Make your way to the Black Beck tomb and walk west for some 50 yards. If the heather has grown any more than a foot tall, it’s impossible to see.
Archaeology & History
Near the northernmost section of the Hawksworth Shaw prehistoric graveyard, some 50 yards west of the Black Beck cairn, exists the remains of a small prehistoric enclosure whose walling is deeply embedded in the peat. Although I describe the place as an ‘enclosure’, we don’t know for certain whether it is a ruined settlement or large hut circles (although this latter idea is the more improbable).
Two large open arcs of walling—like large letter “C’s”—with their open sides to the east, have been constructed next to each other, virtually coming together in the shape of an inverted number “3”. The walling in the southern arc—measuring some 33 yards in length and barely higher than 1 foot above ground level—consists of standard stones and rubble, similar to some of the hut circles that are found in greater abundance on the north-side of Ilkley Moor. The smaller, less visible arc of stones—some 18 yards of it—is lower in the earth. Both lines of walling may have been robbed in part to construct some of the extensive cairns close by, as neither of the two arcs were very high and it was very difficult to work out even what sort of structure they might have been.
Like many other prehistoric sites on Rombalds Moor, only an excavation is going to tell us precisely what was going on here…
There are various ways to find this. When we came here, we started from the Barton and Crosland Moor side, parking up on Ivy Street and walking to the fields at the end of the road. From here, walk along the track to your left and just over 100 yards on there’s a small footpath on your right that veers down the slope. Walk on here for another 100 yards, keeping your eyes peeled for another path on your right that almost doubles-back on you, heading into the trees. Another fifty yards along and you’ll see some tell-tale stonework!
Archaeology & History
Highlighted on the 1854 OS-map, the site has seen better days. Although the waters today emerge from a blasted rock face and collect into a relatively modern round stone trough, there is a larger square stone structure just a few yards away that seems to have been where water was previously collected. According to local antiquarian Andy H, this was known to be a local Wishing Well in bygone times, but apart from this there are no literary accounts about the place. The area was decimated by 19th century Industrialists who, as is well known, destroyed much of our indigenous histories and sites—and the Huddersfield district was particularly hard hit by them.
On a recent visit to the site—in superb pouring rain!—the waters were choked with modern trash and bottles, making it unsafe to drink. This is surely a good case for renovation, then stuck on some local tourist route to ensure better, more appreciative attention.
Holy Well (destroyed): OS Grid Reference – TA 026 223
Archaeology & History
This curiously-named, lost holy well was to be found somewhere between the old terrace at West Field and the old road of West Acridge, but even when Henry Ball (1856) wrote about it, the site had passed into history. He told that,
“In the old enclosures to the west of the town was a spring of clear water called St. Trunnion’s well, and in a field in the West Acridge a very old thorn tree called St, Trunnion’s tree, which was standing in 1736; but who St. Trunnion was is not known…”
The close proximity of the tree with the well is highly likely. Throughout the British Isles there are many relationships where sacred trees and wells of the same name are next to each other and we have little reason to doubt this was the case here. However, unless local historians can uncover some old field-name maps, the exact location of the site seems to have been lost. It was named as St Tronians in 1665; with his sacred tree mentioned in early enclosure awards dated 1681 and 1697 respectively.
The enigmatic saint ‘Trunnion’ is thought to derive, not from some old hermit or heathen holy dood, but from the corruption of an early word: “a perversion of Trin-union or Tri-union, used as an asservation or oath”; although another option cited by Cameron (1991) is that it derives from “trinune, trin-une, referring to the Trinity”—which would explain the sanctification of the waters.
Holy Well (destroyed): OS Grid Reference – TA 032 222
Archaeology & History
Not far from the middle of this small town there lived, many centuries ago, a sacred spring of water dedicated to St. Catharine. Described in local field-names from 1697 (as St. Catherin’s Well), all trace of it has long since vanished. Indeed, even when Henry Ball (1856) wrote about it, local knowledge of it had already fallen into obscurity. He could merely tell us that,
“At the end of Newport, in what was called “the Colony,” was St. Catharine’s Well, and the road from thence to Finkle lane was named Catharine street.”
