ii 
KING: KADAPAH AND KARNÚL FORMATIONS. 
at Kurnool.—Shore-beds, Mr. Foote's notes.—Evidence of Kistnah valley 
being older than KaRNULS.—Indefinite position of sandstones and breccia 
beds.—Unconformity of Jummulmudgoos on strata of Gundycotta hills.— Lime- 
stone, grits and conglomerates.— Denudation.— Thickness 
CHAPTER 4.—Banaganpilly group.—Quartzite sands and grits.— Might be called 
the Diamond group.—Relation with other groups.— Thickness variable, but 
small.—Lie.—Distribution.—Mr.  Foote's notes.--Doubtful beds.— Possible 
strata of KADAPAH series.— Outliers between the Paupugnee and Chitra- 
vutty.—Character of strata of the group.—Diamond beds.—Banaganpilly 
mines.—Stratigraphy of Banaganpilly.—Moonimuddagoo mines.—Gooraman- 
conda.— Busswapoor.—Ramulkota.—Other localities 
CHAPTER 5.—The Palnád Beds.—Extreme north-east area of KARNUIS.— Great 
obscurity in grouping the strata.—Analogous to relations of limestone on east 
side of Khoond-air valley.—BStrata of western part of Palnád nearly identical 
with KARNUÍ rocks.— Further small detached area on the Kistnah plateau.— Lie 
of Palnád strata.— Traces of diamond beds.—Cleavage in Palnád limestone.— 
Deceptive succession of strata.—Apparent strike of beds not parallel with 
shoreward edge.— General dip eastwards under quartzites of eastern ridges,— 
Exceptions to this.— Considerations on this obscure stratigraphy.—Attempt 
at solution.—Palnád limestones may be partly of both formations.— Lines 
of separation unrecognizable.— Karempudi break in succession of strata.— 
Continuity of outcrops broken by  cross-faults.— Outer eastern boundary 
faulted.— Downthrow of rocks on west side with a hade to eastward.—Mr. 
King's idea of the relations of Palnád beds.—General unconformity of lime- 
stones on the quartzites beneath.— Conclusion 
PART III. 
CHAPTER l.—KADAPAH FORMATION.—KARNULS rest quite unconformably on 
another series of rocks.—Sections showing general unconformity.—Series, a 
complicated succession of quartzites and slates.—Divisible into four groups.— 
Kistnah Beds.—Nullamullay Beds—Chey-air Beds.—Paupugnee Beds.— 
Difficulties in grouping the series.—Lie of strata.—General easterly dip.— 
North-south undulations due to original form of floor.—Conditions under 
which the deposits were formed.—Thickness of series.—Faulted eastern edge 
of field.—Any natural boundary concealed by eastern talus.— Abruptness of 
boundary not necessarily due to faulting.— Sections showing abruptness of 
boundary.—Mr. Foote’s notes on eastern edge of field.— Other, and cross- 
faults.—On the Chey-air.—East side of Khoond-air valley.—Kirkumbady 
fault.—Calastry ridge.— The Palnád.— General character of slates.—Of quart- 
zites.— Natural grouping of series in bands of thin strata.— Series, a mineral 
producing one.—Difficulty in describing KADAPAHS in descending order.—An 
apparent triple grouping in parts of the field.—Series to be described in 
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PAGES. 
67—86 
87—106 
. 107—123 
