132 " ECONOMICAL MINERALOGY. 



wells in the village of Fredonia are strongly charged with the gas. It may also be added, that 

 there are frequently to be observed in this vicinity disruptions in the strata of slate, which 

 have probably been caused by some expansive force exerted from beneath. 



Mr. Storke, one of the engineers on the Buffalo and Erie railroad, obligingly furnished me 

 with the height of several points in the vicinity of Fredonia, from which some conclusions can 

 be drawn concerning the thickness of the strata which are impregnated with this bituminous 

 matter. 



It will be recollected that the gas issues through the strata of slate which form the bed of 

 Lake Erie, as at Van Buren Harbout. 



The slate on the bank of the Canadawa creek, at Fredonia, through which the carburetted 

 hydrogen issues, is a hundred and thirty-seven feet above the level of the lake. 



The Laona sandstone quarry, the rocks of which contain petroleum, and have a strong bitu- 

 minous odour, is two hundred and forty-one feet above the level of the lake. 



The gas spring, four and a half miles southeast of Fredonia, is four hundred and eighty- 

 one feet above the level of the lake. 



On the west branch of the Canadawa creek, six miles south of Fredonia, at the height of 

 six hundred and seventy-four feet above the level of the lake, the same slate occurs. 



Three miles northeast of Jamestown, at the height of nine hundred and twenty-six feet 

 above the level of the lake, is a quarry of sandstone. 



The strata of sandstone and slate are, therefore, ascertained to be nearly a thousand feet 

 in thickness. 



Extending the computation to the other strata through which this gas is evolved, we find it 

 at Albany upwards of four hundred feet below the surface, or about three hundred and seventy 

 feet below tide, issuing throu_gh slate. 



At Vernon, in Oneida county, through the red sandstone, nearly four himdred feet above 

 tide. 



At Gasport, six and a half miles east of Lockport, through limestone, nearly five hundred 

 feet above tide. 



If Lake Erie is five hundred and sixty-five feet above tide, we have this same gas issuing 

 from strata from fifteen hundred to two thousand feet in thickness, and not less than four 

 hundred miles in extent. 



The above facts afford the most convincing proofs that the evolution of this gas is no evi- 

 dence of the existence of coal at any moderate depths below the surface ; unless, indeed, the 

 views which are at present entertained concerning the geological situation of this mineral are 

 entirely erroneous. And although carburetted hydrogen frequently has its origin in beds of 

 bituminous coal, the facts which have just been detailed tend tp show that its occurrence does 

 not necessarily depend upon such an agency. 



