NEIGHBOURHOOD OF lULABAGH. 



39 



glomerate above. This conglomerate is so largely composed of carboni- 

 ferous, eocene, and other limestone pebbles, it can be readily distinguished 

 from the Siwalik metamorphic-pebble conglomerates which also occur in 

 the neighbourhood. It is disposed partly in a basin-like form tilted con- 

 siderably to the west and nearly horizontal on the opposite side of the 

 exposure capping the hill. 



The rocks forming so much of the sequence as can be traced in 

 this part of the hills, and, combined with the 

 list previously given in the Salt Range Memoir 

 (partly from Dr. Waagen's notes), page 273, show the following suc- 



Section. 



cession : — 



POST- TERTIARY 



Pliocene 



Miocene 



Eocene 



Cretaceous 



... Limestone boulder conglomerate ... 



Unconformity. 

 .. Brown clays and gray sands, Siwalik ? 



Unconformity. 



fEed clays and gray sandstones, Murree or' 

 " i Nahan? 

 fNummulitic limestone (part of) ,.. 

 Soft gray -marl 

 Thin-bedded marly limestone 

 Ashy-gray calcareous marl with numerous 

 Conoclypeus 

 , Alum shale, inferior quality, a little coal, and 

 many fossils 

 Yellow nodular limestone, irregularly bedded, 



many Nwmmulites 

 Alum shale with Nummulites (many pits, but 



few workable beds) 

 Haematite ... ... 



e Dark gray glauconitic sandstone with Belem- 

 X nites, badly seen ... 



up 



to 500 feet.. 



About 9,500 



>r 



About 400 



»■ 



50 to 60 



» 



20 



feet. 





15 



» 





20 



to 30 feet. 



20 



to 30 



M 



10 



feet. 





50 



» 





10 



a 





200 



feet. 





10 



n 





10 



feet. 





249 ) 



