Burnt House Well, Tunbridge Wells, Kent

Healing Well (covered):  OS Grid Reference – TQ 6000 3963

Archaeology & History

Shown on early OS maps as a chalybeate spring, the denuded remains of this site can still be seen in Dunorlan Park, between the tearoom and the lake, where the spring can be seen on the left beneath a large tree.  It was first described in John Britton’s (1832) famous account of the area, who told us:

Site shown on 1872 map

“There is a spring, called Burnt House Spring, situated in a little dell, in a romantic spot to the right of the road leading from Tunbridge Wells to Pembury. It is a good chalybeate, and the iron is in a state of carbonate. This spring rises rapidly into a stone basin, placed in the centre of a circular excavation, about ten feet in diameter and six or eight feet deep, which is bricked round, and with the remains of stone steps leading down to the basin at the bottom. This spring, therefore, has clearly been, at some time, made use of as a medicinal water. It was accidentally discovered choked up with rubbish. The country about Tunbridge Wells abounds with springs of this character.”

The spring was cleaned up some time ago and its waters rise in a square stone-lined chamber—accessed by four stone steps—into a circular stone basin, before flowing down a short channel and into the drains.  I’ve no idea whether or not the water is still drinkable.

References:

  1. Britton, John, Descriptive Sketches of Tunbridge Wells and Calverley Estate, Longman: London 1832.

© Paul BennettThe Northern Antiquarian

Heugh Well, Blairgowrie, Perthshire

Healing Well:  OS Grid Reference – NO 17103 46984

Also Known as:

  1. Mineral Well

Archaeology & History

This little-known iron-bearing spring can still be found in the woodland known today as the Heugh of Mawse, a mile north of Blairgowrie.  It was included in the Object Name Book of 1863, where they referred to an earlier account in the New Statistical Account, which told that,

“On the south end of it is a chalybeate spring much resorted to by the people of the locality. “There are one or two chalybeate springs in the parish; but they have never been chemically analyzed. There is one very fine spring called the “Heugh Well” It springs from the face of the “Heughs of Mause” (a mortar cliff of singular appearance; which descends abruptly into the bed of the river with an almost perpendicular declivity of about 200 feet) and judging from its colour, contains a considerable quantity of ferruginous matter. The use of its water has been found to be very beneficial in cutaneous eruptions, & affections of the Stomach.””

Heugh Well on 1867 map

Subsequently highlighted on the 1867 OS-map, a singular footpath led to the site and no further.  It was mentioned by the regional historians J.G. McPherson (1885) and John MacDonald (1899), albeit briefly, where they respectively told that its waters were “formerly much resorted to by persons in the neighbourhood.”  It possessed considerable medicinal properties which, according to tradition, were “found very beneficial for skin diseases and derangement of the stomach”!  Doubtless such attributes will still be effective.

References:

  1. MacDonald, John A.R., The History of Blairgowrie, Advertiser Office: Blairgowrie 1899.
  2. McPherson, J.G., Strathmore: Past and Present, S. Cowan: Perth 1885.

© Paul BennettThe Northern Antiquarian

Redman’s Spa, Bingley Moor, West Yorkshire

Healing Well:  OS Grid Reference – SE 1159 4343

Also Known as:

  1. Redmire Spa
  2. Redmond’s Spa
  3. Richmond’s Spa

Getting Here

Redman’s Spa on 1851 map

From East Morton village, take the moorland road, east, and up the steep hill.  Where the road just about levels out there’s a right turn, plus (more importantly!) a trackway on your left which leads onto the moor.  Walk up this track for ⅔-mile until you get to the point where the moorland footpath splits, with one bending downhill to an old building, whilst the other smaller footpath continues on the flat to the north.  Go up here for 400 yards then walk off-path, right, for about about 150 yards.  But beware – it’s boggy as fuck!

