DEVONIAN OF NEW BRUNSWICK. 



505 



" West and north of Mount Prospect, where the Cordaite shales 

 disappear beneath the stratified gi-avel which covers the top of that 

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



-*! 



S 





«1 







to 



Bay of Fuiidy. 



West Beach . 



o 



Mispeck River., 



Beaver Lake 



cs 



Mount Prospect.. .•eji;! 



Coldbrook . 



to 



G 



^ P- 





Q 



i 5 = 





„ 3 



L1 



5 ^ 



■ .- 3 

 t7 P 



2 "O 



■p ° S .; = ■? 



u O 



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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 Avitli large subaiigular 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 



