C. U. Shepard—Oorundum of N. Carolina and Georgia. 111 
exhibit 
the following order of formations, commencing on the N.W. 
gated without order, much as mica is in large-grained granites; - 
but what is bere chiefly remarkable is, the entire absence of 
quartz. Narrow veins, containing besides the chlorite and 
corundum, a dark blackish green spinel (mostly massive), more 
or less mingled with black tourmaline, traverse layers 4 and 5, 
Chester (Mass.) emery mine. I have not been informed as to 
the underlying rock of the above mentioned strata, but sup- 
As to their linear prolongation, nothing is yet established ; but 
18 quite probable that it is not very considerable in it sot 
ton to the thickness of the beds; and it is most likely t 
ted on the road from Walhalla, S. Car., to Franklin, and 10 
or 15 miles to the S.E. of that above described. At the Culla- 
Kenee (sometimes written Cullakenih) mine, on Buck creek, in 
