288 



THE GEOLOGY OF THE LABRADOR COAST. 



were beds of a dark fine-grained hornblendic quartzose 

 gneiss, capped by the syenite. At Indian Harbor, about 

 thirty miles north of Tub Harbor, and on the opposite 

 side of Hamilton Inlet, these same rocks appear. These 



J Saddle Is 

 T ijde£- 



-MAP OF « PORTION 



OF THE COAST QF 



LABRADOR 



-1 • • ■\ Kiiu£&(/-buc/i.Bcw 

 - - ■ ■ f^^^y r^T^ TltamasSdu' 



Sajidu^ic/f^SoLf 



SfnOaiJs 

 tlsle nflb/uis 



^^SUt/t^ I J 





CapeSaul/lr 



rocks Occur also at Sloop Harbor, rising two hundred 

 feet high, and are capped by syenite, which is very pale 

 in color, with particles of black hornblende. Here, as 

 at Tub Harbor, the strata at the point of contact with 



