It seems, therefore, that after most of the magma had crys- 

 talhzed into the peridotite, and the pipe-hke mass of Uquid was in- 

 jected into the peridotite, where after further differentiation, the 

 material crystaHized into enstatite and chromite. Hydrothermal 

 solutions later altered the enstatite to wilhamsite. 



The Line Pit, Red Pit, Jenkins' Mine and Reynolds' Mine deposits 

 all fall on a line on the map. The significance of this is not known. 



(454) 



