= = eee rw 
16 C.C.N.EZS. 
Then we get a seam named after Terebratula Fimbria, a fossil 
common in this particular bed, and higher still Unfossiliferous Oolite, 
passing above into Rubbly Oolite of a dark brown colour which 
contains very many and perfect fossils, and above all this, the 
Gryphite and Trigonia grits named after two well-known fossils 
found chiefly in those beds. Thus we have risen to the top of 
Leckhampton Hill. 
Other quarries of Freestone on the Birdlip Road, of Rubbly 
Oolite at the top of Shurdington Hill, and of Ragstone and Stones- 
field slate on Sevenhampton Common, often repay the walk there 
with good specimens of fossils. 
In the summer Mr. Wethered conducted a party over Leck- 
hampton Hill and explained the Geological formation of the 
neighbourhood. This is the only expedition of this Section which 
we have to record, though we hope to have more during the coming 
season, as well as more collections exhibited at the end of the year. 
