202 MIDDLEMISS: GEOLOGY OF HAZARA AND BLACK MOUNTAIN. 



that exposed along the continuation of the same outcrop south of 

 Changla Gulee : — 



(i) Nummulitic limestone. 



(2) Sandstone variegated with pisolitic-iron bed. 



(3) Thin-bedded grey limestone (small fault)* 



(4) Thin-bedded buff-coloured marley limestone, nodular limestone, grey 



and drab, full of compacted shells (passage-beds). 



(5) Spiti shales and Gieumal sandstone in several alternations and inter- 



beddings. 



(6) Trias limestone. 



As Nugree is reached, a fault, dying out to the north-east and 

 becoming more marked to the south-west, parts the last outcrop of 

 the Trias from the great expanse of Nummulitic strata with enfolded 

 lines of Kuldana beds which next sets in. 



Want of space must make me condense the account of the parallel 

 sections found in a north-east and south-west 

 direction. Fig. 26, below, gives a section from 

 the 6,545 feet hill through Hothla to the stream- 

 bed below Seer. 



Hothla. 6,545 



Parallel sections 



north-east and south- 

 west along the Maree 

 ridge. 



btream. 



S.E. 



Fig. 26. 

 a ■» Trias limestone. 

 b = Spiti shales. 

 c — Gieumal sandstone. 



d = Thin -bedded buff-coloured calcareous shales, 

 e «■ Grey limestone. 

 / = Nummulitic limestone and shales. 



( 202 ) 