Archaeology & History

On this featureless southern-side of Rombalds Moor, all but lost and hidden in the scraggle of rashies, a very boggy spring emerges somewhere hereabouts.  I say hereabouts, as the ground beneath you (if you can call it that!) is but a shallow swamp and its actual source is almost impossible to locate.  If you want to find the exact spot yourself, be prepared to put up with that familiar stench of bog-water that assaults our senses when we walk through this sort of terrain.  Few are those who do, I have found… But somewhere here, amidst this bog—and still shown on the OS-maps—is the opening of what is alternatively called Redman’s or Richmond’s Spa.  We don’t know exactly when it acquired its status as a spa-well, but the 18th century Halifax doctor, Thomas Garnett—who wrote the early work on the Horley Green Spa—appears to be the first person to describe it.  Garnett (1790) said how the place:

“was first mentioned to me by Mr W. Maud, surgeon, in Bradford, who went with me to see it.  It is situated on Romalds-moor, about two or three miles from Bingley, and goes by the name of Redmire-spaw.  The access to it is by no means good; the ground about it being very spongy and soft.  On the bottom and sides of the channel is deposited an ochrey matter, of a very fine, bright, yellow colour; and which I believe is used, by the country people in the neighbourhood, to paint their houses.  It sparkles when poured into a glass and has a taste very like the Tewit-well at High-Harrogate; which water it very much resembles in all its properties, and seems to be about the same strength… This water seems to hold a quantity of iron dissolved by means of fixed air.  Its taste is very pleasant; it is said to act very powerfully as a diuretic, when drank in considerable quantity, and may prove a useful remedy, in cases where good effects may be expected from chalybeates in very small doses; the fixed air, and even the pure water itself may be useful in some cases.  It is, however, necessary to drink it at the well, for it seems to lose its iron and fixed air very soon.”

I’ve drank this water, and believe me!—it doesn’t quite taste as pleasant as Mr Garnett espouses!  Its alright I s’ppose—but drinking water from a bog isn’t necessarily a good idea.  That aside, I find it intriguing to hear so much lore about such a little-known spring; and it is obvious that the reputation Garnett describes about this spa came almost entirely from the local people, who would have been visiting this site for countless centuries and who would know well its repute. Below the source of the well the land is known as Spa Flat, and slightly further away Spa Foot, where annual gatherings were once held at certain times of the year to celebrate the flowing of the waters.  Such social annual gatherings suggests that the waters here were known about before it acquired its status as a spa—which would make sense.  The remoteness of this water source to attract wealthy visitors (a prime function of Spa Wells) wouldn’t succeed and even when Garnett visited the place, he said how he had to travel a long distance to get here.

The origin of its name was pondered by the great Harry Speight (1898) who wondered if it derived from the ancient and knightly Redman family of Harewood, whose lands reached over here.  But he was unsure and it was merely a thought.  As an iron-bearing spring (a chalybeate) you’d think it might derive from being simply a red mire or bog (much like the Red Mire Well at Hebden Bridge), but its variant titles of apparent surnames casts doubt on this simple solution.

No one visits the place anymore.  Of the countless times I’ve wandered the moors, rare have been the times when I’ve seen folk anywhere near this old spring.  It is still coloured with the same virtues that Garnett described in the 18th century: the yellowish deposits, the boggy ground, much of which reaches to the truly dodgy Yellow Bog a short distance north and which should be completed avoided by ramblers after heavy rains (try it if y’ don’t believe me—but you’ve been warned!).

References:

  1. Garnett, Thomas, Experiments and Observations on the Horley-Green Spaw, near Halifax, George Nicholson: Bradford 1790.
  2. Short, Thomas, The Natural, Experimental and Medicinal History of the Mineral Waters of Derbyshire, Lincolnshire and Yorkshire, privately printed: London 1724.
  3. Speight, Harry, Chronicles and Stories of Old Bingley, Elliott Stock: London 1898.

© Paul BennettThe Northern Antiquarian


Mineral Well, Glen Lyon, Perthshire

Healing Well:  OS Grid Reference – NN 72110 47768

Also Known as:

  1. Iron Well

Getting Here

Mineral Well, Glen Lyon

From Fortingall village, head west and turn down into the incredible beauty that is Glen Lyon.  As you enter the trees, a half-mile along you pass the small gorge of MacGregor’s Leap in the river below.  2-300 yards pass this, keep your eyes peeled for an old small overgrown walled structure on the left-hand side of the road, barely above the road itself.  A large tree grows up above the tiny walled enclosure, within which are the unclear waters that trickle gently….

