D2 KING: KADAPAH AND KARNÜL FORMATIONS. [PART II. 
Koilkoontla limestones come to the surface, and are quarried 
i around Cuddapah, Dhoor (and to the westward), 
Localities. 
Chagulmurry, up the bed of the Serawul stream, : 
in the bed of the Khoond and the country on its right bank opposite 
Banaganpilly, about Bundy Atmacoor, and in the northern part of the 
field between Puggydeal and the Kistnah. There are, of course, numer- 
ous other localities where the rock is to be seen, but these are the most 
marked. More particular instances will be given further on where 
sections of nearly the complete series of KARNUL rocks may be found. 
CHAPTER 2.—THE KARNÜL FORMATION.—PANEUM GROUP. 
As one passes from the wide plains of the Khoond valley north 
Khoondairs underlaid Of Nundial, which are of the Khoond-air rocks 
UNIQUE just deseribed, on to the rising rocky ground of 
the Oondootla and Poolcherla ranges of hills, it is found that the lime- 
stones and purple shales he up over beds of quartzite. These quartzites 
are best displayed in the low range of hills north and west of Paneum*, 
and as they constitute a group of rocks distinct in every way from the 
limestones above and. below, we distinguish them as— 
THE PANEUM GROUP. 
The quartzites so associated together are characterized by features 
ERE M Ur es which point them out as of two varieties, often 
تن‎ in different localities, and occasionally at the 
same place. The one feature is, that certain of the beds have a peculiar 
way of weathering along their scarps, and over their exposed surfaces, 
in lines of low buttressed and pinnacled cliffs, while they are generally 
of a white colour; and the other is, that the rest of the beds of the 
group do not wear away after this fashion, but in the usual manner 
of horizontally bedded grit and sandstone quartzites, while these are 
* Paneum, Khoond-air valley, on the road from Nundyall to Kurnool. 
Qua) 
