256 



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



Periploma caispidatum. Trigonia Maiidensis. 



Tellina Skidegatensis ? var. 



No. 11. '' From South Ishuul : C." (CI. M. D.) 



Haploceras Pereziannm. 



" Timotheanum. 



Stephanoceras cepoides. 

 Amauropsis tenxiistriata. 

 Cinulia pnsilla. 



Thracia semiplanata. 

 Trigonia Maudensis. 

 Yoldia arata. 

 Inoceramns concentricus. 



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



Unit) Hubbardi. 



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

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



Belemnites densus. 



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

 Amauropsis tenuistriatus. | Nucula (Acila) truncata. 



No. 15. " From 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 stratigraphical 

 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 tlie Gault of Europe. 



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



