oT es, eS ee ee eee 
VOL. XV. (3) EXCURSION—LECKHAMPTON HILL 189 
Thickness in 
Feet inches 
. Whitish, chalky-looking rock, here more in- 
durated than usual; Zerebratula fimbria, 
Sow.; 8 feet to 10 feet... : . 
OoxitE Maru 
(10 feet) 10 
. Massive yellowish limestones: about  . 34 
Noticeable rubbly deposit which can be seen 
passing laterally into a markedly false- 
bedded oolite. This deposit in its rubbly 
condition consists of two or three bands of 
rubbly limestone with intervening brown 
clay-streaked oolitic marl with pebbles in 
places ....... Rare, Sa oe ey oe 9 
. Massive yellowish limestone, oolitic, false- 
bedded, and the whole very much bored: 
ADOUEN, ke) ts 40 fo) 
{ 33 
| 34 
Lower FREESTONE 
(77 feet 9 inches) 
e 
Fe 
37 
L 
PEA-Grir pisolitic limestone. Usual fossils 12 fc) 
(32 feet) . Massive-bedded, grey pisolitic limestones the 
upper strata being called the “Weather- 
stones.” Usual fossils 20 
Lower LIMESTONE 38. Brown and grey limestones: about 6 
(6 feet) (39- Ferruginous oolite “made up of small 
brown, oval, shining grains like small seeds, 
cemented together by a sort of calcareous 
paste of a yellow and brown colour.” 
Belemnites and Ostreé &. o 
4o. “ Yellow sand without fossils” fo) 1% 
41. “Hard dark grey, approaching to brown, 
shelly, crystalline limestone, containing 
Belemnites, some Ammonites, Pectines ( P. 
lens), Terebratula (especially 7. bidens) 
[= Rhyn. cynocephala], Lima, Amphides- 
ma, Gervillia, and Serpule. Bones, scales, 
Coprolites and Teeth of Fish are dispersed 
throughout the mass, and may be most 
readily distinguished on the surface, inter- 
mixed with the same brown oval grains as 
in D [i.e. bed 39] higher up. The Lime- 
stone has been bored into by Lzthodomz, 
and the cavaties are often filled up with 
fragments of bones, etc. At its junction 
ScissuM-Beps 4 
| with the sand above [bed 40] it is of a 
42. 
(4 feet 4% inches) 
yellow colour, and it passes in a yellow 
ferruginous, pure, sandy, micaceous stone, 
with fewer oval particles, full of Belemmnztes, 
Ammonites, Pectines, and numerous frag- 
ments of Bones, Scales and Coprolites. On 
the whole, Belemnites, are more abundant 
than Ammonites at Leckhampton ‘ I oO 
“ Brick-coloured and dark yellow sandy marl, 
with broken Shells, chiefly Pectins, and 
L small spines of Czdaris” fe) 3 
Upper L1ias “ Blue micaceous shale” : about ape 290 ° 
Mippte Liss '  -Marlstone 
