England (north)

Sulphur Well, Wigglesworth, North Yorkshire

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Healing Well: OS Grid Reference – SD 8055 5677

Also Known as:

Spa Well
Wigglesworth Spa

Archaeology & History

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.

References:

Addison, William, English Spas, Batsford: London 1951.
Brown, G.H., Walks, Drives and Excursions around Settle, Craven Printing: Settle 1880.
Howson, William, An Illustrated Guide to the Curiosities of Craven, Whittaker: London 1850.
Short, Thomas, The Natural, Experimental and Medicinal History of the Mineral Waters of Derbyshire, Lincolnshire and Yorkshire, privately printed: London 1724.
Short, Thomas, A General Treatise on Various Cold Mineral Waters in England, privately printed: London 1765.
Anonymous, Water for Life, North Craven Building Preservation Trust 2010.

Acknowledgements: Many thanks to the North Craven Building Preservation Trust for use of their photo.

Chalybeate Well, Wigglesworth, North Yorkshire

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Healing Well (destroyed?): OS Grid Reference – SD 8047 5700

Archaeology & History

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.

References:

Howson, William, An Illustrated Guide to the Curiosities of Craven, Whittaker: London 1850.
Short, Thomas, A General Treatise on Various Cold Mineral Waters in England, privately printed: London 1765.

Hawksworth Shaw, Hawksworth Moor, West Yorkshire

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Cairnfield: OS Grid Reference – SE 143 439

Also Known as:

Hawksworth Moor cairnfield (2)

Getting Here

Curious small ‘long cairn’ (photo © James Elkington)

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.

Another ‘long cairn’ during an utter downpour!

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…

Small cairn, 50 yards N of Black Beck cairn

Small cairn 100 yard SE of Black Beck tomb (photo © James Elkington)

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…

Black Beck Tomb, Hawksworth Moor, West Yorkshire

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Cairn: OS Grid Reference – SE 14233 43987

Also Known as:

Small Skirtful of Stones

Getting Here

Old tomb looking east (photo © James Elkington)

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

…and looking NE (photo © James Elkington)

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 that 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.

Small Skirtful, looking S (photo © James Elkington)

Ring-cairn or just a cairn? (photo © James Elkington)

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!

Black Beck, Hawksworth Moor, West Yorkshire

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Hut Circle: OS Grid Reference – SE 1415 4401

Getting Here

Take the same directions as if you’re going to visit the Black Beck cairn. From here, walk through the heather northwest for about 60 yards. If the heather’s been cleared, you’ll see it low down, otherwise you’re pretty much screwed when it comes to finding this one!

Archaeology & History

Seemingly in isolation, this low-walled, D-shaped hut circle is presently the only the structure of its kind known to exist on this part of Hawksworth Moor; although to be honest we should expect there to be such structures in the area when we consider the size and proximity of the associated cairnfields immediately north and southeast of here.

NW section of walling; Black Beck tomb to rear

As with most hut circles, it’s nowt special to look at in all honesty. The south side of the structure is rubble walling typical of these structures, curving round as usual; but its more northern section straightens out, creating a D-shaped structure. This line of straight walling seems attached to another, outer parallel wall 3 feet away, creating its very outer edge. The rubble walls themselves average three feet across; whilst the hut circle measures 6-7 yards across. We assume that it was constructed during the same period as the adjacent prehistoric necropolis.

Dragon Well, Eccleshill, Bradford, West Yorkshire

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Sacred Well (destroyed): OS Grid Reference – SE 17567 35473

Also Known as:

Pendragon Well

Archaeology & History

A most curious place: this ‘Well of the Dragon’ as it was first called (on the 1852 OS-map) and subsequently the ‘Pendragon Well’ (on the 1922 map) just off Pendragon Lane, seems to have been forgotten in both folklore and history. I grew up round here and no legends of dragons were known, either in my life, nor that of the old folks I knew; nor any pub of that name that might account for it.

Equally unexplained is the name of the adjacent ‘Pendragon Lane’, which has been known as that for some 175 years. We have no Arthurian myths anywhere in West Yorkshire that remains in folk memory—and certainly nothing hereby that accounts for it.

As for possible landscape associations (i.e., serpentine geological features), nothing in the vicinity has any bearing on the name. Indeed, the only thing of any potential relevance was the former existence of a healing rock known as the Wart Stone, some 100 yards to the east at Bolton Junction. Such stones are usually possessed of naturally-worn ‘bowls’ of some sort on top of the rock—akin to large cup-markings—into which water collected that was used to rid the sufferer of warts or similar skin afflictions. But such an association seems very unlikely.

