BUNDELCUND. 25 



The supposition I am in favor of reconciles some of these difficulties, 



though introducing the new one regarding the 

 Original limitation. 



limestone itself. Such rocks as those of the Ohun 



valley and in the Pysunnee, would come in rather naturally as lower 

 Semri rocks, analogous to the Dulchipore group, to the S. W. Indeed 

 they rather identify themselves with these rocks through that limestone 

 in the Pysunnee, which I am disposed to consider the Semri limestone. 



Although I endeavoured to show that the Vindhyans betrayed no symp- 

 toms of faulting, it can hardly be denied that they in some degree partake 

 of the peculiar disturbance of the lower rocks, and thus they help to 

 point out what the nature of that disturbance may have been. When 

 overlying the Tirhowan limestone, the sandstone shows no disturbance ; 

 still, slightly modified and contorted beds of sandstone are often found 

 close to and on the same horizon as the limestone beds, and which must 

 be considered of later date than the limestone, and the characters of 

 which seem to pass into unchanged Kymore rock. This is well exhibited 

 along the N. W. face of the extension of the Punwarree spur beyond 

 Kole, " a low hill E. by N. of Kole point shows the same section, the 

 limestone is capped by sandstone ; over the village at the next point is 

 the same section; in these the limestone does not reach to more than 100 

 to 150 feet from base: beyond this the most Southern of the E. N. E. 

 ranges shows only sandstone, and the bottom beds seem very much 

 altered ; this is just South of Simurea, and E. by N. of same, a spotted 

 sandstone is going S. 40° E. at 20° and considerably intensified : just 

 above Beor, the rocks are better seen, the sandstone rolling confusedly — 

 at 50° to N. W. and N. and S. &c." 



This troubled condition continues along this ridge. " The next is a 

 higher hill, and, just South of Bhowree, the limestone shows for a small 

 thickness apparently horizontal, but broken and with much of the agate 

 breccia about it ; but again just N. E. of Bhowree the sandstone shows at 

 base rolling as before — beyond this again, the limestone comes out ou 



JE 



