JAIPUR FIELD. 47 



stream south of Kanugdon, running parallel and close to the fault 

 between the Sub-Himalayan and Disang rocks, I picked up one or two 

 pieces of coal, which may indicate that the coal-measures are not wholly 

 obscured along this line. The fragments may, however, have been washed 

 out of the Sub-Himalayan coal-conglomerate (p. 29). 



Coal outcrops. — During the cold weather of 1874-75, Mr. Greig, of 



Jaipur, to whom I am indebted for valuable inform- 

 Tipam tea garden. 



ation respectmg the coal of that neighbourhood, 



discovered and cleared several outcrops. The most northern of these, near 



the edge of the hills at Tipam tea garden, has the following section :— 



Ft. In. Ft. In. 

 Grey shale, seen ... ... ... ... i o 



Coa?, dipping W. 30° N. at 60° ... 18 



Grey shale seen ... ... ... ,,, 3 



Two hundred yards south-south-west of the above, Mr. Greig cleared 

 another with a section as follows : — 





Ft.] 



[n. 



Ft. In. 



Grey shale, seen ... 



... 





9 



Carbonaceous shale 



... 



6 





Coal ... 



... 



9 





Grey shale 



... 1 



1 





Coal ... 



... 1 



4 





Grey shale 



... 



3 





Coal ... 



... 1 



1 





Grey shale 







1 





Coal ... 



... 



8 





Grey shale 







2 





Coal ... 



... 1 









Grey shale 



... 



4 





Carbonaceous shale 







9 





Soft grey earthy sandstone ... 



... 



.. 



. 1 6 



Grey shale 



... 



.., 



, 6 



Coal in seam 



... 4 10 





Carbonaceous shale 



... 1 



3 





Shale ... 



... 1 



11 





Total thickness of seam ... ... 8 



( 315 ) 



