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DAMUDA SERIES : BATIAKABS. '57 



Dip W. N. W. 



Exti'cniely fine grained pale yellow sandstones 



A small tault lets down this carbonaceous sliale, the depth of three feet. 



Carbonaceous sandstone ,.. 



Purple felspathic micaceous sandstone 



Carbonaceous shales 



Sandstone (about) 



Carbo-siliceous shales ... 



Felspathic sandstone at ghat where Ranchee road crosses the i-iver 



On the west side of the Ranchee road the ironstones come in once more, 



Mver east of Mando. — At the mouth of the river, east of Mando, 

 Bardkars occur; but after an interval ironstones come^in. A turn of 

 the river re-exposes BarakarSj and a fault is seen, heading north of west. 

 At the fault is a seam of coal very much twisted and disturbed. Going 

 up the river another seam dipping at an angle of 10° is exposed. The 

 thickness is about 10 feet. 



Coal near Bunwar. — South of Bunwar In a small stream which joins 

 the Hoharooj a seam occurs 10 feet thick. 



Coal near Mungurdoolia. — A river west of Mungurdooha contains 

 some seams. None of them appeared to be of even average quality, 

 although quite fitted for burning bricks; and so I measured none of them. 



Nearly opposite Toeera to the north some seams occur near the 

 boundary, which passes north of the Hoharoo. In the Hoharoo itself 

 two seams are exposed near the western boundary. 



Dutman. — Coal crops out north-west of Dutman. And one or two 

 seams in the vicinity of Kodway. 



The Barakars are exposed in a river north of Kodway, which 

 is not marked on the revenue map. The dip of the beds is north-east 

 to north-north-east. 



I have no other information to afford regarding the localities in 

 which Barakar coal occurs. I am aware that all the outcrops have not 

 been mentioned, and that there are two or three nullahs whose sections I 

 have not referred to. These, however, as was previously explained, were 

 only at a short distance from other rivers, whose sections I had given, and t 



( 95 ) 



