'2 The entire Devonian series here given was laid down quietly, one group on another, with no marked 

 unconformability or disturbance. 



n Overlying conformably in places the St John group, and underlying conformably the Devonian. 



" trnited with Coldbrook on litholosrical grounds. 



'» Contains intercalated Upper Silurian strata, but Coastal overlies them. 



'• Overlying Upper Silurian and Lower Devonian strata, but from its lithological characters is placed in the 

 Huronian. 



'" Contains pebbles derived from the St. John group. 



" Placed here on account of palseontological evidence, although lithologically identical with the Huronian, 

 and apparently dipping beneath that formation. 



-0 In part. 



2' Lithologically undistingui.^hable from the Huronian, and formerly regarded as belonging to that age. 



'2 No instance of the superposition of this on the Laurentian observed. 



" In part. 



[These notes represent in a brief form the statements of the geologists above quoted regarding these for- 

 mations, as given in their publications and in the text preceding.] 