St Catharine’s festival date—known as Cattern Day in some parts of England—is November 25.
Easiest way to find this is from the Great Skirtful of Stones. From here, follow the line of the fence 250 yards south, then climb over and walk dead straight south onto Hawksworth Moor for 150 yards. You can clearly see the mass of reeds and marshy ground way before you reach it; just be very careful not to walk straight into the reeds or you’ll get sucked down into the waters—and it’s pretty dodgy if you walk into the wrong spot, with good old Jenny Greenteeth lurking beneath the surface!
Archaeology & History
Highlighted on the 1851 OS-map of the area, this all-but-forgotten clear spring emerges a short distance south of the Great Skirtful of Stones and adjacent to the Hawksworth Moor cairnfield—a proximity that was probably not without meaning in prehistoric times. Curious though it may sound, in traditional cultures across the world, water is as much an important ingredient in the cosmologies of the dead as it is in the land of the living. In earlier centuries this water-source was much more fast-flowing and wider than it is today and it would obviously have been vital for our prehistoric ancestors. Its virtues and folklore have long since been forgotten.
In William Addison’s (1951) standard work on the history and development of Spa Wells, he told us that “the spas began as holy wells”; yet in spite of him listing the Wigglesworth Spa in his work, such “holiness” wasn’t a feature found here and, sadly, we have no written records that tell of any. But that doesn’t mean to say it had no sense of importance or animistic sacrality to local people. The earliest written record we have of this Sulphur Well is to be seen on the stone-work at the top of the small well-house, where the year “1666” was carved, marking the year when the structure was built under the directions of a local rich dood. But earlier knowledge of these healing waters would have been passed to the land-owner by local people, as indicated in Thomas Short’s (1765) words where he told that “it has been used time out of mind.”
Mr Short (1724) makes mention of this Sulphur Well in his gigantic early work, but only in its similarity in both taste and smell to the Sulphur Well at Harrogate and letting us know that, “I have tried carefully” the waters of the two sites. We had to wait another forty years before he gave us a more detailed account of the medicinal properties here. He wrote,
“Now come we to a sulphur water of a very peculiar nature, such as I never met with or heard of in England besides, and deserves to be much more strictly examined and enquired into, viz. Wigglefworth Spaw, near Settle, in the parish of Long-Preston. It has been used time out of mind, and more formerly than at present, because it is little known; rains and drought affect it not. Country people drink four or five pints of it in a morning to vomit them, and six or seven pints to purge them. The water is very black, smells strong of sulphur, has a very small stream, but stagnates not, bubbles not, but springs up; it is always covered with a white scum, (and) dies all in its course white. It rises out of a great stone soil, near much lime-stone, at the foot of a hill. It tastes salt, yet curdles not soap, and boils with milk. A phial glass, one third part full of it, well corked, and tied down with a bladder, and set in the cold water to be evaporated; when the water began to boil, it was taken out and poured a little of it on solution of silver, which turned black and curdled. The phial was corked again, and set half an hour longer in the boiling water, it still turned solution of silver black. It was corked a third time, and set half an hour longer in the boiling water, then tried, but was not so black as before, and caused little curdling. This last stood all night, next day its precipitation was blackish; the water was clear above. This is the only blackish sulphur water I have met with (as Rippon is a greenish yellow) and retains its sulphur the longest, from its contained oil.”
