80 * THE EED KOCKS OF THE DEYON COAST-SECTION. 



a thinning-out of the Permian marls and sandstones in the Severn 

 country similar to that which Mr. Ussher had shown to occur in 

 Devon. He reminded the President that Sir A. Eamsay had anti- 

 cipated him (the Author) in suggesting that the breccias were of 

 Permian age, and, in conclusion, expressed his satisfaction at the 

 warm interest in the question evinced by the discussion. 

 Prof. Blake also spoke. 



