140 PROCEEDINGS COTTESWOLD CLUB 1903 
above the Insect-limestone,’” that Prof. T. Rupert Jones 
obtained Darwinula liasstca (Brodie), and DP. fzasszca var. 
major, Jones. The Rheetic facies of this bed induces me to 
dissent from Mr Wilson’s classification and group it with 
the Upper Rheetic. Above 1% feet of such shale is the 
basement bed of the Lower Lias, a bluish-black limestone 
crowded with Ostrea liassica and Modiola minima. 
At Wainlode the Upper Rhetic is 13 feet 4 inches 
thick ; the Lower, 14 feet 7 inches. 
2.—THE GRAY HILL, APPERLEY. 
Not quite a mile to the north of Wainlode Cliff is the 
Rhetic and Liassic outlier of Gray (or Grey) Hill. A 
fault affects the outlier on the north, running east and 
west. The small quarry on the summit mentioned by 
Brodie is now completely overgrown. He noticed the 
‘“ Ostrea-bed” and Pseudomonotis-bed or “ Insect-lime- 
stone,’ remarking that the insect remains were very 
abundant, “many small slabs, three or four inches square, 
exhibiting several elytra and wings, and a few small 
beetles.”" In the escarpment facing west, above the Upper 
Keuper Marls, there is evidence of the following beds :— 
SECTION I.—GRAY HILL. 
ft. ins. 
2 LIMESTONE, Psewdomonotis-bed, Natadita? (fragments) 
4 LIMESTONE, Estheria-bed, with ‘‘ dendritic” markings, 
Naiadita .. ute oe oe = oe ee 4 
7 LIMESTONE, hard, blue, separating into two layers, Aviczla 
contorta, Protocardium rheticum, Modiola minima, 
Gervillia precursor, Myophoria, scales of Gyrolepis. 2 
13 SANDSTONE, hard, grey, calcareous, ‘* Pullastra” “et I 
15 SANDSTONE, (Bone-bed-equivalent); whitish, micaceous, 
non-calcareous, ‘* Pullastra” ea ee : 
1 “ Fossil Insects,” p. 61. 
