cases) cutting off the very

source of the materies morbi, but also (when there) by eliminating it from the system by the great emunctories, viz., the skin, kidneys, lungs, and bowels.  As the large proportion of invalid visitors to Buxton consist of those suffering from the uric acid or gouty diathesis, and rheumatism, and seek relief from the excruciating pains and cripplement incident to such diseases, the great attraction must of necessity be the medicinal waters, of which there are two kinds—the cold chalybeate or iron spring, and the natural thermal water.  Of the former there are numerous springs in the neighbourhood of Buxton, but the only one now resorted to has been conveyed through pipes from a distance to a room adjoining the natural baths, and is used with much benefit in many forms of uterine disease as a douche.  As such also it is prescribed in cases where the conjunctivæ are in a relaxed condition, consequent either upon rheumatic inflammation or local injuries.  It should on no account be applied to the eyes until the inflammatory action has entirely subsided.

When drunk, one tumbler (twice or thrice daily after meals) may be taken by an adult with much advantage when suffering from anæmia, chlorosis, amenorrhœa, dysmenorrhœa, diabetes connected with the gouty diathesis, chronic cystitis, or general debility.

Although it may be classed as a mild chalybeate, I have frequently seen great benefit derived from its internal use (partly, no doubt, owing to the presence of sulphate of lime), especially in children of an undoubtedly strumous habit, where glandular swellings presented themselves in the neck, and the mesenteric glands were enlarged.  In such cases, when taken regularly for some weeks (half a tumbler thrice daily after meals), the appetite returns, the digestive functions are improved, the glandular swellings subside, and the whole system becomes reinvigorated, so as to restore bloom to the cheek, brilliancy to the eyes, vigour to the limbs, and the natural buoyancy of spirit to childhood.

According to Dr. L. Playfair’s analysis in 1852,

one gallon of the water was found to contain the following solid constituents:—

The thermal water, as before stated, arises from various fissures in the limestone rock, upon which formation the greater part of the town of Buxton is built.  The flow is uniform (during the heat and drought of summer, and the cold and frost of winter) in volume, about 140 gallons per minute, in temperature 82 deg.  Fahrenheit, and in solid constituents.

According to the latest analysis, made by Dr. Thresh in 1881, the following results were obtained.  The mud which had settled around the mouths of the springs and floors of the tanks into which the water is conveyed consisted of—

The following is the result of his analysis of the water:—

There were also traces of lead, strontium, lithium, and phosphoric acid.

As the gas issued from the fissures in the limestone rock, it was found to consist of 99.22 grains of nitrogen, 0.88 grain of carbonic acid, and that held in solution in the water, 6.1 cubic inches nitrogen, 4.1 carbonic acid.

In comparing Dr. Thresh’s analysis with those previously made by Drs. Pearson, Muspratt, Sir Charles Scudamore, and Sir Lyon Playfair, it will be seen that a new constituent appears in the form of molybdinum, which, as mentioned above, was detected in the mud deposit at the bottom of the tanks into which the water is conveyed, as it issues directly from the springs.  In other respects the analyses differ but slightly, nor does the efficacy of the water appear to have become less potent in alleviating or curing those diseases for which it is so deservedly celebrated.

The Romans, ever luxurious in their use of hot and tepid baths, doubtless selected the Buxton basin as a station, not merely from a military point of view, but on account of the thermal springs, the