﻿200 



PROCEEDINGS OF THE GEOLOGICAL SOCIETY. 



[Feb. 6, 



Returning to the shore opposite Balmacarra we find that the 

 quartzose flagstones already described cross into Skye and form the 

 great mountain-mass of Een-na-Cailleaich. Their dip on the north- 



20 



5> 



25 



5Q 



2? 



CJO 



3 



Off 



western side of the anticlinal arch is obscured by the faults ; but their 

 south-eastern dip is well shown along the bare grey slopes of the 



morphism than that of the Lias limestones. It occurred to me also, last summer, 

 while on the hills above Ord, that possibly some parts of the metamorphic lime- 

 stone of Strath may possibly be also Silurian. — A. G-. 



