198 W. BLANFORD, WESTERN INDIA. [PaRT II. 



South of the Euttunpoor stream very little rock is seen as far as 

 Eocks near Dholekoowa, *^® ^^^* watercourse, the Kaverec. About Dhole- 

 *''• koowa agates abound on the surface, and frag- 



ments of conglomerate are met with, though no rock is seen in place. 

 Further to the south-west, more conglomerates are seen; the edges 

 of beds, with a high dip, cross above the surface in the continuation 

 of the line of the Euttunpoor antichnal. 



Further to the south low dips prevail, with a general direction to 

 north-west or north. 



E-eturning to the trap boundary near Dumlahee and Padwani very 



n.-r . 1.1. -u ^ r J. few rocks are seen, and the boundary itself is, in 



Neighbournood of trap ' j ' 



boundary near Padwani. places, obscure. Fragments of conglomerate, of 

 laterite and of a white calcareous sandstone, are seen scattered about. 

 East of Padwani laterite is seen, and a little further east, fossil wood 

 in abundance, but rather ill preserved. All the interior portion of the 

 stems is generally replaced by crystalline calcspar. 



Where the nummulitics rest upon the trap they consist of argil- 

 laceous beds with small trap pebbles, and have a 



Basement beds. , . m t n ro , no 



low westwardly dip oi 5 to b . 



In the Kaveree, the section which is exposed is somewhat similar to 



^ that seen in the stream which flows past Euttun- 



Section m Kaveree 



near Wasna, poor, but it is much less continuous, and more 



laterite occurs, especially about Wasna, where the dip is very low. 

 Where the laterite beds are cut into by the stream west of the village, 

 they so closely resemble decomposed trap as to be undistinguishable, and 

 are very probably formed of trappean detritus. Another thin ferrugi- 

 nous bed, closely resembling decomposed trap, is seen resting upon white 

 and lilac shales at the village of Wasna. A similar bed, probably 

 identical, is again seen, similarly associated with white and purple shales, 

 about a mile to the south, in a small nulla, where no continuous section 

 can be seen, and where the surface is covered by alluvium. 

 ( 360 ) 



