iiUTAR field: mahadeva series. 107 



southern and western boundaries appear to be continuations of the Bijka 



and Binda faults, which would intersect one an- 

 Sitwaliill outlier. 



other near Kajuri. 



I have on the map indicated the probability of the Bijka fault 

 being continued to Tatapani, but am as yet by no means certain that it 

 is so. 



The lithological characters of the rocks forming this outlier are 

 normal, i. e., identical with those of the adjoining main area. 



( 107 ) 



