450 



A. F. BUDDINGTON 



are confined almost exclusively to the shore lines, and often to small 

 valleys at the mouths of brooks which may be from a fraction of a 

 mile to several miles apart. 



10- 



Geological and 5ubmarine 

 Topographical Map of 

 5.E. Newfoundland^^_ ^^ ri^h?^' 



bv J P Ho-kj .,<,-, I- ^ 



Sjbmonnc To^graphy based On Attfni--aH^ 



Fig. I 



LITERATURE 



The literature on Newfoundland pre-Cambrian geology is well 

 summarized by Van Hise and Leith ( 1 909) . Jukes ( 1 843 , p. 5 1 ) first 

 separated the Cambrian from the pre-Cambrian and noted the 