Consistent with other writers of his time, Mr Short then wrote at length on how the Wigglesworth waters reacted to various chemical tests, many of which were done in order to indicate the veracity, or otherwise, of any medical qualities. He also made comparative studies between this and the sulphur wells at Harrogate and elsewhere, and concluded that the Wigglesworth Spa would successfully deal with the following ailments or conditions:
“Sloth, idleness, too violent slavish exercise or labour, too great affluence, or plenty of nourishing rich high foods, spices, forced meats, acrid, stimulant and aromatic viands; the earthy viscid dregs of fermented liquors, or the parching, drying, shriveling spirits of wine, sugar, fruits, grain, or fermented liquors, as well as poverty and unwholesome diet, irregular hours, etc, are the parents of many diseases, whose cure lies in relieving oppressed nature from the unwieldy load (brought upon her by indolence, gratifying the vitiated taste, intemperance and debaucheries) by cleansing and rousing the vessels, restoring the juices to a healthy state; rectifying and establishing the secretions and excretions of the body, and restoring vigour and activity to the fibres, vessels and solids. To the above causes of diseases, we may add pride, luxury, sensuality, inverting the natural course of time, turning day to night, and night to day. These give birth to many chronic diseases, as well as acute, from acidities, crudities, viscidities in the stomach, communicated thence to the bowels, and so to the whole habit; hence are vitiated juices, great obstructions, and a long train of diseases affecting sundry parts of the body, and therein the whole nervous system, with hypo, hysterics, melancholy, costiveness, or looseness, suppression of natural necessary discharges, etc., which require thinning, relaxing, resolving, opening, or invigorating remedies.”
For about two centuries this well had a very favourable reputation. It’s therefore slightly curious as to why the great spa-writer, A.B. Granville, in his visit to this part of Ribblesdale to seek out some of the medicinal springs in the 1830s (including a petrifying well), made no mention of our Sulphur Well. Whether this down to his patronizing attitude towards local people isn’t known, but it certainly wouldn’t have helped him in Yorkshire! One might suggest it was due to the fact that the spa had fallen into disuse, but this wasn’t the case as, subsequent to Granville’s visit, the local writer William Howson (1850) later told that,
“In the woody dingle to the north of the village is a sulphurous spring, protected by a neat and antique stone canopy bearing the date 1666, and the initials of Sir Richard Sherburne and Isabella his wife, a daughter of John Ingleby of Lawkland Hall. Of this well, Dr (John) Murray the well-known analytical chemist says, ” It is a most valuable and unusually strong sulphuretted water, and as far as I have examined mineral waters, second to none.” From his analysis and that of Dr. Garnett it appears that a gallon of the water contains seventeen cubic inches of sulphuretted hydrogen, four of azote, and a small portion of carbonic acid, sulphate of magnesia in the proportion of seventy five grains to a gallon, a considerable quantity of muriate of soda, and a minute proportion of carbonate of lime.”
(The aforementioned Dr Garnett was a renowned 18th century authority on medicinal wells in Yorkshire, best known for his works on the spa wells of Halifax (1791) and Harrogate (1791, 1792), along with some in Scotland.)
Messrs Short (1765) and Howson (1850) mentioned other medicinal springs very close by, including the Chalybeate Well in the field immediately north on the other side of the stream.
Addison, William, English Spas, Batsford: London 1951.
Brown, G.H., Walks, Drives and Excursions around Settle, Craven Printing: Settle 1880.
A mile south of Kislingbury village, just by the roadside is the old Hill Farm. In times gone by—as the early OS-maps show—a trackway led from here, westwards, for just a few hundred yards, until it reached the old farm of Hollowell Hill, all trace of which has long since gone. The farm owed its name to the existence of a holy well mentioned briefly in 14th century records in the Cartulary of St. Andrews, Northampton, where it was described as Halywellhille, or the Holy Well on a hill. All trace of it seems to have been lost. A ‘Spring’ that is shown on the 1885 map, a few hundred yards south of the old farm, seems to be the closest contender, but it seems more likely that the well was adjacent to, or beneath the farm-building.
Gover, J.E.B., Mawer, A. & Stenton, F.M., The Place-Names of Northamptonshire, Cambridge University Press 1975.
