Some Kyanite-p.earixg Rocks i-’ro:m the Eastern Goldfields, 
Western Australia. 
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ai}art on a north-northwesterly line, their highest points being marked by 
small cairns. The northern Camel Hump is the more prominent and consists 
of a long ridge extending over a length of more* than ‘20 chains, broken by 
erosion gaps into thi'ee liills, the central and highest eari*yinga cairn. (Eig. 1.) 
These hills are made up of outcrops of a hard yellowish-Avhite coloured, 
rudely jointed and bedded quartzose i*ock which dips from veilical to SO 
degrees to the east. The jointing has resulted in the production of lai‘ge 
