46 Brush and Dana—Fairfield County Minerals. 
\ 
mineral which proved to be chabazi 
_ oceurrence of these minerals, we will now proceed to describe 
inutely. 
and, as far as tested, in composition, to that described in out 
The lithiophilite of which we are now speaking has, in al- 
most all cases, the salmon color of that first described. In one — 
specimen the amount of iron was determined by Mr. Penfield 
and found to be but 3°56 per cent. The lithiophilite some- 
times contains imbedded rhodochrosite. Other constantly asso- 
ciated minerals are: apatite, garnet, uraninite in_ brilliant 
slightly different composition as shown by the analysis given 
on p. 47. Closely associated with the lithiophilite was acon- 
siderable amount of a granular, often also cellular, mangane- 
sian carbonate, rhodochrosite. This was quite impure, often 
mmediately connected with the minerals described, was a 
LITHIOPHILITE. 
_We have already stated, that almost all of the lithiophilite 
discovered was similar in its salmon, and salmon-pink colo 
* 