In Thomas Short’s (1765) description of the once-renowned Wigglesworth Sulphur Well, he mentioned briefly that there were “some (other) chalybeates near it.” Thankfully 85 years later, with the aid of William Howson (1850) who gave us a marginally better description, we were able to locate the whereabouts of one of them! From the Sulphur Well, this one could be found,
“two hundred yards above, on the other side of the rivulet there is a chalybeate spring, but (it was) of no unusual strength.”
In fact it’s a little closer to being 300 yards than 200—but that’s a minor issue in the grand scheme of things! The place in question was marked on the 1852 OS-map, marked simply as a “Well.” …This iron-bearing spring would have been a good pick-me-up and, as with all such wells of this nature, fortifies the blood and the immune system. Mr Howson also told us that “ferrugineous springs, stronger than this, are of frequent occurrence in the neighbourhood,” echoing Short’s earlier remark. Sadly, it seems that all trace of this Well has disappeared.
It’s a bittova pain-in-the-arse locating this site unless you’re into walking off-path, through excessive dense heather or burnt coarse ground. You can either follow the directions to the Black Beck tomb, or set off from Horncliffe Circle and walk up parallel to the fencing for nearly 300 yards (275m). From here, walk due east for nearly half a mile through the deep heather until you reach an overgrown track that keeps you eastwards towards a line of grouse butts abaat 275 yards (250m) on. Naathen, walk on the north-side of this path-track and for a few yards and you’ll begin to see either small piles of stones, or heather-covered mounds. Zig-zag about. You’re in the middle of the cemetery!
Archaeology & History
This cairnfield, or burial ground, or necropolis (choose whichever term you prefer) is a bittova beauty! Although some of the tombs here had been ‘officially’ noticed a few years back, the magnitude of it was understated to say the least. On a visit to the place a few months ago in the middle of one fuckova downpour, James Elkington and I found not only the large Black Beck tomb, but scattered clusters of many more cairns. But it wasn’t until a few weeks after that we got a longer time to check it over and, even then, I think the job was only half-done. So this site profile is merely an overview of some of what we found there. Along with the Black Beck tomb, we found more than thirty examples of prehistoric cairns—probably Bronze Age in nature—around the Hawksworth Shaw area near the middle of Hawksworth Moor, scattered around (seemingly) in no particular order.
Three types of cairns were identified in this large cairnfield. The majority of them are of the standard circular form, averaging 3-4 yards across and rising to about two feet high. They are of the same architectural form as those found in the Hawksworth Moor cairnfield 4-500 yards northwest of here (there is the possibility that the two of them are part of the same necropolis, but unless we can locate an unbroken continuity between the two groups, it’s best to present them as separate clusters). When we looked at them a couple of weeks ago, most cairns of the ’round’ type were overgrown, albeit in low growth, as a couple of the photos here show. The main cluster of the round cairns are just a few yards off the aforementioned track, but there are others scattered here and there at other points on this part of the moorland. A number of these cairns seem to have have been damaged and robbed of stones to build a line of grouse butts close by.
The second type of cairn in the necropolis—close to the main cluster of round cairns—are curious small, long cairns. Each one of them measures between 8-10 yards in length, are up to three yards across, and rise to a height of about one yard. They are built of the usual mass of small stones typical of the huge number of other cairns on Rombalds Moor, but have been constructed in an elongated form, in contrast to the more usual circular ones. Four of them are very close to each other with a fifth further away from this main group. A sixth one appears to be under the heather 50-60 yards away to the northeast. Unlike some of the nearby round cairns, this group looks as if it’s barely been touched by the hand of man, with only fallen scatters of stones around the outer edges of them. Tis an interesting group…
The third architectural cairn-types are scattered unevenly across the necropolis and are characterized as smaller, mini-versions of the round cairns, i.e, small piles of stones between 1-2 yards across and and just one or two feet high. Each of this type of cairn are more deeply embedded in the peat with more vegetational growth covering them due to their small size. This makes them much more difficult to see in comparison to their larger compatriots. One example (at SE 1423 4404) can be seen in the photo, above left, some 50-60 yards north of the Black Beck tomb; with another, above right, some 100 yards away to the southeast. There is the possibility they may be so-called ‘clearance cairns’, although I have some doubts about this and believe they are more likely to be individual graves…. but I could be wrong…
There’s little doubt that other tombs are hiding away in this area, waiting for fellow antiquarians to uncover them. Equally probable is the existence of hut circles or similar living-quarters lost beneath the heather. Two such sites have been found on recent ventures here: one a short distance west of the Black Beck tomb and another hiding away nearly 300 yards southwest, right beside the Black Beck. The main thing lacking up here are cup-and-ring stones. Apart from several uninspiring cup-marked rocks it seems few exist hereby; but there are, no doubt, some hiding away that have been hidden for millenia…
One final thing: the grid-reference given for this necropolis is based loosely on where some of the cairns can be found, but there are others whose positions lies slightly beyond that grid-ref, as you’ll find if you potter about.
