SUMMARY OF CONTENTS. 111 
PAGES, 
ascending order.— Fundamental beds apparently along the whole of western 
edge of field.—Searp beds of northern half.— Overlap scarp beds of southern 
half.—Near Goolcheroo south of Cuddapah.—Goolcheroo quartzites, lowest 
beds.—Points against this view.—Present classification of series mainly 
tentative e M des nc M: .. 124—148 
CHAPTER 2.—The Pawpugnee Beds.—Lowest group of KADAPAHS best seen on 
the Paupugnee.—A set of quartzites and overlying slates with limestones.— 
Character of Goolcheroos, details.—Mr. C. Æ. Oldham’s work northwards 
from Goolcheroo.— Bottom or contact beds.—Traces of a higher series coming 
in.—Faulted valley north of Nulkoorty Peak.—Section at the Paupugnee pass.— 
Goolcheroos decreasing in thickness.—Rippled beds.—Coarse bottom beds. 
Pebble beds of jasper coming in.—Ribbon jaspers.—G oolcheroos still thin- 
ning out.—Distinetive western scarp ceases.— Ridges of fault-rock in CRYS- 
TALLINES.—Very coarse conglomerates of fault-Crock.— No scarp, strata tail 
up slope.—Indications of alteration of contact rocks.— Bottom bed apparently 
baked into the gneiss.—Signs of old shingle banks.—Coarse conglomerates 
decrease with ridges of fault-Crock.— Further cases of altered contact.— Signs 
of dislocation and folding.— Altered contact again.— Conglomerate of adjacent 
granite.—Uniform run of outcrop broken by Gunygull fault.—Strata north of 
fault.—Felspathic grits.—Bottom beds thinning out at Kurnool.—V aimpully 
slates.—Die out east of Goolcheroos.—Obscure faulting.— V aimpullies 
essentially a limestone sub-group.—Intrusive trap.—Character of limestones.— 
Silicious bands of oolitoid structure.—Northwards, limestones become more 
silicious.— Different beds seen underlying the next group.—Strata thin out 
as Kurnool is approached.— Thinning out at Cuddapah end.—Intrusive charac- 
ter of trap.—No cases of direct cutting across the beds.—Alteration of lime- 
stones, &c., in contact with trap.—Serpentine-limestones.—Steatite, or “ Bul- 
pum.”’—Serpentine-limestones near Kurnool.—Vaimpullies overlap Gool- 
cheroos on the Kistnah.— Denudation.— Thickness of group... ... 148—167 
CHAPTER 3.—Chey-air Beds.—Poolavaindla quartzite.—To the north, in de- 
tached areas.— Continuous thence in Puspulla ridge to Cuddapah,—South of 
Cuddapah, continuity broken.— Constitution of sub-group.—Intrusive trap.— 
Unconformity to subjacent series not always clear.—On the Kistnah.— Containing 
fragments of Vaimpullies.—Spread out over the gneiss.— Mr. Foote considers 
some of these beds as KARNÜLS.— Character of strata in the ridge of continuous 
outcrop.—Unconformity on the Paupugnee.—Series of faults in Paupugnee 
valley.— Partly accounts for abrupt bend in strike east of Cuddapah.—Quart- 
zites beneath Polleonda pagoda apparently Poolavaindlas.—Pagoda beds are 
Naggery quartzites.—Tripply banded.— Conglomerates.— Strata on west side 
of Chey-air field.— Tripetty scarps.—Mr. C. Æ. Oldham's notes.— Character of 
sub-group.— Natural boundary between Naggerys and ORYSTALLINES, until 
near Kirkumbady.—Kirkumbady fault.—Tadapurtee slates.—Character 
of— Three classes of rocks,—Slaty shales.—Cleavage generally faint.— Variety 
(0 NR) 