Archaeology & History

In previous centuries, this all-but-forgotten spring of water wasn’t just a medicinal spring, but was one of the countless sites where sympathetic magick was practised.  The old Highlanders would have had a name for the spirit residing at these waters, but it seems to have been lost.  The site is described in Alexander Stewart’s (1928) magnum opus on this stunning glen, where he wrote:

“Still a few yards more and Glenlyon’s famous mineral wishing well is seen gushing up, surrounded by its wall of rough stones now sadly in need of repair.  It has a stone shelf to receive the offerings of those who still retain a trace of superstition or like to uphold old customs as they partake of its waters.  The offerings usually consist of small pebbles, but occasionally something more valuable is found among them. The roadmen may clear that shelf as often as they like, but it is seldom empty for long.”

A local lady from Killin told us that she remembers the stone above the well still having offerings left on it 20-30 years ago. Hilary Wheater (1981) sketched it and called it the Iron Well.

Close-up of the waters (photo by Paul Hornby)
Hilary Wheater’s sketch

The waters in this small roadside well-house actually emerge some 50 yards up the steep hillside (recently deforested) and in parts have that distinct oily surface that typifies chalybeates, or iron-bearing springs – which this site is an example of.  Its medicinal properties would help to people with anaemia; to heal women just after childbirth; to aid those who’d been injured and lost blood; as well as to fortify the blood and stimulate the system.

Across the road from the well, Stewart (1928) told of a giant lime tree that was long known to be the meeting place for lovers (perhaps relating to the well?), and the name of the River Lyon here is the Poll-a-Chlaidheamh, or ‘the pool of the sword’, whose history and folklore fell prey to the ethnic cleansing of the english.

References:

  1. Stewart, Alexander, A Highland Parish, Alexander Maclaren: Glasgow 1928.
  2. Wheater, Hilary, Aberfeldy to Glenlyon, Appin Publications: Aberfeldy 1981.

© Paul BennettThe Northern Antiquarian


Airthrey Mineral Wells, Bridge of Allan, Stirlingshire

Healing Wells:  OS Grid Reference – NS 79504 97686

Also Known as:

  1. Airthrey Spa
  2. Airthrey Springs
  3. Bridge of Allan Spa
  4. Canmore ID 317260

Getting Here

Site shown on 1865 OS map

The old well-house is accessed easily.  From the main road of Henderson Street (or A9), that runs through the town, as you approach the main shopping area, go up Alexander Drive, then immediately turn right up Well Road. 100 yards up, take your first right again along Kenilworth Road and then first right up Mine Road.  100 yards or so along here, as you reach the tennis courts on your right, a small crumbly-tumbly building is to your left, just by the car-park to the hotel, with some old trees hiding its presence.  You can’t get into it and the waters therein sound to have fallen silent.

Archaeology & History

In 1761, the great writer Daniel Defoe in his Tour across Britain, found himself visiting a healing spring under the western reaches of the Ochils:

“Airthrey Well, two miles north of Stirling, flows from a mountain, where is a copper mine, with some mixture of gold; the water is very cold, and being tinctured with the minerals it flows through, is of use against outward distempers.”

Airthrey Wellhouse in ruins

Perhaps the earliest literary description of this site, the Bridge of Allan that we see today was little more than a stretch of old abodes, reaching into woodland above the crystal clear river and burns, chiming with countless fauna and that rich chorus of colours that pre-date the Industrialist’s ‘progress’.  The old hamlet was said by Robert Chambers (1827) to be “a confusion of straw-roofed cottages and rich massy trees; possessed of a bridge and a mill, together with kail-yards, bee-skeps, colleys, callants, and old inns.” But all of this was about to change.

In the old woods on the northwest slopes above the hamlet was indeed an old copper mine as Defoe described, and housed therein were a number of mineral springs–six of them according to the early reports of Forrest (1831) and Thomson. (1827)  They were obviously “known to the country people,” said Thomson, and had been “used by them as an occasional remedy for more than forty years”; although in Forrest’s very detailed account of these wells, he told how

“one of the old miners, an intelligent man and an enthusiastic admirer of the medicinal virtues of these waters, informs me, that they have been known for at least one hundred years.”

This comment was echoed a few years later when Charles Roger (1853) wrote his extensive book on the village.

It was in the 1790s when the mineral waters were channeled out of the mines for the first time, and Mr Forrest told that they were collected lower down the slope,

“in a wooden trough, for the use of the miners, and of the country people, some of whom used it as an aperient, whilst others, deeming the water impregnated with common salt merely, employed it for culinary purposes. …It was…much used as a medicine by the country people of the neighbourhood who attended regularly every Sunday morning to partake of it.”

