338 



R. A. DALY— THE OKANAGAN COMPOSITE BATHOLITH 



white, massive outcrops of the granite are very conspicuous on the north- 

 ern spurs of Park mountain ; the rock may be referred to as the Park 

 granite (see figure 6). 



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Figure 5.— Ground Plan showing Relations of the Cathedral and Remmel Batholiths and 



the Ashnola Gabbro. 



The Younger phase of the Cathedral batholith is shown by stippling. The remarkably 

 straight contact line of the Cathedral granite lies sensibly parallel to the gneissic banding 

 in the Remmel batholith, Eastern phase. Scale, 1 : 120,000. 



Within the 5-mile belt these various rock bodies occupy areas shown in 

 the following table. The bodies are noted in order from east to west, 

 beginning on the east : 



Square miles 



Osoyoos batholith 50 



Kruger schist 15 



Kruger Alkaline body 



Siinilkameen batholith 



Chopaka schist 



Chopaka basic intrusives 



Horseshoe schist (pendant) 



Snowy schist (pend;int) 



Cathedral batholith 61 



Remmel batholith 64 



Ashnola gabbro (pendant) iy 2 



Basic complex (pendant) 6y 2 



Park Granite stock 



1% 

 1 



Total 200 



