OF DURNESS AND ASSYNT. 



245 



been obtained from the quartzite, tending to show that the two 

 rocks hang together. The Assynt series, though less distinct than 

 that at Loch Emboli, was not inconsistent with such an idea. The 

 unequal tension of the two rocks might in part account for local 

 discordance of strike. 



Dr. Callaway could not agree with Mr. Hudleston as to his 

 interpretation of the Durness section ; such discordant strikes were 

 incompatible with the idea of a conformable succession ; nor did 

 he agree with his view of the Loch-Erriboll rock. He accepted the 

 age of the limestone. 



Q.J.G.S. No. 146. 



s 