The only thing we can say of this Dragon Well is that probably, in times gone by, a folktale or legend existed of a dragon in the neighbourhood that had some association with the waters here. Dragons are invariably related to early animistic creation myths, and this site may have been all that remained of such a forgotten tale. The nearest other place in West Yorkshire with dragon associations is six miles northwest of here on the south-side of Ilkley Moor. In Britain there are a number of other Dragon Wells, the closest of which is in South Yorkshire.

St Peter’s Well (1), Leeds, West Yorkshire

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Holy Well (destroyed): OS Grid Reference – SE 2894 3382

Archaeology & History

Not to be confused with the other St. Peter’s Well that once existed in the city centre, this site was shown on an 1815 map of Leeds (which I’ve not been able to get mi hands on!), known as the Waterloo Map. But when the Ordnance Survey lads visited the place in 1846, it had been covered over. Immediately west of here, the saint’s name was also given to a nearby hill, whose folklore seems has been forgotten.

Although Ralph Thoresby mentioned it in passing, Edward Parsons (1834) gave us a brief description of its qualities, telling us that,

“Near North Hall is the celebrated spring called St. Peter’s Well ; the waters are so intensely cold that they have long been considered very efficacious in rheumatic disorders.”

Bonser (1979) reiterated this in his survey, also telling that, like its nearby namesake, its waters were “intensely cold and beneficial for rheumatism, rickets, etc.” An old bathing-house that was “annexed to the Well” may have been used specifically to treat such ailments, but we cannot say for sure.

Interestingly, Andrea Smith (1982) told that 400 metres away a well was sunk in 1838 and a quantity of petrified hazelnuts were recovered from a broken red jar which had a female head painted on it. Such a deposit is not too unusual, as a number of sacred wells in bygone days were blessed with nuts and signified the deity Callirius, known by the Romans as Silvanus, the God of the Hazel Wood – though we have no direct tradition here linking St. Peter’s Well with this ritual deposit.

St. Peter’s festival date was June 29.

References:

Bonser, K.J., “Spas, Wells and Springs of Leeds,” in The Thoresby Miscellany – volume 54, Leeds 1979.
Hope, Robert Charles, Legendary Lore of the Holy Wells of England, Elliott Stock: London 1893.
Parsons, Edward, The Civil, Ecclesiastical, Literary, Commercial and Miscellaneous History of Leeds, Halifax, Huddersfield, Bradford, Wakefield, Dewsbury, Otley – volume 1, Frederick Hobson: Leeds 1834.
Smith, Andrea, ‘Holy Wells Around Leeds, Bradford & Pontefract,’ in Wakefield Historical Journal 9, 1982.
Thoresby, Ralph, Ducatus Leodiensis, Maurice Atkins: London 1715.

St. Pancras’ Well, Scampton, Lincolnshire

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Holy Well (destroyed): OS Grid reference – SK 9542 7853

Archaeology & History

Mentioned in Thompson’s (1999) survey but without comment, it was, curiously, Skyring Walters’ (1928) that drew my attention to this site. He added it to his list of St Pancras sites, telling how even in his day, it had fallen into memory. Indeed, it had already gone when the Ordnance Survey lads came here in 1885. Thankfully we were left with an albeit piecemeal account of the place by Cayley Illingworth (1810) before its destruction. It was an iron-bearing well that existed some fifty yards from an ancient Roman villa and was probably the water supply for the Romans who lived here. He told us:

“The circumstance…of the chalybeate spring within a few yards from the entrance of the villa, and still called Saint Pancras Well…favours the conclusion of a chapel having been erected on its site. (This) is supported by the strong evidence of a discovery, upon record, that a chapel dedicated to Saint Pancras did actually exist on this spot, so early as the beginning of the twelfth century; about which period Richard Fitz-Robert of Scampton gave to the monastery of Kirksted three selions of land in that lordship, two of which are described in the gift as lying in the south field, on the south side of the chapel of Saint Pancras.”

He further told that at the bottom of the well an oak floor had been laid, which had been dug up “several years ago.”

St Pancras’s festival date is April 3.

References:

Cameron, Kenneth & Insley, John, The Place-Names of Lincolnshire – volume 7, English Place-Name Society: Nottingham 2010.
Harte, Jeremy, English Holy Wells: A Sourcebook – volume 2, Heart of Albion Press: Loughborough 2008.
Illingworth, Cayley, A Topographical Account of the Parish of Scampton in the County of Lincoln, T. Cadel & W. Davies: London 1810.
Thompson, Ian, Lincolnshire Springs and Well, Bluestone: Scunthorpe 1999.
Walters, R.C. S., The Ancient Wells, Springs and Holy Wells of Gloucestershire, St Stephens Press: Bristol 1928.

