BUNDELCUND. 17 



varying in thickness from 10 to 12 feet; its junction with the granite 

 does not make a marked line although weathered vertically, the breccia 

 fills the irregularities in the surface of the granite like concrete : im- 

 mediately over this massive bed, green flaggy sandstones come in without 

 any transition or unconformity : the fine thick beds show at top." 



The actual junction with the granite may be well studied at the N. 



point of the small flanking hill, just over Sun- 

 Sungrumpoor hill. 



grumpoor — " an actual contact ot coarsely crys- 

 talline and of compact granite with a 15 feet bed of the nondescript stuff 

 is here seen. The calcareous element is here more prominent, the 

 bottom of the bed is charged in places with blocks both angular and 

 rounded of the granite, and cracks in the granite are filled with the sandy 

 and calcareous covering rocks; just below this point an earthy trap is 

 seen filling veins in the granite." — (See Fig. II.) 



Fig. II. Section of point over Sungrumpoor. a , thin flaggy sandstone ; b, the massive 

 calcareo-siliceous rock, about 15 feet ; c, a hard felspar rock ; d, coarse decomposing 

 granite ; e, the limestone vein. 



This junction would, I think, yield most interesting results to a close, 



mineralogical examination, especially attractive to 

 Chemical changes. 



such investigators as Daubree, Kuhlman or 



Delesse. There is no reason to suppose that these rocks have ever been 



subjected to much heat; there is no sign of mechanical disturbance, the 



trap which shows so abundantly in the granite as an intrusive rock, is 