Acknowledgements: With huge thanks, as always, for James Elkington for use of his photos. Also to the evolving megalith and landscape explorer Mackenzie Erichs; and to Linzi Mitchell, for additional input…
Probably the easiest way to find this is to use other sites as guides. From the Great Skirtful of Stones tomb, get over the fencing and follow it eastwards for exactly 500m (238 yards) where you’ll meet a small footpath on your right that goes southeast up the small slope of Craven Hall Hill and onto the moorland. Go along here for literally 0.2km (223 yards) and, just where the path bends slightly to the left, drop diagonally down the slope to where the moorland levels out close to the Craven Hall Hill (2) tumulus. From here walk WSW onto the flat moorland for literally ⅓-km (0.21 miles; 365 yards) where you’ll find either a large rounded mass of stones, or a large heather-covered mound—depending on whether there’s been a burning. Best o’ luck!
Archaeology & History
Very troublesome to locate when the heather’s fully grown, this large prehistoric tomb was uncovered very recently as a result of extensive moorland fires. It’s the largest such structure in a cluster of more than thirty cairns near the middle of Hawksworth Moor, many of which were rediscovered at the end of May, 2021. Due south of the Great Skirtful of Stones, this smaller skirtful of stones measures some 45 feet across and is more than three feet high in parts. Probably built in the Bronze Age, the tomb looks as if it’s been deliberately robbed at some time in the past, probably before the Victorians by the look of things—although only an excavation would tell us for sure. Primarily, the cairn has been robbed from its centre outwards mainly on its western side, where you’ll also see a small and rather dodgy cup-marked stone. Scattered into the surrounding peat are visible remains of where some of the loose stones have been cast.
A possible alternative to this being simply a large cairn, is that it’s a much-disturbed ring cairn. Some sections on the north and western edges give the impression that the mass of stones may be collapsed rubble walling. There are also a couple of internal features beneath the overgrowth of peat and compressed vegetation: one being a small circular piece of stonework that has either fallen in on itself, been dug into, or is the home of an animal; and a yard or two from this is what looks like another internal U-shaped stone structure – again, deeply encased by centuries of encroaching peat. But I must emphasize that these features are far from certain and can only be proven one way or the other by an excavation.
The site is well worth seeing, not only for its own merit, but also because of its place in a much wider prehistoric cemetery in the middle of Hawksworth Moor. There are at least six small single cairns (which may be clearance cairns) scattering this area—the closest of which from here is some 20 yards to the north. A more curious group of at least five small long cairns exist about 100 yards to the south; and below these is the largest cluster of standard tombs in the form of small round cairns. A curious D-shaped hut circle structure can be found less than 100 yards to the northwest, and what seems to be remains of a larger deeply embedded enclosure exists beyond the long cairns. Check ’em out!
Acknowledgements: With huge thanks, as always, for James Elkington for use of his photos. Also to the evolving megalith and landscape explorer Mackenzie Erichs; and to Linzi Mitchell, for additional stimuli…