22 BUNDELCUND. 



Kymore shale. Similarly on the N. E. I have described the perfectly 



tranquil and conformable section of the north face of the Punwaree spur, 



having its counterpart or former extension on Chutterkote hill, and at 



Paldeo on the face of the table land immediately to the South of this 



village ; but, in going S. E. from any point of this line the Tirhowan 



limestone is not again met with. The S. E. side of the Punwaree hills is 



not abrupt except for 50 or 100 feet at top, for the rest one descends along 



the surface of sloping beds of sandstone, and in the valley of the Ohun 



the same features show in an increased degree, strong beds of sandstone 



sharply rolled about ; in the scarp of the table land on the other side 



there is no recurrence of the limestone, the table land sandstones are in 



their normal horizontal condition. The subdivisions of these are more 



apparent in the section along the Pysunnee. 



" The Pysunnee enters its narrow precipitous gorge in the table land 



about 7 miles above Chutterkote : a short way up 

 Pysunnee section. 



from the entrance is a settlement of fakeers, who ■ 



live in nests cut in the vertical cliff of massive horizontal sandstone. 

 The falls are about seven miles higher up, near the village of Bumbheea. 

 Just under the cliff of horizontal rock at the entrance to the gorge, 

 strong bedded hard sandstones dip at 20° to N. N. W. ; there is no gap 

 between this and the rocks of the high scarp. There is no very marked 

 lithological contrast, nor any separating beds exposed, so that one might 

 suppose at first that the whole mass had taken a sudden plunge ; how- 

 ever, 150 yards North of this the same sandstone is going at 50° to S. by 

 E. and at similarly short distances, the dip varies 30° to E. by N. — 20° to 

 S- and so on, showing a frequent folding and rolling of what may be but 

 a small thickness of strata ; a state of disturbance very similar to that 

 already noticed in the lower Semri groups to the S. E. After a blank 

 reach of some two miles there is just below Mohurgurh the most marked 

 case of disturbance any where observed, " there is a low vertical cliff 

 about 200 yards long — all distinctness is lost, the sandstone is completely 



