WANDERING BOY VEINS. 



DISPLACEMENT OF THE WANDERING BOY FAULT. 



153 



The Wandering Boy fault, as .shown on the map, separates the earlier andesite 

 on the northeast from the Fraction dacite breccia on the southwest. It has 



Scale 



o 10 20 40 co ao loofeet 



FIG. 42. Plan showing outcroppinK veins near the Wandering Boy and their probable relation to the veins encountered 



underground. 



therefore a downthrow on the .southwest, and underground workings show that 

 it has a southwest dip, making it a normal fault (fig. 43). That the contact is 



