CRAP. 1.[ .. FAULTS AND FLEXURES. 261 
Doopad Valley 
eee 
۱ N ` $3. DIES AME 
Fig. 43. Sketch section across Waumyconda range, east-north-east of Kakeralla. 
S3. Cumbum slates with limestone. Q3. Byrenconda quartzites. 
The sharp double of the quartzite band in the middle of the ridge is very clearly displayed in the 
side valleys. 
NNW: e ERI ed SSE. 
? Q3. 
Fig. 44. Section displayed on the eastern side of the deep lateral valley leading up to Waumyconda. 
NW, SE. 
Fig. 45. Sketch section of the Waumyconda. The quartzites capping the lower hill to the north- 
west correspond to those at the bottom of the inversion in the section above. 
NNW, 
3 SSE. 
g 
7 en 
=~ s3. S Doopad Valley 
IBS ren 
7 HWY his ee 
g 4: 
Fig. 46. Sketch section across the Waumyconda range, north-north-west of Marripalem. The posi- 
tion of the quartzite bands in the KADAPAFS is as yet doubtful. 
arms of the curve have slid over each other. There is every sign of a 
fault along here—in the odd juxtaposition of the limestone and different 
bands of quartzite at such high angles, and the non-appearance in the 
$1201: ) 
