132 PROCEEDINGS COTTESWOLD CLUB 1908 
EBRINGTON-HILL QUARRY: NO. 2 
Thickness in feet inches 
1. Limestones, pale yellowish-grey, coarsely 
Lower 
Rr somewhat disturbed at f, and 
Freestone 
fz; seen, at least ue . soy as 
. Limestones, sandstones and ee Ostrea 
Sp.5 Pecten (Amusium) personatus, Gold- 
fuss, Pentacrinus - ossicles, echinoid- 
radioles . 9° * a 
Pea-Grit | 3: sand, yellowish, “with a thin ferruginous 
; layer : 4to 8inches ... a OG 
Equivalent | 4, Brown, sandy, shelly rock, with occa- 
and sional sandy partings: slightly ferru- 
ower ginous at the top Ammonites sp. (? 
; ‘Welschia obtusiformis, S. Buckman, at 
Limestone 
5 feet below the Sand Bed 3) ee ee 
. Limestone, pale yellowish-grey, coarsely 
oolitic ; Rhynchonella sp. (of the AAyz.- 
subangulata- group), Lecten (Amusium) 
personatus, Goldfuss: seen... oooh fre 
The third quarry, the “ Ilmington-Down Quarry,” is 
of considerable size, and shows fairly massive-bedded 
deposits of yellowish-grey oolite with numerous specimens 
—especially in the top-portion—of A museum personatum 
(Goldfuss). Such rocks are exposed to a depth of 23 
feet. There are conspicuous infillings of a rubbly sandy 
rock, sand of various tints of yellow and brown, and 
sandy clay. The source of the small amount of argill- 
aceous matter is not quite clear, but there can be no 
doubt that the sandy material has been derived from the 
Pea-Grit Equivalent: indeed, on the south side of the 
quarry the sandy beds are very well shown zz se¢w above 
the Lower Limestone, and are seen to embrace-layers of 
fissile sandstone. 
To sum up, then, the sequence of deposits at Ebring- 
ton Hill is as follows : 
Lower Freestone (fars). 
Inferior Pea-Grit Equivalent. 
Oolite Lower Limestone. 
[? Scissum-Beds. 
