294 DESCRIPTIVE MINERALOGY. 



Silica, 51.00 



Lime, 21.00 



Magnesia, 11.50 



Alumina, 3. 50 



Peroxide of iron, with a trace of manganese,. . 11 .53 



Water, 1.00* 



Lamellar pjrroxene of a dark colour, and exhibiting cleavage in the direction of P, is found 

 at many of the localities of magnetic iron ore in the town of Monroe, as at the Forest of Dean 

 mine, the Rich iron mine, Long mine, Mountain mine, Patterson mine. Sterling mine, Cross- 

 way mine and O'Neil mine. There is a great deal of similarity in the characters which the 

 mineral pre sents at these different localities. 



The granular variety coccolite is also exceedingly abundant in this county. In the town 

 of Monroe, a mile west of Coffee's hotel, it is in small gi'ains, perfectly black. Near Green- 

 wood furnace, it is light green and translucent, and often in large grains which admit of 

 cleavage. Again, in the Forest of Dean, it is black ; and the same character will apply to 

 that which occurs at the Forshee and O'Neil mines, as well as that from Bull's pond in the 

 same town. It is also found at Rocky hill in Warwick, and in the town of Cornwall, four 

 miles west of West-Point. 



At some of the above localities, pyroxene is found in such abundance as to constitute rocky 

 masses ; and there is often oliserved at, or near, the same spot, the crystallized, the lamellar 

 and the granular varieties, passing into each other, and varying in colour, so that it becomes 

 almost impossible to indicate the line of distinction between them. 



Putnam County. At Hustis' farm in Phillipstown, there is a variety of pyroxene which 

 has been called diopside. It is translucent, has a light green colour, lamellar structure, and 

 a glistening surface. It sometimes contains small crystals of pale green apatite. Associated 

 with it are white, rose-coloured and green coccolite. The whole is contained with serpentine 

 and other allied minerals in white limestone. The white coccolite was formerly considered a 

 new variety. It is made up of grains of various sizes, and resembles dolomite. Pyroxene, 

 crystallized in eight-sided prisms, has been found at Coldspring in this county, where other 

 varieties, similar to those just noticed, also occur. 



About two miles south of the village of Carmel in the town of Southeast, there is a dark 

 green, almost black, coccolite, associated with crystallized epidotc, hornblende, etc. It is not, 

 however, abundant. Pyroxene also occurs on Tovmsend's farm, about half a mile north of 

 the preceding locality. 



In the dolomitic beds near Patterson, crystallized white pyroxene is very abundant ; so 

 much so, that in some places it greatly injures the value of the limestone for the uses to which 

 it is ordinarily applied. In some places, the surface of the little elevations of the rock is 



^ Jomnnl of the Ac(id':my of Natvral Sciences of Philadelphia. III. 63. 



