264 PROCEEDINGS COTTESWOLD CLUB 1906 
Thickness in 
Feet inches 
SHALES, coarsely laminated; Schizodus  ... 1 2 
| LIMESTONE, earthy, similar to bed 7: Pecten 
(Chlamys) valoniensis a ae ate A 
6 SHALES, coarsely laminated; Schizodus Ewaldi, 
Myophoria, Pteria contorta... ie tac TO 
7 LIMESTONE, greenish-brown, somewhat earthy ; 
Pecten valoniensis, Pteria contorta, shell- 
débris, fish-seales oe: oye Ae % 
8 SHALES, black, imperfectly laminated, with 
sandstone-layers near the base : Us.) See 
»| 9 SHALES, black, thinly laminated; constitute 
| a conspicuous feature dee Pre ae ee 
| 10 SHALES, black, coarsely laminated... rae ee" 
®4( 11 SANDSTONE, yellowish-white, micaceous, cal- 
o careous ; layer intermittent ose avs 4% 
&| 12 SHALES, black ; lower 4 inches earthy ; upper 
4 7 inches clayey ; Schizodus Ewald, Selenite II 
13. SANDSTONE, very pyritic ; Acrodus minimus, 
Gyrolepis Alberti, Sauricththys acuminat- 
us, (%"—1%".) Selenite on upper surface | 1 
14 SHALES, black, clayey, with thin pyritic 
sandstone layers (6”—10") ... 4% eee 8 
15 SANDSTONE (Bone-bed); highly _ pyritic, 
coarse-grained in places, small quartz pebbles; 
Acrodus minimus, Gyrolepis Alberti, 
teeth of Gyrolepis? and Saurichthys acu- 
minatus als as ees aa eee O-I 
I.“ Tea-green Marls.” Greenish-grey marls 
(weather-whitish,) angular fracture ; hard 
zone 6” to 8” thick near top ... ies see 
II. Red Marls seen in road ascending the hill to 
the cottage : re re 
Upper 
Keuper 
The importance of this section lies in the fact that 
there are no Pudlastra-Sandstones. The Bone-bed rests 
directly upon the “Tea-green Marls” of the Keuper, all 
the infra-bone-bed deposits of Garden Cliff being absent 
from here. Whilst at Garden Cliff the Lower Rheetic 
measures 19 feet 8% inches, at Denny Hill it measures 
only 9 feet 7 inches. So reduced a thickness for the 
Lower-Rheetic beds is seldom obtained. 
When, on June 14th, 1904, a party of this Club visited 
the outlier of Rhetic and Lower-Lias rocks of Berrow 
