st-riKe. The lithological characteristics are very much like th* S p 
of the- Pogonip above the Harabur 
'O’ r nn « p 
e> ^*v/. 
j. 116 9 8t> i m a t/ 6 d u n i c loi 0 s s 
is 1000 leet. No well determined fossils were observed. 
In Bulletin XXX men&ion is made of the occurrence of the 
Eureka quartzite just north of Bristol; Par.68, p.36. 