Craven Hall Hill (2), Hawksworth Moor, West Yorkshire

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Ring Cairn: OS Grid Reference – SE 14574 44098

Getting Here

Unless the heather’s been burnt back, this takes a bitta finding. Direction-wise, the easiest is from the moorland road above Menston. Go up Moor Lane and then turn right along Hillings Lane. 350 yards on is a dirt-track on your right marked as Public Footpath. Walk up here for two-thirds of a mile—going past where the track goes left to the Shooting Range—to where the track splits. Bear left and after 250 yards you reach a fence on your left where the moorland proper begins. Follow this fence SW for 300 yards until it does a right angle turn. Just before this, you’ll see a large worn overgrown trackway or path running north into the moorland. Walk up here for nearly 100 yards and look around. Best o’ luck!

Archaeology & History

Shown on the 1851 OS-map adjacent to the long prehistoric trackway that runs past Roms Law, the Great Skirtful and other prehistoric sites, the antiquarian wanderings of Forrest & Grainge (1868) came past here and, although didn’t mention the Craven Hall cairns directly, they did write of “a group of barrows” hereabouts, and this may have been one of them. James Wardell (1869) gave an even more fleeting skip, only mentioning “pit dwellings” hereby. A little closer to certainty was the literary attention Collyer & Turner’s (1885) pen gave, where they described, “near the adjoining old trackway, which runs from East to West, will be seen a small barrow”—but this could be either of the Craven Hill sites. And the usually brilliant Harry Speight (1900) gave the place only more brevity….

Structurally similar to Roms Law nearly ¾-mile northwest of here, this little-known and much denuded prehistoric tomb has seen better days. It is barely visible even when the heather’s low—and when we visited recently, the heather was indeed low but, as the photos here indicate, it’s troublesome to see. It’s better, of course, with the naked eye.

It’s the most easterly cairn in the large Bronze Age necropolis (burial ground) on Hawksworth Moor. Measuring some 12 yards across and roughly circular in form, the ring is comprised mainly of many small stones compacted with peat, creating a raised embankment barely two feet high above the heath and about a yard across on average. A number of larger stones can be seen when you walk around the ring, but they don’t appear to have any uniformity in layout such as found at the more traditional stone circles. However, only an excavation will tell us if there was ever any deliberate positioning of these larger stones. It would also tell us if there was ever a burial or cremation here, but the interior of the ring has been dug out, seemingly a century or two ago…

References:

Collyer, Robert & Turner, J.H., Ilkley: Ancient and Modern, William Walker: Otley 1885.
Faull, M.L. & Moorhouse, S.A. (eds.), West Yorkshire: An Archaeological Guide to AD 1500 – volume 1, WYMCC: Wakefield 1981.
Forrest, C. & Grainge, William, A Ramble on Rumbald’s Moor, among the Rocks, Idols and Altars of the Ancient Druids in the Spring of 1869, H. Kelly: Wakefield 1868.
Speight, Harry, Upper Wharfedale, Elliott Stock: London 1900.
Wardell, James, Historical Notes of Ilkley, Rombald’s Moor, Baildon Common, and other Matters of the British and Roman Periods, Joseph Dodgson: Leeds 1869.

Hough Hill, Bramley, Leeds, West Yorkshire

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Tumulus (destroyed): OS Grid Reference – SE 234 336

Archaeology & History

Today, Hough Hill has almost completely given way to modern housing; but in bygone centuries, this hilltop once housed a prehistoric burial mound—albeit an inconspicuous one. It was mentioned briefly in Faull & Morehouse’s (1981) magnum opus, but we know very little of its overall appearance and stature. Its existence was recorded posthumously thanks to the antiquarian John Holmes, without whose notes it would have been lost to history.

During quarrying operations at Hough Hill in December 1879, an ornamental urn was found,

“filled with calcined bones (that) was placed on a dish shaped hollow, some two or three feet deep, with charcoal and burnt earth.”

Holmes compared some markings that were upon this urn to one that was uncovered in Acrehowe Hill above Baildon by J.N.M. Coll in 1845. Unfortunately the Hough Hill urn was broken into fragments shortly after being uncovered. All remains of the burial mound have been completely destroyed.

References:

Faull, M.L. & Moorhouse, S.A. (eds.), West Yorkshire: An Archaeological Guide to AD 1500 – volume 1, WYMCC: Wakefield 1981.
Holmes. John, “A Sketch of the Pre-Historic Remains of Rombalds Moor,” in Proceedings of the Yorkshire Geological & Polytechnic Society, volume 9, 1886.
Wardell, James, Historical Notes of Ilkley, Rombald’s Moor, Baildon Common, and other Matters of the British and Roman Periods, Joseph Dodgson: Leeds 1869. (2nd edition 1881).