200 
PROCEEDINGS COTTESWOLD CLUB 
1920 
WSW. 3 F 2 F 1 E.71.E. 
SECTION C THROUGH PART OF THE NORTH-WEST SLOPE OF 
MAY HILL. 
(Horiz. scale, 6 inches=i mile.) 
1. Llandovery Sandstone (Yartleton Beds). 
2. Woolhope Limestone. 
3. Old Red Sandstone. 
FF. Faults. 
and close to the bounding fault farther to the east it is 
horizontal. 
On the north-east slope of Glasshouse Hill there is a stretch 
of Woolhope Limestone which runs for about half a mile west- 
wards from the eastern boundary fault. It is to be seen in an 
old digging in the woods to the south of Castle Hill, where the 
rock dips 12° north-north-east, and nearer Glasshouse other 
exposures show dips to the north-north-east and north-east ; 
but there is another set of exposures in a stream to the south 
of the above which first shows Llandovery Sandstone dipping 
south-south-east and then more Woolhope Limestone, so that 
the beds roll slightly here (vide Section D). 
4. THE WENLOCK SHALES. 
These shales are very soft, exposures in them are scanty, 
and their presence is often only indicated by a broad valley or 
