BRINK SPRINGS. 103 



Near Riilledge, in the County of Cattaraugus, there arc several springs with a shuhl 

 impregnation of salt. Some attempts have been made to work them, but they have not been 

 attended with the least success. 



Although brine springs have not heretofore been noticed in Chautauque County, the fre- 

 quent occurrence of gas springs would lead us to suppose that brine will j-et be found asso- 

 ciated with them, as it is in various parts of this State and Ohio. 



From this brief account of the localities of the brine springs in this Slate, it appears that 

 they occur with various degrees of frequency in almost all the counties west of a line passing 

 through Otsego, and bounded on tiie nortli by the southern hues of Lewis and Jefferson. It 

 is, however, well known, that favourably as many of these springs are situated, none of them 

 are at present employed to any extent in the manufacture of salt, e.xcept those found on the 

 margin of tlie Onondaga lake. This fact proves most conclusively the superiority of the last 

 mentioned springs, the great importance of which cannot well be over-estimated. 



Chemical composition. In regard to the chemical composition of tlie waters of these dif- 

 ferent springs, great uniformity is found to prevail. All those which have been subjected to 

 analysis contain, altliough in somewhat various proportions, the chlorides of calcium and mag- 

 nesium, and the carbonate and sulphate of lime, in combination with the common salt. All 

 of them, moreover, when freshly drawn, give the characteristic test of iron, which exists in 

 minute proportions in the form of carbonate ; or perhaps in some cases the oxide of iron may 

 perform the jiart of an acid, which, by combining with lime, may thus exist in the fonn of 

 ferrate of lime. Bromine is also known to be one of the constituents of the Salina brine, and 

 it will probably be- found in most of the others ; but iodine has- not yet been detected in any 

 of them. It may be interesting to observe, that all these ingredients are found in sea-water, 

 although the order of combination is somewhat different. In the brine, the proportion of car- 

 bonic acid and of iron is usually greater, while that of magnesia is less, than in sea-water ; 

 and iodine, which has not been detected in the former, is frequently found in the latter. And 

 to show, that so far as it regards the chemical nature of these substances, there is no incon- 

 sistency in the theory that these brine springs result from the solution of beds of rock salt, it 

 may also be stated that all the saline matters which they contain are met with in rock salt, 

 except that the chloride of magnesium is either entirely wanting in the latter, or exists only 

 in very minute proportion. The rock salt of Droitwich and Cheshire contains the chloride of 

 calcium, but not of magnesium. These facts, although they appear to be of little importance, 

 may hereafter be found to have some bearing upon the views which are entertained concerning 

 the origin of our salines. 



Brine Springs of Onondaga County. The fact that the Slate derives an important part 

 of her revenue from these springs, and that they furnish employment and give support to 

 many thousands of her citizens, seems to render it necessary that I should present a detailed 

 description of them ; and also thai I should offer such suggestions concerning the maiuifacturo 

 of salt, as may be thought worlliy of attention. 



