91 
STONY FURLONG CUTTING (continued) 
ft. ins. 
4. Sandy parting ae Sr ae a as Oo 4 
5. Compact bed, very hard, “ perforated” 5 Sy ak, Oka U 
6. Falsely bedded Oolite, with very thin partings bas rane 3 
7. Well marked bench top, a soft friable grey Oolite, probably 
two beds and parting caer 4 0 
8. Compact rock, varying in character, but perforated through- 
out and crowded with fossils is Ee 
9. Sand parting : 
10. Rock, “ perforated ” 
11. Parting 
12. . Rock, Freestone 
wooo ® 
Conon Fr Oo 
Twenty yards north of the bridge these beds from No. 7 
downwards are faulted ten feet down. There isa second and 
most important fault at about fifty yards N. from the bridge, 
i.e., thirty yards from the small fault. Apparently a quite new 
set of beds are faulted either up or down, I cannot determine 
_ which, but as it was only newly excavated a few days ago, the 
following section is a rough one, and less likely to be quite so 
correct as those at the two ends, which have been longer 
accessible. 
Section of faulted beds fifty yards N. of bridge. 
ft. ins. 
_ Rock ee ot ts =~ e i, ie a" 3 — 42 10 
Parting clay or marl 8 
‘Hard “ perforated” bed eG 
_ Parting marl ee: 
Rock not determined a 0 
Clay parting eG 
Rock “ seggregated ” 20 
Clay parting... Ke 0 6 
Very compact freestone 3&6 
we eh 0 6 
Hard compact Oolite, 4 feet thick at fault—but rising furtheronto 14 0 
and isa dense white Oolite with thin sandy partings 
Here apparently is the termination of the fault. Beneath 
this occurs a remarkable band which is persistent hence forward 
and easily recognized. It is absolutely unlike anything I am 
