DELHI QUARTZITE SERIES. 8i 



cisive as to dip, though the strike was plainly indicated as being 



N.N.E. — S.S.W. along the ridge and also along the foot-hills. 



A climb, over the main ridge from the west and then down the 



steep spurs to Chorivad, revealed the impossibility of gauging the 



dip, though the outcrops continued down in that direction as if 



the bedding were steep, which is very likely to be the case. 



In connection with these exposures should be mentioned the 



. , . outlying patches of Delhi quartzite at the 876 



Outlying patches. "in .1 -i * 



teet knoll, If miles east of Medh, and the 



842 feet knoll, at 2$ miles S.E. of Vadali. They reveal no 



structure. 



A noticeable feature about the four localities referred to in th c 



,„ . ,. , area N. of Chorivad, is the slightly plamo- 



Plagioclinal range : ,. , . . & J * ° 



four strike masses. clmaJ nature ol the hill-range from north of the 



Ilarnav R. to Chorivad, whereby one can recognise 



as composing it four slightly differently-behaving strike-masses 



(A, B, C, and D of the diagram text fig. 13) which traverse obliquely 



/ 





/ ' 

 / / 





/ A , 



PLAN 







/ ' 



N 



/ / 





/ / 



1 



^ 



' B ' 

 1 t 

 1 4 

 t '* 

 A ^.' 1 ' 

 1 / / 

 / / / 



/ to* 





' ' ,4 





A ' '/ 



^ 



-— * / ; 





/» 





/ 





1 





1 





1 





1 

 \ 







Fig. 13. 



/ 

 / 

 / 



I 

 / 

 / 

 I 

 I 



across the range. There is the mass east of Walren (A), there is that 

 composing the western and middle spurs in the Harnav river-bed, which 



