132 WYNNE : TRANS-INDUS SALT REGION, KOHAT DISTRICT. 



the Manzulli and Band£. range (see page 110). Fig. 30 is a diagram- 

 matic sketch of the structure seen on the left bank of the stream here. 



13. Red clays and greenish-gray sandstones in thick alternate zones, more sandstone 



than clay. 

 12. Gray and purple sandstone and thin clay layers. 

 11. Red clay 15 feet in deep blackish purple thin sandstones. 

 10. Purple and gray sandstones and red clay. 

 9. Red clay much thicker in opposite bank of stream. 



Crushed line of junction, 



8. Hard dun Alveolina marble 6 to 20 feet. 



7. Green clay. 



6. Gray and white gypsum 15 to 20 feet. 



5. Green clay, weathered olive. 



4. Dark, cherty limestone with a flat-coiled shell like a Planorbi? solarium, a 



couple of feet. 

 3. Dark-olive shaly clay, in places blackish. 

 2. Dull-red clay passing towards (1) into a purple, earthy, coarse sandstone with 



ferruginous base 1 foot thick. 

 1. Red clay v 



The junction of the red clay No. 1 with the gypsum of the in- 

 terior is concealed, but at a little distance to the northward the latter is 

 seen overlying black alum shales, with thin pieces of bituminous, hard, 

 black, flaggy limestone scattered over their surface, apparently derived 

 from the dark bituminous parts of the adjacent gypsum. The alum 

 shales, from their decayed state, are evidently pyritous, and native sul- 

 phur in small quantities was observed in their planes of division. 



To the eastward of this place the axis of the anticlinal seems to lie 



Eastern part of the very much towards the north side of the ellipsoid, 



on the southern side of which a large mass of the 



tertiary sandstones has been apparently let in below the general surface 



of the nummulitic beds, and the contortions of the latter are seen to 



form strange elongated zigzags on the mountain side between the high 



tertiary ground and the eastern end of the hill. 



( 236 ) 



