Stone Implements in latevitic formations. 7 



The Implement was imbedded in bed " c." 



Fifteen or twenty yards further down the gully, I came 

 upon a large hatchet shaped Implement (Plate XII) lying 

 in situ on the here exposed top surface of the bed c } fully 

 six feet below the general surface. 



The banks of this gully and its tributaries show in several 

 places two distinct beds of latevitic conglomerate divided 

 by sandy clay corresponding with the bed c of the pagoda 

 gully section — in other places the sandy clay is absent and 

 but one bed of laterite seen. 



About \ a mile eastward of the spot where the above two 

 Implements were met with, and a little below the junction 

 of the Kalingula gully with the main stream — another sec- 

 tion is formed by a small gully running northward, 



The beds seen in this section are : — - 



a. Vegetable soil 2 U — 3 U , 

 a\ Loamy sand 10 u . 



b. Latevitic gvavel 9 U . 



c. Clayey sand with much kunkuv and a few pebbles of 

 kunkuv and laterite V — 4?\ 



d. Lateritic conglomerates with Implements. 



e. Plant shales with kunkur infilteration V — V . 



On the face of the bed e at this place a large, and rather 

 water-worn implement was well exposed, but the non-ex- 

 posed part was so firmly impacted in the conglomerate as 

 to require several blows from a rather heavy hammer to 

 detach it. A few yards to the north two other Implements 

 ^ere extracted from the same bed in which they were also 

 firmly imbedded. 



A Gradual thinning out eastward of the lateritic deposits 

 from the pagoda gully section can be distinctly traced, and 



