Rex T. Prider. 
:J2 
lady (>ricnt<‘(l, in the intrusive a|)l()i»'ranit<‘. No attempts have therefore been 
made to intei’pret the minor dra;^- folded stnud-iires seen in these rocks. 
The drag-folds in the fine banded granitic gneisses are more constant 
in character and indicate that the easterly dipping rocks of this l»Jind form 
the eastern limb of a normal anticdine witli n pitch to the south varying 
from 0° to All outcro])s in this band were carefully examined for 
these drag-folded structunis and wherever visible they invariably indicated 
that this band formed the east limb of a normal anticline. 
