DAMUDA SERIES : BARAKARS. 29 



Here we come to the mouth of the Kanjo. The section continued 

 in it, in descending ordeij is— 



Tliiu-bedded reddish brown siliceo-micaceous sandstones, and carbo- 



argillaceous shales 



by N. 60° 



Ft. In. 



43 



6 

 25 8 

 15 6 



Dip N. N. W. 



5. Coal 



6. Carbo-argillaceous shales 



7. Coal seam 

 A few yards south of this comes the boundary. 



Returning once more to the Damoodah— 



No. 3 reappears, then higher in the series : — 



a^J). Nos. 2 and 1. Thin-bedded micaceo-siliceous sandstones ,,, 20 



h. CoaZ seam. ... ... ... ... ... 29 



Ft. In. 

 CoaZ(good) ... ... ... 13 



Coal containing irregular partings 



of ironstone and shale ... 16 



e. Carbonaceous shales with black band, and thin bedded micaceous 

 shales and sandstones succeeded by sandstones containing pebbles. 



The section is then obscure to within a short distance of a nullah, 

 between the Kanjo and Jhoonjko nuddees, where a seam occurs dipping 

 at an angle of 50° and possessing a thickness of 38 feet. 



The next rocks above this coal are not exposed in the Damoodah, 

 and no intelligible section is seen until opposite the mouth of the Hur- 

 rUadeeh Nullah. 



A little west of the Jhoonjko stream, a cross fault cuts off the 

 Barakars, and brings them against metamorphic rocks in the bed of the 

 Damoodah. In the Jhoonjko Nuddee no strata occur near its out-fall, 

 but on going up it, the seam h of the above section shows in the bank 

 of the river, and also No. 3. The boundary exposed in the Jhoonjko is a 

 natural one, and pebble beds are seen resting upon the gneiss. 



The throw of the south fault near Angwalee is not great. This 



can easily be shown to be true, because, in the Jhoonjko, there is an 



unbroken succession from the conglomerate to the two seams which are 



visible in the Damoodah, so that the fault cannot exceed the thickness 



of strata included between them. Some indistinct outcrops occur west 



of Angwalee. 



(67) 



