TRANS-INDUS HILLS. 



878 



severe sickness prostrated tbemj and limited their labors until it was, 



found necessary to leave tbe place. Durincj one of 

 Section. _ "^ ^ f 



these visits, however, Dr. Waag-en, with difficulty, 

 made his way to the mountains north-east of Kalabagh and noted the 

 following succession"^ : — 



NxrMMxriiTic 



Cbetaceous 



fNummulitic limestone (part of) ... ,.. ... 50 to 



Soft grey marl 

 Thin -bedded marly limestone 



Ashy grey calcareous marl with numerous Conoclypeus 20 to 

 Alum-shale, inferior quality, with a little coal and many 



fossils ... ... ... ... ... 20 to 



Yellow nodular limestone irregularly bedded : many 



Niimmiilites ... ... 



Alum shale with Nummulites (many pits, but only 



a few beds workable) 

 Haematite 



. Dark grey glauconitic sandstone with Belemnites, badly 



60 feet. 

 20 „ 

 15 „ 

 30 „ 



30 „ 



10 „ 



50 „ 

 10 „ 



10 „ 



Jtjeassio 



TJncontoemity. 



r Grey clay with gypsum in thin beds, numerous canali- 

 culate Belemnites and Pleurotomaria ... ... 6 to 10 



Yellow marly limestone, numerous Mi/tili and other 



bivalves ... ... ... ... ... 20 



Ashy grey nodular marls ... ... ... 6 



White hard splintery limestones ... ... ... 10 



Yellow thin limestone with Fecten and * indistinct 



Myacites ... ... ... ... ... 50 



Variegated sandy clays ... ... ... ... 10 



Sandstone and limestone in alternating layers ... 30 



Soft yellow sandstone with whole beds of fossils ; 



Nerinma, Cerithium 2ia.dihiva\.Yes ... ... 50 



Variegated sandstones and shales with thin coaly layers 

 i_ and alum-shales on three horizons ... ... 300 



* Portions of this section are three times repeated by faults and contortions. 

 Besides the unconformity and irregularity it shows, there is also the unconformity of the 

 tertiary sandstones upon some of the above beds in other places, and upon the salt-marl 

 on the right bank of the river at Kalabagh. 



l3 { 273 ) 



