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PROCEEDINGS COTTESWOLD CLUB 
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Yartleton Farm Ma * mi 
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SECTION A THROUGH THE NORTHERN SLOPE OF MAY HILL. 
(Horiz. scale 3 inches= 1 mile.) 
(Yartleton Beds). 
[The dip of the Old Red Sandstone to the east of the Newent Woods is 
nowhere visible.) 
is faulted against Wenlock Shales and Ludlow beds. Along its 
southern margin there is an important fault which runs nearly 
east and west close to Rock Farm, and this will be referred to 
as the Rock Farm Fault. 
The third part extends over Bright’s Hill, Huntley Hill and 
Nottswood Hill to a point just south of the railway beyond 
Blaisdon. In this portion of the area the eastern boundary is 
a fault, which separates Llandovery beds for the most part, 
but to the south Woolhope Limestone, Wenlock Shales and 
Wenlock Limestone, from Triassic rocks, while to the west Old 
Red Sandstone rests conformably on Downtonian beds. 
Throughout almost the whole of this part of the area the 
dip on the eastern side is to the south-west, except where to 
the south the Silurian beds approach the fault which separates 
them from the Trias, and there they swing round so that the 
dip is to the south-south- west. On the west side of the ridge 
the overlying Woolhope Limestone is vertical near Little 
London, so that the Llandovery beds may be bent as represented 
in Section B. 
O.R.S. Old Red Sandstone. 
c. Llandovery Sandstone (Huntley 
WS. Wenlock Shale. 
a. Woolhope Limestone. 
b. Llandovery Sandstone 
Hill Beds). 
T. Trias. 
FF. Faults. 
