Geological Notes on the Khasi Hills. 



[No. 1, 



dip of the gneiss is very marked, in a white coloured soft band that 

 crops out at the very base of the hill, and is continued E. S. E. past 

 the village of Laoburtun. 



From all I could see of this formation here, the Mokasa valley, 

 lies on a very sharp anticlinal bend of those gneisose rocks, the 

 granite appearing to curve over the Maotherichan ridge. 



^ The rock near the summit of Maotheric- 



han is very porphyritic, containing large 

 oblong crystals of felspar. In the valley it 

 disappears, and coloured gneiss, soft and 

 friable, comes in, to which is very probably 

 due the present configuration of the valley. 

 To the south near Mahaton, the porphyritic 

 granite is again seen, with a corresponding 

 rise in the hills. The above kind of granite 

 is very common about here, forming as a 

 rule the lines of the higher ground and ele- 

 vated masses ; it is of a very hard nature, 

 | often pink, and is generally used by the 

 § people for the monoliths set up beside the 

 f ashes of their dead. 



» On and about the summits of the low 



s- hills, south of Maotherichan, that rise some 

 ► 150 feet above the present level of the rice 

 bo cultivation, or what was originally the bed 

 4 of a lake, I was surprised to find, scattered 

 =< over the surface, a few well water-worn 



2 pebbles, mostly of a hard quartzitic rock. 

 » No beds exist anywhere near from which 

 g such well-rounded pebbles could have been 



3 washed, and I was quite unable to account 

 for their appearance. They were not nume- 

 rous, but sufficiently so to preclude the pos- 

 sibility of having been carried there by hu- 

 man agency, the nearest spot whence they 

 could have been brought was the bed of the 

 valley below. No well marked traces of any 



