40 Miseellaneous Localities of Minerals. 



3. Amianthus in seams, traversing the serpentine. 



4. Radiated Tremolile. 



5. Sphene imbedded in Tremolite. 6. Lamellar Talc. 



7. Asbestos^ intermixed with marble. 



8. Rhomhic Carbonate of Lime ^ pale flesh colour. 



9. Mica, in six sided crystals, in do. 



10. Diopside, a variety of pyroxene, colour light green, 

 structure lamellar, with a glistening surface. 



11. iVhtte Coccolite, in grains, the size of large shot, ea- 

 sily separable, colour clear white ; the cavities coDtain 

 crystals of white pyroxene, eight sided, the terminations 

 irregular, mica is sometimes associated with it. This new 

 variety is found in blocks and masses, in considerable 

 quantity, associated with marble, and serpentine. 



it was discovered by the writer, with the above mention- 

 minerals in 1820. The white coccolite is a new variety, 

 not mentioned in works on mineralogy ; it has already been 

 noticed in the American Journal of Science, Vol. 7, No. I, 

 page 171. 



12. Rose coloured Coccolite^ same locality, associated 

 with Diopside, or a variety of Pyroxene, it has been found 

 but in small quantities. 



13. Green Coccolite. 



14. Magnelic Iron Ore, in marble intermixed with as- 

 bestos. 



15. Pyrites. 



This interesting locality is on the declivity of a small hill, 

 principally composed of marble, serpentine, and white coc- 

 colite, on the farm of Mr. Joseph Hustis. These minerals 

 extend little more than a hundred yard--; the hill slopes to 

 the east, its foot is washed by a small stream, and its op- 

 posite bank is an abrupt granite precipice, in which horn- 

 ijlende, green pyroxene and green coccolite occur. 



In Philipstown Continued. 



16. Compact Feldspar. 



17. Pyroxene in several localities, green and also gray- 

 ish white. 



18. Green Coccolite, in several localities. 



19. Carinthin Hornblende. 20. Lamellar Hornblende. 



