SEC. 3.] WAGTJR, E. KUTCH. 133 



On the south side of the contortion above the sandstones forming 



the centre of the curve are hard 



ih 





calcareous rocks against which 

 rests a quantity of soft calcareous 

 and sandy white clay the bedd- 

 ing of which is very difficult to 

 detect, though somewhat harder 

 portions seem to align themselves 

 S parallel to the nearly vertical beds 

 g close by. This rock, if vertical, 

 g must have a thickness of nearly 

 I 100 yards, which does not re- 

 B appear at the north side of the 

 ^ curve ; it is therefore more likely 

 I that this mai-ly deposit belongs to 

 -2 a later period, and in the absence 

 I of the laterites it may represent 

 I some of the unconformable ter- 

 5" tiary rocks. 



•2 Similar sandstones and shales 

 I Adhooe to with ferruginous beds 



J Badurghad. , , , 



00 undulate over the 



^ country north of the anticlinal be- 

 tween Adhooe and Badurghud, 

 the fossiliferous band of Adhooe 

 reappearing south-west of Wassi- 

 tooa on the south side of the con- 

 tortion and nearer that village, 

 with dips which would indicate 

 either a fault or sharp double bend 

 along the line of strike. 



( 133 ) 



