
Cowling then describes a number of flints and other prehistoric working utensils that he found all round here. The remains of the cairn measure some 25 feet east-west and 23 feet north-south. There has been no excavation here, although the fella’s who dug out much of the stone to build the shooter’s butt on its top may have found summat, but have kept it quiet!
The cairn is an ancient marker along the boundary line marking the townships of Denton and Great Timble and was visited in perambulation walks in previous centuries. Grainge (1871) describes the extensive perambulation in his Knaresborough Forest work. ‘Lippersley’ itself first appears in records from 1576, although A.H. Smith (1963:5) does not suggest an etymology. The place is worth visiting as a good starting point to explore the other little-known prehistoric remains on these moors, including the Crow Well settlement, the Heligar Pike tomb, etc, etc.
References:
Cowling, E.T., Rombald’s Way: A Prehistory of Mid-Wharfedale, William Walker: Otley 1946.
Grainge, William, The History and Topography of Harrogate and the Forest of Knaresborough, John Russell Smith: London 1871.
Grainge, William, The History and Topography of the Townships of Little Timble, Great Timble and the Hamlet of Snowden, William Walker: Otley 1895.
Smith, A.H., The Place-Names of the West Riding of Yorkshire – volume 5, Cambridge University Press 1963.
John Dixon took a bunch of us on a pleasant amble here via the Fair Oak Circle site. From Fair Oak, go round the back of the farm and past the small cluster of hidden cottages, then bear right down the dirt-track and up the slope, then cross the field in front of you, going over the stile, following the footpath round the eastern edge of the slightly limestone New Laund Hill, and down again, thru the gate. From here, head diagonally across the field 150 yards towards the fencing at the woodland edge. Over the fence, into the trees, head halfway down the steep-ish slope and keep your eyes peeled for the rocky outcrop nearly halfway down. Alternatively, an easier way here is apparently from the Inn at Whitewell. Go across the river via the stepping stones (or wade!) and follow the footpath uphill towards a farm, where you’ll find a large steel gate on the left that leads into the woods. Here there are 2 paths: follow the higher of the two until it starts bearing to the right. Once here, look up the hill to the right you’ll see the rock outcrop. The caves are there!
Archaeology & History
Smaller Fairy Hole
There are at least 3 caves here, close to each other along the edge of the small footpath a few yards apart. The small rounded entrance of the northernmost one (photo, right) is reported by English Heritage to have had no human remains found therein, but further investigation is required here. The main cave however is where intriguing prehistoric finds were located. It appears that the entrance was deliberately built-up and blocked by stone walling a few yards inwards, giving the remains found therein a state of protection and sanctity. Writer and historian John Dixon (2004) tells what was in the cave:
“In 1946, an excavation was carried out on the site by the archaeologist Reginald C. Musson. In front of the larger cave is a flat platform on which evidence of Bronze Age daily life was found. This included animal bones, a pebble pounder (used to extract marrow from bones) and shards of a food vessel.
“All that survived of this tripartite collared urn was a large rim-collar shard, two fragments displaying neck/shoulder/body elements and five smaller pieces, probably from the base of the body. This is the only collared urn to have been found in a cave in Lancashire. Its tripartite Pennine form assigns it to an early Bronze Age date.”
The main Fairy HolePlan of cave chamber (after J.Dixon 2004)
The artificial walled entrance may not merely have been an ingredient giving sanctity to the place, but this could well have been a site for ritual shamanic practices, including prolonged rites of passage and death rituals (authentic ones, not the modern pagan nonsense). The ‘ritual death’ elements are highly probable here for, as John Michell (1975) told, caverns and crevasses are “most responsive to the necromancer’s invocation”. It’s geomancy, spirit association and the archaeological finds therein are strongly suggestive of this usage. (Eliade 1989, 1995; Maringer 1960, etc) Bearing this in mind, it is of some concern regarding the individual who thought it wise to spray-paint his name against the wall of the cave entrance (see photo); for many are those even in these days of shallow minds who fall prey to the car-crashes and creeping madness brought upon themselves by desecrating ancestral sites of ritual magick. It would be intriguing to keep a prolonged eye on the ‘Forsh’ who painted his ego in this cave of dead spirits…
Folklore
Not surprisingly, the little people hold legend here. Jessica Lofthouse (1946) found tales of these ancient peoples in several places close by, but at the Fairy Caves specifically,
“everyone knew that these little caves in the limestone at Whitewell were the homes of the little folk.”
…And in relation to the ingredient mentioned above, about ritual use of the cave in ancient times: are there any serious ritual magickians who’ve spent time working in this cave, overnight or longer, and who can let us know of their encounters here? (long shot, I know – but it’s worth asking, considering the probable use of the place) Or perhaps spontaneous encounters of other people here…
Very close to the once impressive Dorchester Cursus, this double-ringed prehistoric monument can no longer be seen thanks to the self-righteous arrogance of modern industrialists who care little for the ancestral monuments of the British people, destroying all traces of the site — an activity which, in this case, astonishingly started in more ancient times, as Jean Cook (1985) told: “The banks and the ditches had been levelled through agricultural activity, possibly in the Iron Age”!
Big Rings ground-plan1938 photo of the Big Rings, by Major George Allen
The destruction of this environment continues to this day, destroying many important archaeological remains with little care. Thankfully we we’ve got a good account of the site due to the archaeological excavations of R.J.C. Atkinson (1951) and his team in the late-1940s, from whom Cook and just about everyone else gets most of their data regarding the site.
The Big Rings Henge was probably built sometime in the middle of the second millenium BC. It was an important prehistoric ritual site and, most likely, had some relevance to the adjacent cursus monument. A number of important mortuary and ritual sites were also built close to the site over a period of nearly two thousand years, showing the importance this landscape had to our ancestors.
