204 MIDDLEMISS: GEOLOGY OF HAZARA AND BLACK MOUNTAIN. 



The appearance of the section along the hill-spurs to the east is 



as shewn Fig. 28 drawn in per- 

 spective from north-west of 

 Chinali village. The apparent 

 dip must not be confounded with 

 the true dip, which is nearly ver- 

 tical, but waving. 



A very similar section is found 

 along the path from Loruh to 

 Trimun ; but south-west of this 

 a change takes place; the south- 

 ern Trias band continues intact 

 to Hullee and beyond, but the 

 northern band vanishes under 

 undulating folds of the Jurassics 

 which, over a large area near 

 Maira and south of Rahee, are 

 badly exposed in rough and 

 complicated country. 



Uniformly in all these parallel 



. 2 1? sections illustrative of the struc- 

 V. « 



"g ture of the long hill-range above 



1 £ g, Nugree, there is a complete 



J 'f £ o absence of the Cretaceous band. 



s rt o «*- 



B " o ° All endeavours to fix it among 



- I V £ 



2 a S £ some one or other of the chrome- 



•c .2 *s i2 



coloured bands failed, for not a 



single characteristic fossil, so 



profuse on the other side of the 



Hurroh R.j was detected. On 



the other hand, the incoming 



of a calcareous element among the Gieumal sandstone, and the 



development of a zone of compacted shelly limestones and 



buff-coloured thin-bedded shaley limestones further shew that 



( 204 ) 



H O o 



d a 1 