Airthrey waters channeled along the long trough (Robert Mitchell 1831)

The fact that Sunday mornings was when people came here tell us that the Church had something to do with the timing; strongly implying that the wells possessed earlier indigenous traditions—probably similar to those practiced at the Christ’s Well, the Chapel Well and countless others across the country.  But written records on this are silent.

The main history of the Airthrey Springs is of them becoming famous Spa Wells and, much like Harrogate in Yorkshire, were responsible for the very growth of Bridge of Allan itself.  Oddly enough, this came about a few years after the copper mines were closed in 1807.  This wouldn’t have stopped some of the local people still getting into them and drinking the waters when needed—but the written records simply tell that, for a few years at least, their reputation faded.  Around the same time in the village of Dunblane, just a few miles to the north, another Spa Well had been discovered and it was attracting quite a lot of those rich wealthy types—bringing fame and money to the area.  As a result of this, the medicinal virtues of the Airthrey Springs were revived thanks to the attention of the local lord, a Mr Robert Abercromby, who thought that Bridge of Allan could gain a reputation of his own.  And so in the winter of 1821-22, Abercromby procured the research chemist Thomas Thompson to analyse the medicinal waters at Airthrey and have them compared with the ones at Dunblane.  He was in luck! Not only were they medicinal, they were incredibly medicinal!

Dr Thomson then wrote a series of articles in various academic journals in the early 19th century—each espousing, not just the health-giving property of the Airthrey waters, but lengthy chemical analyses outlining the active constituents.  To his considerable surprise he found that the Airthrey waters were as good as any of the great spa towns in England at Harrogate, Buxton, Bath and Leamington.  Their virtues were so good that Mr Forrest (1831) doubted any of the Spa Wells in England were as beneficial as the waters here!  R.M. Fergusson (1905) echoed this sentiment in his massive work on the adjacent parish of Logie, calling the Airthrey springs “the Queen of Scottish Spas”!—and these accolades prevailed long after Dr Thomson’s analyses.  He wrote:

“At Airthrey there are six springs containing, all of them, the same saline constituents, but differing a good deal in their relative strengths. I analyzed two of these during the winter of 1821-22, and the other four during the autumn of 1827.”

He found that, in varying degrees, the main constituents were salt, muriate of lime, sulphate of lime and muriate of magnesia. At that time, in medical circles, these ingredients were beauties!  As Mr Logie (1905) said:

“This mineral water has been for long distinguished as a specific for derangements of the stomach and liver, and skin and chest diseases, rheumatism, gout, sciatica, and nerve affections…”

Thomson’s initial findings were much to the liking of Mr Abercromby; for hereafter, he realised, all and sundry who could read and travel to the country spas in England and beyond, would visit Bridge of Allan and bring with it great trade.  So Abercromby quickly,

“caused the water of the two Springs analysed by Dr. Thomson, one of which was characterised by its strength, the other by its comparative weakness, to be carefully collected and conveyed apart in earthen pipes, to two stone troughs placed in a convenient situation, from which it was raised by two well-constructed forcing pumps. Over these pumps a commodious house was erected.

In 1822, several thousand copies of Dr. Thomson’s analyses were circulated; and the water acquired immediate celebrity.  Invalids from all parts of the country, but especially from Glasgow and its vicinity, resorted to Airthrey. Every house, in fact, in its neighbourhood, however mean and incommodious, was occupied by strangers; and so great was the popularity of the new springs that even in 1823 they threatened to supersede all the other same springs of Scotland.”

The success of these medicinal waters created the town itself and, unlike many other spa wells, this one continued to be used until the end of the 1950s.  Its demise came when, in one financial year, only two people came to “take the cure,” as it was called.

