254 WYNNE : GEOLOGY OF KUTCH. [PAET II. 



Ft. In. 

 12. Paeudo-conglomeritic concretionary bed with spongiform organisms, 

 Nmnmulifes scahra, Tapes nonscripfa, Fleurotoma Voyse^i, 



Natica, &c. ... ... ... ... ... 3 



11. Blue, gray, argillaceous streaky sands with some soft yellow mud beds 20 



10. Ferruginous nodular beds with fossils, a fish tooth, a Venus, &c. ... 10 



9. Greenish silty beds with ferruginous concretions — more than ... 8 



(Similar beds to these soft silty variously coloured sands undulate 

 for a mile south of Waieor. They are believed to represent the leaf 

 beds near Bayr, for although no leaves could be detected in them here, 

 these were found again in the next stream section to the eastward) . 



Some ferruginous sandstones at the village, with annelid tubes, are 

 supposed to underlie these (No. 8); beneath them are — 



7. Pale yellowish marl stone and fine sands and plastic clays ... 20 



6. Marly sandstone with fragmentary shells ... ... ... 20 



5. Obliquely laminated red and purple soft mottled sandstone ? thickness 12 

 4. Hard buft' marly limestone, lower part rubbly, and white foramini- 

 ferous organisms, small Fectens, large Gastropods and bivalves, 

 corals, &c. ... ... ... ... ... 10 



3. Yellow sandy marl, parts raggy, corals, &c. .. ... ... 8 



2. Brownish, gray, granular or oolitic soft sandy beds, part seen ... 12 



( Slight break). 

 1. Solid, white, marly limestone with much coral, the upper portion of 

 the nummulitic series. 



The last bed is seen flooring the stream course north of Waieor. 

 The ground near Cheroperee, where the above section commences, 

 is low, and passes gradually into the alluvial 



Plain north of Jukow. 



plain north of Jukow, in which the stream from 



the Teyrah and Mhurr basin seems to have wandered from an older 



channel. 



The prominent hill of Saheind rises, by two or three terraces on 



the outcrop of its strata, south of the village of 

 Saheind hill. 



Wallusera, to a height of over 300 feet, slopmg 



o-ently to the southward on the dip and with steeper declivities to the 



easb and west. At the top of the hill is a black ferruginous gritty bed 



with hollow nodules, overlying a large thickness of soft yellow sand- 



( 254 ) 



