VOL. XV. (1) RHATIC ROCKS 35 
“ White Lias,” such as occurs at Radstock, in Somerset. 
“Tea-green Marls” are again visible in the north bank of 
the road a little over a quarter of a mile west-south-west 
of “ The Forest.” Thence the escarpment is well marked, 
trending northwards to its bold termination, Turret Hill. 
A little under a quarter of a mile north-west of “ Gorse 
Hall,” sandstone (17) resting upon “ Tea-green Marls,” is 
visible in a pond side, and the same bed caps Turret Hill. 
The north flank of this hill is very steep, but as we pro- 
ceed south-eastwards, the declivity lessens, the Rhetic 
being faulted against the red marls of the Keuper. Pro- 
ceeding south from the locality marked as Lane End, and 
taking the second turning to the left, limestones and clays 
are exposed in the banks of the stream just below the 
bridge. One bed of limestone, the first seen when pro- 
ceeding down stream, may be the equivalent of the 
Pseudomonotis-bed, and the subjacent and superincumbent 
deposits are blue and yellow calcareous clays. A little 
further down stream the Os¢rea-beds (pre-flanorbrs) are 
visible. 
In the fields on the escarpment east of the locality 
marked as “ Stoners” on the Geological Survey Map, are 
numerous pieces of sandstone (Rhetic), and in the field- 
track from this locality to Castle Hill the “Tea-green 
Marls” are exposed, and again about 700 yards north-west 
of Feckenham Church. Between Noers Green and Beanhall 
Mill the physical indications of the junction of the two series 
are not prominent; but at the latter locality, in the bank 
immediately to the north of the cottage, the “ Tea-green 
Marls” are visible. From Morton Underhill to three- 
quarters of a mile east-south-east of Netherton, the Lower 
Lias is faulted against the Keuper. This fault is very 
accurately delineated on the Geological Survey Map, but 
unfortunately it was not possible to obtain the date of the 
newest Liassic deposit, which occurs in juxtaposition with 
D2 
