NERBUDDA DISTRICT. 



169 



.*=> 



£ 



F N 



1. — The conglomerate of the Mahacleva group nearly hori- 

 zontal, overlies, unconformably, the lower Damuda 

 rock. 

 2. — 50 feet of grey thick bedded sandstone with bands of red 



and blue shale — dip 1 5° — E. 5° N. 

 3. — 10 feet of coal. 



4. — 30 feet of hard grey micaceous flag stones. 

 5. — 16 feet, 7 feet grey and blue shales; 2\ feet earthy- 

 coal; \\ feet sandy grey shale ; 5 feet coal ; dip — 25° 

 E. 35° S. 

 From 5 to 7, 180 feet of sandstone — flags, some being hard 

 micaceous, and some coarse and friable, and some bands 

 pebbly. 

 6. — 6 ; places where shales occur among the above; at 

 both the shales are very carbonaceous, and at one there 

 is a thin layer of coal ; in both the shales contain vegeta- 

 ble impressions. 

 7. — A trap dyke. 

 8. — A break in continuity ; may be caused by a small 



fault. 

 9. — Green mud and earthy sandstone, boulder bed, and con- 

 glomerate. Dip irregular, but reversed to the N. 

 -Trap dyke, probably marks a small fault, the beds to 

 the north of it dip at a much higher angle than those 

 to the south. These seem to be the same; both are 

 earthy sandstone. 

 -Coal 4 feet. 



Close to this coal band a bed of brown earthy sandstone 

 abounds withGlossopteris and Phyllotheca, some blue and grey 

 shales are associated ; these beds are vertical. 



12. — The above beds pass on into other similar strata which 



begin to dip S. 

 13. — The same beds apparently now dipping K 

 14. — Trap lying against them. 



10.- 



11.- 



K 



