112 MIDDLEMISS: GEOLOGY OF HAZARA AND BLACK MOUNTAIN. 



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Cretaceous, the 

 thin-bedded Grey 

 limestone and pos- 

 sibly some of the 

 Nummulite-bearing 

 limestone also, form 

 the rather steep and 

 rough hill-side lead- 

 ing to the top of 

 the ridge. 



Leaving the 



higher parts and 

 continuing on to- 

 wards Nugukkee 

 we cross a band of 

 the Trias as an 

 anticlinal, sharply 

 reflexed, and then 

 come upon all the 

 Jura- Cretaceous 

 and Nummulitic 

 series again in a 

 | slightly inverted 

 ~ | £.!!'* position. The Spiti 

 I u o w 5 shales here yielded 

 II f some fairly perfect 

 specimens of am- 

 monites and belem- 

 nites collected by 

 Hira Lai. This Jura-Cretaceous band continues north-north-east and 

 joins up with the band in the glen going towards Shakur Bandee, 

 where a marked depression in the hill-side (about the position 

 of the word Ookhreeluh on the map) reveals its presence. The 

 accompanying sketch-section shows its position and the rocks 

 below and above. 



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