666 



Appendix. 



78 5 do with pyritous copper, Sterling 



786 Galena and blende, do 



787 Reddish sulphuret of Zinc, do 



788 Red Oxide of Titanium, Conway. 



Talcose Slate. 



serpentine locality, 

 near the steatite, >* 



789 Scaly greenish Talc, 



790 do 



791 Foilated light green do 



792 do 



793 do 



794 Green steatite or neaidy compact talc, 



795 Steatite /with rhomb spar, 



796 do 



797 do with bitter spar, 



798 do with brown spar, 



799 do 



800 , do bored for aqueduct pipe, 



801 do very fine, 



802 do 



803 do 



*403 and 1548 do from Gneiss, Worcester. 



804 do asbestus, 



805 do passing - into serpentine, 



806 Between steatite and chlorite form a bowlder 



originally from Whitingham Vt. 



807 Dark green scaly chlorite with feldspar 



808 Finer grained, do 



809 1 Slaty Chlorite, 



810 do with the steatite. 



811 Chlorite Slate, 



812 do with red oxide of titanium and feldspar, 



813 Talco-chloritic Slate, 



814 do 



815 do epidotic, 



816 do do and psssing into hornblende slate, 



817 Talcose Slate — talc and quartz, 



818 do do nearly white, 

 819, 820 do do do 



821 do do greenish soapstone quarry, 



822 do do do 



823 do do whetstone quarry, 



824 do do 



825 do do 



826 Talcose Slate, talc, quartz, and mica. 



827 do do 



828 do do 



829 do do 

 830, 831 do do 

 832 



Westfield. 

 Middlefield. 

 Rowe. 

 Middlefield. 

 Windsor. 

 Zoar. 

 do 



Windsor, N.W. part. 



do N. E. part. 

 Smithfield,R. I. 

 Middlefield. 

 Grafton, Vt. 

 Blanford. 

 Somers, Ct. 

 Groton, 



New Salem. 



do 



| Conway. 



Cummington. 

 Goshen. 

 Smithfield R. I. 

 Middlefield. 

 Peru. 

 Windsor. 



Little Compton, R. I 

 Smithfield R. I. 

 Cumberland R. 1. 

 Smithfield R. 1. 

 Little Compton R. I. 

 Stafford. 

 Hawley. 

 ■Middlefield. 

 Plainfield. 

 Smithfield. 

 Florida. ' 

 Lenox, 



Hawley. 



Iron Liine, Somerset, Vt. 

 east side of serpentine, Chester. 

 Barre. 

 Rowe. 



Talc and Limestone, 



Whitin^ham, Vt. 



* I was not apprised of the existence of steatite in Worcester till it was too late 

 to notice it in the proper place. Although I have not visited the spot, I have rea- 

 son to believe that it occurs in gneiss, in the southeast part of the town. The 

 owners informed me that they had penetrated the bed as yet only about five feet- 

 The specimens will show that it is the handsomest steatite in the State yet discov- 

 ered: and should the bed prove to be a large one, its situation near the Blackstone. 

 Canal, will render it of high value. 



Worcester ought also to be mentioned among the towns that abound hi peat. 



