.'1 
. I 
•' I 
• '» 
• I u 
‘I 
t ‘ 
,1 
Jyi 
r 
t. 
y 
>; 
*, k 
r 
Fig- 36. ■'>, 
Generalised Section across the Bangemall Anticline, ' , 
Gascoyne Goldfield. 
■ I 
( 
o 
1* 
< 1 
'■i.' 
j ' 
< I 
_ ;i 
i-' 
I 
i . 
.•i. 
4 
i 
.1 
,« 
4 
5 
Fig. 37. 
Sandstone Bu'.te, thirty-three miles east of 692 VI. Rabbit 
Proof Fence. 
Tn post-Nullagine times erosion of the series was excessive, i 
and possibly long continued. The strata were cut down until in \ 
some cases they were represented by mere isolated outliers (Fig. 37 ) ■ 
such as may be seen thirty-three miles east of the mile* po.st on 
the rabbit proof fence near the head of the Oakover River. The 
horizontal or gently inclined beds have been deeply incised, and 
narrow trenches cut into them, forming magnificent canons, hut 
often some miles in length down which the waters find their wav 
seawards. A view of one of these canons, carved out of the 
OARAfiF ■ I A A I argillACECKJS SHAL£EftsL*TE‘,..(2SXI MICACEOUS OCAPTZ 
SW 
* Lands Dept. Litho. 03/300. 
