1ISCELLANE0U5 COLLECTIONS 



VOL. 75, NO. 5, PL. 75 



Rounded ridges formed of the shales of the Chancellor formati( 

 Stephen, and Cathedral formations. 



in the fiireRroiind with cliffs uf tin 



npcrjacent Ottertail limestone at the left in Washmavvapta kidKe. in the distance, to the right of the center, peaks of the Bow Range, that are eroded in the Middle Canihrian limestones of the ICldon 

 Locality. — View taken from a low mountain northeast of Wolverine Pass, British Columbia, and about 16.5 miles (26.5 kin.) southwest of Castle Mountain Station (at 7 on map. pi. 2(1), .Mherta 