Side wall of ruined wellhouse

If you visit the well-house nowadays, it’s in rather poor condition and will be of little interest unless you’re a devout architectural fanatic.  It’s thought to be the earliest surviving building associated with this spa town, said by Mr Roger (1853) to have been built in 1821.  Shown on the first OS-map of the area, adjacent buildings were constructed to accommodate the overflow of people who came here.  And in the woodlands above, if you look around halfway up the slopes, an old trough has water running into it just by the side of a path.  This, say some local folk, is the trickling remains of the medicinal waters, still used occasionally by some people…

References:

  1. Durie, Alastair J., “Bridge of Allan: Queen of the Scottish Spas,” in Forth Naturalist & Historian, volume 16, 1993.
  2. Erskine, John, Guide to Bridge of Allan, Observer Press: Stirling: 1901.
  3. Fergusson, R. Menzies, Logie: A Parish History – 2 volumes, Alexander Gardner: Paisley 1905.
  4. Forrest, W.H., Report, Chemical and Medical, of the Airthrey Mineral Springs, John Hewit: Stirling 1831.
  5. Morris, Ruth & Frank, Scottish Healing Wells, Alethea: Sandy 1982.
  6. Roger, Charles, A Week at Bridge of Allan, Adam & Charles Black: Edinburgh 1853.
  7. Stewart, Peter G., Essay on the Dunblane Mineral Springs, Hewit: Dunblane 1839.
  8. Thomson, Thomas, “On the Mineral Waters of Scotland,” in Glasgow Medical Journal, volume 1, 1827.
  9. Turner, E.S., Taking the Cure, Michael Joseph: London 1967.

© Paul BennettThe Northern Antiquarian


Mineral Well, Dollar, Clackmannanshire

Healing Well:  OS Grid Reference – NS 9855 9804

Also Known as:

  1. Dollar Chalybeate Spring
  2. Dollar Spa
  3. Vicar’s Bridge Spa

Archaeology & History

Vicars Bridge spring on 1900 map

Somewhere hiding away above the north-side of the River Devon, just above the Vicar’s Bridge, a little-known healing well came into being following industrial workings in the glen in 1831 by a local iron-working company.  The waters were strongly chalybeate, or iron-bearing—and as the fad amongst the wealthy was, at the time, a love of Spa Wells, this mineral spring was broadcast as a competitor of the Harrogate and Bath Spas.  But it failed pretty fast, sadly.

Bottles of the water were marketed and sold as ‘Dollar Mineral Water’ in many of the large cities, but sales weren’t too good.  Johnston & Tullis (2003) pointed out how the waters would have been coloured like brandy; and despite it being good for anaemia, a good tonic, and favourable in treating cuts and bruises, the mineral spring was no longer of any value as a business, dying a quick death.  Local people still kept using the waters, but in recent years the spring appears to have died too.

References:

  1. Johnston, Tom & Tullis, Ramsay (eds.), Muckhart, Clackmannanshire: An Illustrated History of the Parish, MGAS 2003.
  2. Morris, Ruth & Frank, Scottish Healing Wells, Alethea: Sandy 1982.

© Paul Bennett, The Northern Antiquarian


Mineral Well, Portobello, Edinburgh, Midlothian

Healing Well (destroyed):  OS Grid Reference – NT 314 735

Archaeology & History

This was one of two medicinal springs that could once be found in old Portobello village. Like its companion Chalybeate Well nearly a mile northwest, in the early 19th century those entrepreneurial types tried fashioning these waters into being a Spa Well.  It didn’t really work and the fad passed after just a couple of decades—and soon after the local people had completely lost their water supply here.  The best historical account of it is in William Baird’s (1898) magnum opus on Portobello.  He told how the well,

“was, at the beginning of the century, situated in a garden near to the main road, where there was a well with drinking cups for the accommodation of visitors, a small sum being charged from those using it.  The supply here having in some way become interrupted the spring was neglected for a time. It found vent, however, lower down and nearer to the Promenade at the foot of Joppa Lane. About fifty years ago there was a pretty large open basin, in the centre of which the water bubbled up about half a foot. It was of a red brick colour. Unfortunately on the starting of a pump on the Niddrie Bum to drain the water from the Niddrie coal pits, the supply of water was again interrupted, and this excellent mineral spring, which was strongly impregnated with oxide of iron and sulphate of lime and magnesia, ceased to flow with its former fulness.”

In 1869, the Industrialists dug into the Earth to construct their promenade and, after countless centuries, the waters of this old medicinal well finally died and fell back into the deep Earth…

References:

  1. Baird, William, Annals of Duddingston and Portobello, Andrew Elliot: Edinburgh 1898.
  2. Bennett, Paul, Ancient and Holy Wells of Edinburgh, TNA: Alva 2017.

© Paul Bennett, The Northern Antiquarian