CHAP. l.] THE KADAPAH FORMATION. 135 
on the slates with trap in the eastern 
n ^ x 
D Vl i end of the Paneum range of that 
il ۸۸ district. On the eastern side of 
a3 
auem amie d a the Khoond-air valley, the same 
(BRA 
limestones are lying up over 
quartzites of the flanks of the 
Nullamullays which are of a dif- 
ferent group altogether from any yet 
mentioned. 
The sections 1 and 2 (see Plate of 
Sections) show this 
Sections show- ; 
ing generaluncon- general unconform- 
D ity where it is per- 
haps most plainly visible: and the 
accompanying sketch (Fig. 17) ex- 
hibits its effect on the scenery of the 
country. Other sections illustrative 
of this relation of the two formations 
will be met with as the description 
progresses. 
Z 
This greatly older series of rocks 
constitutes the Ka- 
KADAPAHS, a S f 
complicated suc. DAPAH SERIES of our 
cession of quartz- . : : 
diee. ed classification, and it 
KARNULS 
KADAPAHS. 
Sketch-section from Mulkapoor through Ullabad to the Ramwarum range. 
k 
k 
Fig. 17. 
is essentially a suc- 
cession of quartzites and clay slates ; 
the latter having limestones fre- 
quently associated with them, and in 
one particular group a great thick- 
ness of trappean rocks and their 
associates. But this succession is 
N ty W. 
not a simple and uniform one like 
| (Hes) 
