DEVONIAN <U" NEW BRUNSWICK. 



505 



"West and north of Mount Prospect, where the Cordaiti 

 disappear beneath the stratified gravel which covers the top of thai 



hill, the dip of the beds at the base of this group rapidly diminishes 



C5 



£ 



o 



s 



s 





to 



I!uy of l'muly 



WVst Beach 



MiBpeok River, 



Beaver Lake 



Mount Prospect. ..<; 



Coldbrook 



from 30° to 15°, and the strike at the same horizon varies 10°. The 

 lowest member is a coarse reddish conglomerate, having a red slaty 

 paste filled with large subangnlar fragments of a gray altered rock, 

 like the lower slate of the Coldbrook group. It also contains frag- 

 ments of reddish sandstone, and a few pieces of impure slaty lime- 

 stone. The conglomerate is overlaid by thick beds of purple clay 



