200 MIDDLEMISS : GEOLOGY OF HAZARA AND BLACK MOUNTAIN. 



Fig. 25 below gives the structure along this line. 



With regard to it, the chief 

 point of interest is the expo- 

 sure of Cretaceous rocks at 

 Jubriyan, from which the bet- 

 ter part of the collection of 

 Cretaceous fossils was made 

 by Hira Lai and myself. The 

 rock is abundantly exposed in 

 the low hills to the north of 

 the village, and its more dis- 

 integrated state at one point 

 enabled us to secure some fair 

 specimens. The northern of 

 the two bands of Trias, shewn 

 .as a lying anticlinal in the 

 * sketch section, dies out a little 

 £ further to the west-south- 

 west. As regards the south- 

 ern band it is difficult to say 

 what becomes of it under the 

 dense forest-covered slopes of 

 Doobran, but it seems also to 

 die out there in some way. 

 The Trias band below Jubri- 

 yan is a third band beginning 

 at Jubriyan. It will be men- 

 tioned again later. 



For the present we have 

 gone as far aside from our 

 main line of section repre- 

 sented in horizontal section 



No. 3 as it is prudent to do, and we must now return to it where 



we left at the ascent of the hill-side to Maree. 1 



1 This place must not be confounded with Murree, although both names in the 

 Hunterian sj b m would be written Mari. 



( 200 ) 



