256 



No. 10. " From the north side of Maud Island : C." (G. M. D.) 



Periploma cuspidatum. I Trigonia Maudeiisis. 



Tellina Skidegatensis ? var. 



No. 11. " From South Island : C." (G. M. D.) 



Haploceras Perezianum. 



" Timotheanum. 



Stephanoceras cepoides. 

 Amauropsis tenuistriata. 

 Cinulia pusilla. 



Thracia semiplanata. 

 Trigonia Maudonsis. 

 Yoldia arata. 

 Inoceramus concentricus. 



No. 12. " From Hooper's Creek Tunnel : (G. M. D.) 

 Unio Hubbardi. 



No. 13. " From Coal Locality, south side of Skidegate Channel : base 

 of C." (G. M. D.) 



Belemnites densus. 



No. 14. " From Bay east of Alliford Bay : (G. M. D.) 

 Amauropsis tenuistriatus. | Nucula (Acila) truncata. 



No. 15. " Fi-om the south side of Maud Island : base of C." (G.M.D.) 

 Astrocsenia irregularis. 



On the evidence afforded by the fossils as well as on stratigraphies! 

 grounds it would appear that the rocks at both localities in Cumshewa 

 Inlet and at Nos. 3, 4, 5, 6, 10, 11 and 14 in Skidegate Inlet are unques- 

 tionably Cretaceous ; that they represent the lower half of the Middle 

 Cretaceous, and that they are as nearly as possible the exact equivalents 

 of the Gault of Europe. 



At these localities the Lower Shales contain, among others, the follow- 



