210 REV. R. A. BULLEN, B.A., ON EOLITHIC IMPLEMENTS. 
Irish sea, the only source of the flints is Antrim. They, as a 
rule, possess the physical character peculiar to Antrim flints.” 
In 1893 and 1898 I obtained from gravels of glacial age* 
west of Wells, Norfolk, implements of a rude type, one of 
them in situ at 4 feet down in the sand and gravel. This 
gravel pit is known now as Morter’s, formerly Cadamy’s, 
and is about 300 yards south of the Wells to Holkham 
Railway. The railway is metalled from the gravel of the 
cuttings between Wells and Holkham, and between Wells 
and Fakenham, in which these gravels cap the disturbed 
chalk. 
Fig. 3.—Morter’s GRAVEL Pit, West SIDE. 
The followmg is Rev. O. Fisher’s description of the 
railway-cutting west of Wells :— 
“The deep channels cut out of the chalk surface by these 
(ice) bergs are to be found farther to the west (of Kelland 
and Weybourn). There is a splendid section of such a one 
in the railway-cutting between Holkham and Wells. The 
width of it is 120 yards. It is filled with coarse bouldered 
gravel and fine calcareous sand, containing abundantly frag- 
* Rev. O. Fisher, M.A., F.G.S., “On the Denudations of Norfolk,” 
Geol. Mag., 1868, p. 551. See also Drift Map 68 N.W. of Geol. Survey. 