Jean Cook (1985) described the Big Rings henge as follows:
“The ditches, of which there were two, had opposed entrances on the NNW and SSE. They were about 7.6m wide and 1.8m deep with flat bottoms. Originally there seems to have been a broad low bank on the inner side of each ditch. The southern entrance incorporated an existing monument, consisting of a ring ditch which enclosed a large four-post setting and contained a cremation and a stone axe. Just outside the north entrance was a round barrow, containing a central oval burial pit which produced a crouched inhumation, together with a well-preserved beaker, two small copper or bronze knives and a rectangular wrist-guard of greenstone. The Big Rings ditches themselves contained pottery belonging to the middle or late Beaker period. Although the area within the ditches was trenched, there was no evidence of internal timber structures.”
References:
Atkinson, R.J.C., “The Henge Monuments of Great Britain,” in Atkinson, Piggott & Sandars’ Excavations at Dorchester, Oxon (Department of Antiquities: Oxford 1951).
Atkinson, R.J.C., Piggott, C.M. & Sandars, N.K., Excavations at Dorchester, Oxon, Department of Antiquities: Oxford 1951.
Cook, Jean, “The Earliest Evidence,” in Dorchester through the Ages, Oxford University 1985.
Harding, A.F., Henge Monuments and Related Sites of Great Britain, BAR 175: Oxford 1987.
Harding, Jan, The Henge Monuments of the British Isles, Tempus: Stroud 2003.
Wainwright, Geoffrey J., The Henge Monuments: Ceremony and Society in Prehistoric Britain, Thames & Hudson: London 1989.
The sites that were once here have long since been destroyed as a result of quarrying operations. But thankfully this place was given a quick appraisal by those renowned Scottish archaeologists, Anna Ritchie and D.V. Clarke, before final destruction. They recorded the site in an early edition of Discovery & Excavation in Scotland:
“Two short cists were discovered in November, 1970, during the removal of a long low gravel ridge protruding into the flood plain of the River Clyde. The two cists were both aligned NE-SW and were 14m apart. Both employed identical construction techniques. The side slabs overlapped both end slabs and the N end slab was shorter than the other three slabs, necessitating a building-up of the floor by some 30cm. Both appear to have had a double layer of capstones although this is uncertain in one case. The cists contained and adult and child without grave goods on a gravel floor in one, and an adult with a beaker on a ‘crazy-paving’ floor in the other.”
Crazy-paving in prehistoric times sounds good! The Scots got there first!
References:
Clarke, D.V. & Ritchie, Anna, “Boatbridge Quarry: Short Cists,” in Discovery & Excavation in Scotland, 1971.
There’s no footpath to this site, but we came to it via the car park on Coolham Lane on the southeast side of Earby. Walking uphill, we got over the wooden stile on the moorside and walked up the side of the walling, all the way upwards till we reached the top of the moor. You’ll pass the large Bleara Moor tumulus just by the walling, then head towards the rounded hillock on the top of the moor a coupla hundred yards away. Y’ can’t really miss it!
Archaeology & History
As with many sites in this area, very little has been said of this usually overgrown Bronze Age burial mound. Although no known recorded excavation of the tomb has ever been done, someone dug into the top of the mound in the 1960s, but we have no record of any finds. The tomb stands on the local boundary line between Earby and Lothersdale to the east and was known as ‘Bleara Haugh’ in the 1819 Enclosure Act. But little else has ever been said of it.
Bleara LoweOS-map of site
When we visited the place a few months ago, we were fortunate in that the heather had been burnt back, so allowing a much better view of the site than normally afforded when it’s covered in heather. The rounded mound was between 4 and 5 feet high and measured approximately 20 yards across. The pit which had been dug into the top of the mound was still visible, though much overgrown. The view from the tomb itself was very impressive — which would have been of some importance in the construction of the place. The Pastscape website describes Bleara Lowe as:
“A slightly oval mound of peat and heather-covered stones up to 1.4m high with max dimensions of 21m E-W x 19m N-S. There is a rectangular hollow 3m x 1.5m x 0.4m deep on the cairn’s summit.”
Another larger tumulus or overgrown cairn can be found over 200 yards west of here; plus a number of small singular prehistoric cairns have been located further down the western slope of the moor, known as the Bleara Moor Cairnfield. None of these sites have ever been excavated.
The Hades hill cairn/barrow is located high on the moors some 3 miles north-east of Whitworth and the smaller village of Facit, near Rochdale. Its exact location is close to a footpath halfway between Hades hill and Rough hill, though it is not mentioned on modern OS maps. It is quite difficult to get to so be ready for a long hard walk.
Archaeology & History
This small, low barrow or cairn — a couple of miles north of the little-known Man Stone — measures 15 metres north to south, 13 metres east to west and is 0.9 metres high (about 3 feet in height). But not a great deal can be seen today.
It was excavated in 1898 when a number of artefacts were discovered near the centre of the barrow. The most famous of these ancient artefacts was a Celtic two-tiered urn (of the Pennine type) which had rope imprints and chevrons; inside this urn were the burnt bones of a female, flints, a scraper and a fine pointed borer. Other stuff that came out of the barrow included animal bones, charcoal, flint implements and an arrow head. The urn was placed in the hands of The March Collection at The Rochdale Free Library (now known as Touchstones). A more recent excavation was carried out in 1982 but nothing was recorded at this time. In Dr Whitaker’s History of Whalley, he described there being “the remains of a large beacon, with the foundations of a large circular enclosure” on Hades Hill.
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.
…to be continued…
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.
