The air being so pure and dry exerts a most bracing and tonic effect, especially in cases where the system has become debilitated from any cause—anæmia, chlorosis, chronic liver and splenic disease, many forms of bronchial asthma, the first stage of tuberculosis of the lungs, and tubercular degeneration of the mesenteric glands in childhood, I have seen much benefitted by a short residence in the district. To the closely-confined and overworked residents in towns the crispness and buoyancy of the atmosphere impart a feeling of lightness and exhilaration rarely experienced except in a highland district, making mental and physical labour less irksome and life more enjoyable. The water supply of Buxton is abundant, soft, and free from impurities, doubtless owing to its percolating through the great filter bed of sandstone to the north of the town, and issues in numerous springs far above any source of contamination from the inhabitants in the valley below. It has been stated (and I think much to the prejudice of Buxton) that the rainfall of the High Peak, and especially of the Buxton district, is generally in excess of that of most of the other parts of Great Britain. Such an assertion is quite incorrect, as may be ascertained by a careful examination of the rainfall of other localities; although, as in all hilly districts, we must, on account of the attraction of the hills, expect a somewhat larger rainfall than on the plains. The annual average fall in the neighbourhood of Buxton amounts to about forty-nine inches, which is much less than that of many localities both in the Northern and Midland Counties. Even when there is an exceptionally heavy fall of rain the porous nature of the subsoil precludes the possibility of an accumulation of surface water to any great extent. The following table shows the mean temperature and rainfall for 1890 and 1891, two years in which we have experienced a lower temperature and a greater rainfall than for some years past, which, I believe, has been the experience of most other parts of Britain during the same period:—