= 
taries у 
angle formed by the successive down-dropping of parallel blocks. 
626 Transactions. 
uring mid-Tertiary times after the coal-measures had 
v 
> en la wn. 59 
In my paper on Кейсі Gully (Trans. N.Z. Inst., vol. 45, рр. 340-41, 1918) ` 
be expected. . o 
This system of faulting on subparallel lines results in the Malvern Hills _ 
m 1 a 5 i 
t or 
strike of the weaker Cretaceous sedimen which have occupied the 
