DESCRIPTIVE GEOLOGY: NUMMULITIC ZONE. 209 



is probably a fault near that line repeating the section to the south. 

 The apparent dip is north-north-west all through the gorge, being 

 nearly vertical along the stream-bed, and 40 — 50 on the Sribang 

 ridge above. The beds curve downwards therefore in a fine arc. 



The section down the next gorge from near Lunguryal to Pina, on 

 the Hurroh, is a more perfect one, and it displays the repetition of 

 the sequence better. It is — 



(1) Uppermost Nummulitic concretionary limestone and shales, and a few 



marls full of fossils. 



(2) Dark and light grey limestone interbedded with dark sandy limestone, 



slightly concretionary in upper part, well bedded in lower part. 

 Fossiliferous. 



(3) Cretaceous ....... 4 feet. 



(4) Gieumal sandstone . • . . . . 20 ,, 



(5) Trias 100 „ 



(Fault.) 



(6) Repetition of (2). 



(7) Repetition of (3) and (4). 



(Fault.) 



(8) Repetition of (2). 



(9) Repetition of (4). 

 (10) Repetition of (5). 



The whole of the beds, with the exception of 8, are dipping as 

 In the last section. No. 8 shows a rolling dip. 



I need not stay to describe the intervening sections up the hill- 

 slopes, which possess the same general arrangement of the beds, 

 but with less clearness, and with surface irregularities. 



In a south-westerly direction from the figured section No. 4, the 

 Janomar hill, 4,387 feet, carries on the structure of the hill-range. The 

 comparatively wide valley which runs between it and the Serh hill, 

 4,005 feet, north of Khanpoor, shews the free edges of the beds in 

 that direction. As a summary of various traverses across it and 

 p ( 209 ) 



