WESTERN DISTRICT. Wl 



The facts brought to light by the plienoniena of this range of waters, demonstrate that their 

 characters depend upon tlie rock from wliich the\- issue. Where, for instance, hepatic 

 springs issue from tiic rocks above or below, essential dillerences are known to exist. 

 According to Dr. Chilton, the water of the Sharon spring contains, in one pint, 



Sulphate of macfnesia 2*65 



Sulphate of lime 6-98 



Chloride of sodium 0-14 



Chloride of magnesium 0'15 



Hydrosulphuret of sodium and magnesium 0-14 



Sulphuretted hydrogen gas, one cubic inch. 



An example of the second order of sulphur springs, is found upon the shore of Onondaga 

 lake, near Syracuse. It contains, in a pint of water, 35 "732 grains of saline matter, the 

 major part of which is chloride of sodium. It gave, on analysis, 



Chloride of sodium 30-420 



Chloride of lime 4-822 



Chloride of magnesium 0-490 



The sulphuretted liydrogen is in combination witii organic matter. 



Another class of springs, of which only a few are known, are the sulpluuic acid springs, 

 or those springs which contain an excess of sulphuric acid. These springs are indicated 

 by the charred vegetable matter through which the water issues. They are, I believe, 

 peculiar to the Salt group, or issue only therefrom in this State. They may appear, 

 however, as high in the geological series as the rocks wiiich give origin to the Sharon 

 springs. 



The common sulphur springs are very abundant, and are known throughout the whole 

 wheat region. In Moscow, and its neighboriiood, sulpluir springs issue from the Genesee 

 slate, which are often highly bituminous. 



A fact of considerable interest was reported to me, in regard to the efficacy of (he milder 

 sulphur waters in incipient phthisis. It was stated by Dr. Dwight of Moscow, that con- 

 sumption rarely occurs in tliat neigliborhood ; and that persons who have alreadj- a cougli, 

 attended with irritable lungs, are benefited, and generally cured by the waters of tliis region, 

 many of which are impregnated with sulphur and sulphuretted hydrogen. Strangers, with 

 affections of the kind referred to above, after drinking the waters five or six weeks, are 

 attacked with an eruption of the skin, which appears in the form of a fine rash. Soon 

 after the appearance of this rash, the lungs are relieved. 



A spring, containing less sulphuretted hydrogen than the Sharon spring, but more saline 

 matter, has been discovered in Alden, Erie coimty, near Buffalo. One pint of the water 

 contains 88-36 grains of solid matter, principally the chlorides of soda, lime and magnesia, 

 and no sulphuric acid. A little iron falls to the bottom of a vessel in whicii the water 

 stands, being an organic salt of iron : it contains more organic matter than suffices for the 

 neutralization of the iron. The presence of organic matter in all the mineral waters of 



