296 D. B. DOWLING — CRETACEOUS SECTION IN SOUTHERN ALBERTA 



Two of the greater folds reveal the limestone beneath and several sec- 

 tions were made of the total thickness of Cretaceons strata. As my own 



Jiie 



u.v 



Figure 1. — Mu» of part of Alberta and British Columbia. 



work for the last three seasons has been within the mountains on rocks 

 of the Kootanie series, I can with some certainty correlate them with 



