“It could have been Illmington Spa not Leamington Spa” Newfoundwell, the forgotten chalybeate spring of Warwickshire
Leamington Spa is a well-known spa town, although its spa heritage is not capitalised much, however if only by a twist of fate or geography that the main spa town would be Leamington and not Ilmington spa. For not far from the Gloucestershire border is the village of Ilmington, a quiet sleepy village but once hopes were high for the settlement when in 1681 a plan was made to capitalise on a chalybeate spring found in the parish. Local legend tells that the Lord of the Manor, Henry Lord Capel, saw a local woman washing her eyes in the water of the spring and asked why. She said they eased her eyes and as a result he then contacted local physicians. It was publicised by Oxford Physicians Samuel Derham and William Cole. In their Hydrologia Philosophica or An Account of ILMINGTON WATERS the author describes it great details the qualities of the emerging potential spa. He notes after a lengthy background:
“Now I shall proceed to Enquire, what are the Ingredients of Ilmington Spaw, first taking notice of its Colour, which is far more pale then Rock-spring water. With Syrup of Violets it would turn green, like Alkalizate Liquors with that syrup: with Galls, to a Purple; like Martial Vitrioline Waters: for Cuprous Vitrioline with Galls turn muddy with a very little Purple or Black; but of this more afterwards. Its body being of a thick muddy consistence, I weighed (in a very dry Season) a Pint of this Spaw-water against a Pint of ordinary Water, but the Spaw exceeded near half a Drachm. Another time after a wet Season and when the Ocre was fallen an old Pint pot of common Pump-water weighing 18 Ounces did equalize (and if either, did turn the Scales) the same quantity of the Spaw-wa∣ter: which may caution us from prefixing a determinate Weight to any Spring-water. Variety in the Weight of Waters may appear by comparing That Salt spring water of Droitwich with sweet springs, yea to him that compareth the Waters of several sweet springs together, For the Esurine salt many times being carried along with the water sliding through its secret Meanders or veins of the Earth; of which part insinuateth itself into, and part corroding occurrent bodies; it fretteth off fragments, such as fragmenta ferrea from Iron-stones, and particles from ordinary stones, which are carried along with the water, and lie latent to the naked eye in its pores, but by Distillation, Evaporation &c. will appear, Whence of necessity followeth a great variety in weight, according to the greater or less quantity of sabulum or fragments therein contained.”
He then notes about the mineral properties. He continues:
“Then I proceeded to enquire after the Mineral, with which this Spring was impregnated. And first I took about half a pint of new milk, upon which in a Porringer I poured this water fresh from the Spring-head, but could not discern any coagulation; yea, for anything did appear, this mixture differed not from a mixture of milk and ordinary spring water. After four miles carriage of the water, when the reddish Ocre began to subside, I poured upon warm milk from the cow a pretty quantity of this water, and let it stand at least twelve hours; but neither in this mixture, nor in milk and this Spaw-water boiled together, did any Coagulum appear. Hence I began to suspect, that its brackish taste was not from an acid Salt; therefore on this spring-water I instilled some oyl of Tartar, but upon the instillation, and the standing of the water all night, a very small curdling did ensue; only the mixture looked more white than the Spaw-water itself, which alteration of colour proceeded from the oyl of Tartar. Whereupon I concluded, that no Acid salt was here predominant, yea rather as such, scarce discernable in this Spring; it being, as I shall hereafter prove, far nearer to an Alkali than to an Acid salt.”
After trying with galls, a common method of testing mineral waters, the author notes:
“Now considering the small quantity of Galls, with which a Pint of water was thus tinged, I believe we may compare our new found Spaw (in this particular) with any of the English Medicinal waters, yea with the German Spaws so much in request.”
One of the important aspects of promoting a new potential spa was to compare it to well-known others. The author notes:
“Besides, Aluminous Springs are purgative, witness the Scarbrough Spaw, Epsom and Barnet Waters, &c. but this near Ilmington worketh most what by Urine. Yea perhaps (and truly) I might conclude, That this Spaw in respect of its mineral ingredients worketh not by Siedge. I know it may be objected, That some persons drinking of this water do there upon find a loosness, perhaps to the number of four or five stools or more, To which I might answer, That any simple Spring-water drank in a large quantity, will purge by its own weight: for as it lyeth heavy upon the stomach and intestines it oppresseth Nature, whence the Peristaltick motion is excited to expell that which infests and is burdensome; and if the water doth much oppress the sto∣mach before it pass through the Pylorus, vomiting is the effect according to Dr. Willis. Besides that, Alum is an Acid, as I have al∣ready proved, and also is a Cathartick; both which properties are not to be found in this Spaw, comparatively more than in ordinary Spring-water. I observed also, that the Excrements of those that drank this water were turned blackish, which is a consequent to the taking of Chalibeat Medicines, but not to the drinking of Aluminous waters. But observing this Water after its being exposed to the open air for some time, either stagnating at the Spring-head, or else as it is set in open vessels hath a blewish Cremor swimming on the top or surface of the Water, much resembling waters that stand long upon sulphureous bogs; I began to enquire, whe∣ther this might not be a Sulphureous Spring, like that at Knarsbrough, &c. By an Analysis of this Water into its Principles, not one grain of combustible Sulphur is to be found.”
The new spa begun to popular, it was described by William Dugdale in his 1730 Antiquities of Warwickshire as:
“much frequented’ and of particular value for the treatment of ‘scrophulous and leprous cases”.
However, it would look like the visitors were not enough. The site attracted no well-known visitors, no royalty, no patronage of note and so within the same century the well fell out of favour. It went largely out of use about the time of the enclosure of the common fields in 1781. The Well House built to provide shelter for the users of the well, remained standing for another 80 years. Later the spring became a watering place for stock. In 1998 erosion of the bank of the pond revealed the worked stone. On recovery, it was found to be a sizeable fragment of the basin. This is now incorporated into a fountain a plaque on which reads:
“This is a fragment of a basin installed around 1682 by the Lord of the Manor, Lord Capel to collect water from the chalybeate spring known as Newfound Well. The spring (1/4 m NW of Ilmington on the path to Lower Larkstoke) was described by Dugdale (1730) as: “much frequented’ and of particular value for the treatment of ‘scrophulous and leprous cases”.
Today the site is a large oval shaped pool in fields above the village. Two plastic pipes in the western end of the pool pour copious amounts of water into it which flows beyond the path into a stream. On one side of the pond can be seen stone work which may be part of the bath house, if so it is unrecorded.
Standing on this remote quiet location it is difficult to imagine what the place could have been like if the spring had had more money poured into its development. One the county’s first spas, which ironically unlike its better known cousin still flows from its main source rather from a pipe!
Extracted from forthcoming Holy Wells and Healing Springs of Warwickshire