33 
ELKSTONE 
No. 1.—Scraper. Dense flint. 
5, 3—Scraper. Flint. 
»» %—Scraper. Cherty flint. 
» 8—A partly formed large Javelin or Arrow-head. 
Cherty flint. 
No. 10.—Cherty Flint, partly formed, with serrated edge. 
ANDOVERSFORD 
No. 2.—Celt. Igneous Rock. Probably an aphanite. 
No. 4.—Celt. Unusually dense quartzite. 
No. 5.—Celt. Fine grained quartzite. 
No. 6.—Celt. Basalt—Diorite. 
LEcKHAMPTON 
No. 9.—Seraper. Opaque flint. | 
No. 11.—Javelin or spear-head. Slate. 
BrIrRDLIP 
No. 12.—Flint arrow-head—beautifully formed. 
No. 6.—Large Celt of the Irish type. 
The igneous specimens were shewn to Mr Rudler, who 
submitted them to Mr Teale—a great authority on igneous 
rocks; but he refused to express an opinion unless he had 
sections taken, which could not be done without injury to the 
implements. 
Petrologists now, by the aid of the microscope, make so 
many divisions of the igneous rocks, that the old general term 
of greenstone is in a great measure abandoned; but these 
specimens may safely come under the general head of very 
dense igneous Dolerite and Diorite rocks, which were trans- 
ported from areas far removed from the Cotteswolds. 
I have met with rocks of like character in the drift, and 
also many other rocks derived from distant areas, which will be 
found enumerated in Vol. VIII., page 34, of our Proceedings. 
It was only within the last few days I became aware that 
the Rev. J. H. Cardew, who formerly resided at Cheltenham, 
had made, when he was there, a large collection of implements 
from the high ground of the Cotteswolds, extending as far as 
D 
