THE LAKI RANGE, ETC. 125 



Nari beds, the characteristic yellow and brown limestones with Nummti- 

 lites garansensis, N. suhlcevigata, Pecten labadyei, 

 8fc. In one place at least, a spot called Seri, 



about 8 miles south-east of Jhangar, where a very small sprino- of 



fresh water breaks out not far from the path to 

 Unconformity between t . L 



lower Nari beds and va- the Dharan pass, there is distinct unconformity 



between the two groups. The yellow Nari lime- 

 stone with Foraminifera, and the shales intercalated with the limestone 

 have been denuded, and the variegated beds rest on the denuded surface 

 the stratification of the two groups not being parallel. l 



It is thus evident that there is a break in time between the lower 

 Nari beds and the variegated clays and sandstones. The latter may 

 nevertheless belong to the Upper Nari group, or they may be considered 

 a lower portion of the Gaj formation. The former being, perhaps, the 

 more probable view, these beds have been mapped as Nari. The im- 

 portant point is that there is here denudation-unconformity between 

 lower Nari beds and strata elsewhere conformable upon them. 



The lower Nari beds of Bhagothoro Hill are highly fossiliferous, and a 



large collection of well preserved specimens has 

 Fossils m Nan beds. 



been made. The following, exclusive of Foramini- 

 fera, are the principal forms found :— 



Corals. 

 Trochocyathus burnesi. Montlivaultia vignei. 



ECHINODERMATA. 

 Cidaris verneuili. JEupatagus rostratus. 



Ccelopleurus forbesi. Schizaster beloutchistanensis. 



Clypeaster, sp. S. cf. neioboldi. 



Lamellibeanchiata. 

 Corbula harjpa. Chama, sp. 



C. cf. dubia. Pecten labadyei. 



Venus granosa, par. P. cf. JiopJcinsi. 



Cardium cf. triforme. Ostrea ci.Jlabellula. 



1 These details and the list of fossils, with several other parts of the description, arc 

 from Mr. Fedden's notes, 



( n$ ) 



