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94. KING: KADAPAH AND KARNÜL FORMATIONS. [PART III. 
that run under and behind and above the quartzites of Goomconda, and 
so along the bases of the Lunkamulla towards Nundiallumpett. "There 
is à break in their continuity when they reach the southern end of the 
tank of the last village, but the same beds with quartzites above are 
again found a mile to the westward when they are again traceable into 
the ridge west of Wonypenta. 
Unfortunately in the Nundiallumpett, or Parnapawd, outcrops 
OUO LR there is a very great deal of obscurity ; as, besides 
0 the fact that the ground is much obscured by the 
alluvial deposits of the Annaloor plain, the newer KarNUL limestones 
are in juxtaposition with these KADAPAH limestones ; and they also 
have been affected to some extent by some of the forces which pro- 
duced the rapid folding of the older strata, or their possible fracture 
along what must have been a complicated northerly system of dis- 
locations. 
That there has been some east and west displacement of the strata 
in the Lunkamulla mountain-mass and the lower 
part of the Nullamullays to the north of it is 
evidenced not only by this break at the south end of Nundiallumpett 
Hotcomudgoo faults. 
tank, but by another line of distinct displacement of outcropping bands 
further to the east in the Hotcomudgoo valley. Here the northern 
bands of silicious limestone have been eut off completely, as they do 
not show to the south, while there are no traces of extensions of the 
Jundermorum bands in the Lunkamulla country 
Dore A immediately south. There has clearly here been 
an upthrow* of the beds to the north; and the subsequent denudation 
has thus exposed beds of limestone which are buried deep under the 
basement of the Lunkamullas. Hence northwards the limestone bands 
of the Cumbum slates, as they occur in the Nullamullays, die out 
* That is, supposing that the Lunkamulla beds are Cumbums. 
) 284. ) 
