SEC. 10.] NORTH-WESTEEN KCTCH. 251 



Serpiilce, 8j-c., together with whole bands made up of 0. muUicostata 

 and Placuiia sp. 



This part of the coast is bordered by very high sand-hills extending 

 naore or less continuously from Nariensir to Ukree. 



The highly fossiliferous beds just mentioned extend through the 

 country to the eastward. 



At the village of Ukree^ rugged, yellow, earthy limestone nearly 



horizontal appears from beneath the sand-hills. 

 Ukree. _ 



It contains numbers of Ostrea and Pectens, casts 



of large Stromhus, and forms a characteristic band frequently met with 



in the plains to the east. It occurs again near the village of Janor 



beneath the thick detrital deposit, largely formed of nummulites 



already alluded to, and which is very prevalent over much of this part 



of the district. 



Friable fossiliferous beds underneath the former contain a band, in 

 which small EcJiinoderms, such as Temnojileurus Hooheri, occur abun- 

 dantly associated with fragments of coral, TrocTiocyathus, ^c, small 

 Echinanthus, some Cidaris spines and a few shells. 



Lower in the series are some earthy flags, with minute Foramini- 

 fera, Cupularia, Nummulites spira, Pecten Favri, Oysters and very small 

 Gastropodous shells. 



Another fossiliferous band underlying these is associated with a 



compact arenaceous limestone and some soft 

 Ramwara. 



sandstones near Ramwara old fort. 



Northward of this some lower ground is occupied by thick 



unconformable detrital deposits, beneath which in 

 Leaf beds near Bayr. 



the neighbourhood of Bayr, a broad band of blue 



shaly clays containing the small crab Typilobus granulosus, n. sp. Stol. 



(Pal. Ind., Series VII, PI. Ill, Figs. 3 to 5), and minute bivalves found 



on the same horizon as before mentioned east of Goer, is traceable for 



( 251 ) 



