Lie 
58 Miscellaneous Localities of Minerals, 
Epidote. West-Point. 
Stliceous schistus and Lydian stone. West-Point. 
Dialiage, more or less metalloidal. West Point. 
Ferruginous sand, and some specimens resembling de- 
composed greywacke, containing organic remains, such as 
the chamite, cochlite, gryphite, musculite, ostracite, pecti- 
nite, terebratulite ; and about four miles from here, to- 
wards Newburg, where the secondary formation commen- 
ces, we find orthoceratites imbedded in gr ke. The 
former, containing organic remains, has been found a few 
feet below the surface of the level of West-Point. 
Localities of Minerals, by Dr. Jacon Porrer. 
Radiated Zeolite, at Livingston, New-Jersey. 
Red Oxide of Titanium, at Cummington, Massachusetts. 
Sulphuret of Molybdena, at Chesterfield, Massachusetts. 
Localities of Minerals, by Prof. F. Hauu, Middlebury, V1. 
Ammonite, or Cornu Ammonis, on the surface of secon- 
dary limestone, in several places, in the vicinity of the for- 
tifications on Crownpoint, N. ¥. They are from half an 
inch to two inches in diameter ; are very frangible, and can- 
not be detached, entire, from the rocks, without a mallet 
and chisel. 
Massive Garnet, containing magnetic oxide of iron, erys- 
talized in regalar octaedrons, which are about the size of 
a large pea, and of a brilliant, steel gray colour. Chester, 
Red Sandstone, between the village of St. Albans and lake 
Champlain, where are extensive quarries of it. It is used. 
by the inhabitants of St. Albans as a building stone. 
Steatite, of a very excellent quality, Fletcher, Vt. 
Epidote, crystalized and massive, Middlebury, Vt. 
uh he crystals are small, of a light green colour, and stri- 
ated. 
Epidote, filling cavities in a stone, which appears to be 
quartzeous. 
In some instances, the Epidote forms only the lining of 
the cavity, leaving a smaller cavity in the Epidote itself.— 
This Epidote is all amorphous, and of a lamellar structure. 
