SILICA. 
291 
A fine emerald green coccolite, associated with tabular spar, and quite similar to that of 
Willsborough in Essex county, is found in place, and in considerable abundance, about half 
a mile from the above locality. 
New-York County. Crystallized pyroxene, of the white variety, is very often found in 
the dolomite of this island. It sometimes has a granular structure like the dolomite, and it 
not unfrequently is so much charged with carbonate of lime as to effervesce in acids. The 
crystals heretofore noticed are eight-sided prisms, with the two opposite sides often much 
larger than the other six, so as to present a tabulated form represented in Fig. 202. This, 
however, often has l enlarged to the di¬ 
mensions of r. Another form is that 
represented in Fig. 203, in which the 
lateral primary planes are entirely obli¬ 
terated by the new ones r and l; perior- 
thogone of Haiiy, l on r 90° Ob The 
prism is variously terminated, sometimes 
as in Fig. 201, and at others they are 
more complex, giving rise to a new va¬ 
riety which Haiiy (to whom the speci¬ 
mens were sent) named epimeride* Fig. 
204. M on x 134° 17 / ; i on l 139° 7 / ; r on x 126° 36'; x on x 131° 8b Specific gravity 
3.10. The crystals are of various sizes, from minute to several inches in length, and they 
are imbedded in the limestone which crosses the island at its northern extremity, in greater 
or less abundance throughout its whole extent. The abandoned quarries at Kingsbridge, 
about 208th-street, also afford very good specimens. 
Oneida County. Large bowlders, made up of coccolite, glassy quartz and tabular spar, 
are found at Boonville. The coccolite is of a rich green colour, semi-transparent, and is 
equal in beauty to any in the United States. The specimens closely resemble those which 
are found in place in Lewis on the borders of Jefferson county, forty or fifty miles north (see 
Tabular spar, page 271). 
Orange County. The mineral riches of this county are in no respect more remarkable 
than in the abundance and variety of pyroxenes which are found in it. If it were possible, it 
would perhaps be unnecessary, to enumerate all the localities, and I shall therefore confine 
myself to some of the more interesting ones. And it should here be stated, that we are 
chiefly indebted to Dr. Horton for what is known concerning these and other minerals of 
Orange county ; and the reader who desires more particular information concerning them, is 
referred to that gentleman’s Catalogue, published in the New-York Geological Reports of 1839. 
The lighter coloured varieties of pyroxene, in this county, are usually found in white lime¬ 
stone ; the darker ones are most generally associated with the magnetic iron ore. In many 
Fig. 202. 
Fig. 203. 
Fig. 204. 
Troost. Journal of the Academy of Natural Sciences of Philadelphia . III. 105. 
