54 ball: geology of the rajmehal hills. 



In the absence of good series of fossils either in the typical Maha- 

 devas or these Dubrajpiir rocks, we have little besides lithological resem- 

 blances and physical relations to other known rock groups to enable us 

 to correlate them together. The evidence afforded by these two charac- 

 teristics is, however, distinctly in favour of the view, that the rocks belong- 

 ing to the Dubrajpur group represent, locally in the Rajmehal hills, the 

 upper Panchets or lower Mahadevas of other parts of India. 



( 208 ) 



