AHMEDNAGAR (HIMATNAGAR) SANDSTONE SERIES. 141 



Geological Survey laboratory, its specific gravity was found to 

 be 3-94 and it yielded 7 per cent, of water (see also p. 148). The 





=/Vgf ~:<fk+££=2±*Shaly Setnaf stone 

 g f t T=}-t^h-' ■ J-L-^-^V^ e r ne//j i t non ite 



finjg ctTtrJ Wfiite \ 



Freestone 



Fig. 21 



■Aflu&iian 



t 

 I 



£ym'v :; %h::v*s?\ mfIt ' 



Hr/j-rf i e rruginon. t ? 



Co/tyiotn & cend art'/ 



Fig. 2G. 



DERIA 



-A//nviu/n 



Fig. 27. 



only part which forms a bed 1 to 2 feet thick, is very sandy or 

 siliceous at its upper surface (specimen No. ^ 2 \) and suggests a 

 very ferruginous porphyry with entirely silicified patches that often 

 present the contours of porphyritic felspars. Globular concre- 

 tionary masses, somewhat impure also occur. 



In the quartzitic or silicified conglomerate forming the little 

 hill near the granite, 2 miles N. by E. of 

 Ahmednagar (jffo) there are a few dubious 



Plant remains ? 



