164 KING: KADAPAH AND KARNÜL FORMATIONS. [PART III. 
and traps, in which apparently the same outcrop of trap runs in between 
all these strata; but there is a good deal of contortion and some faulting 
(connected with the evident lines of dislocation to: the east) which makes 
the succession of the beds very doubtful. On the whole, however, the 
trap certainly appears at this point to be intrusive. 
The sudden dying out of these trap sheets, both in this last locality 
and in the limestone terrace below and north of Puspulla Gonda or Conda 
in the Camlapoor valley, is hardly consistent with the generally easy 
and uniform succession of the rest of the strata. 
In the Paupugnee valley, the limestones and slates or slaty shales 
Alterations of limestone, 11 immediate contact with the traps are altered in 
&c., in contact with trap. 4 marked manner. They are stringed with white 
and pink seams, patches, and knots of a rock of serpentinous or mag- 
nesian constitution easily weathered into a white powder. Occasionally 
these seams are of pale green color, and are then a calcareous serpentine. 
The lamination of the beds in contact is undulatory and wavy: and the 
more massive and silicious limestones, not in such close contact with the 
traps, are much segregated in what appear on the edges of the beds to 
be corrugations. On the surfaces of the beds, however, it is seen that 
these corrugations are merely sections of rude columnar segregations. 
A 
AA ART 
Figs. 24, ره‎ b. Surface and section of a block of corrugated or segregated limestone: the walls and 
concentric laminz are of silica, 
(Lede 9) 
