340 
In every case the strata is similar to that at Crisp’s farm on 
the S. slope of Lansdown. The sands are succeeded by the 
“burrs,” these by the iron-shot fossiliferous beds containing the 
characteristic Upper Lias Ammonites. Whether the light blue 
clay below is of Upper or Lower Lias age is doubtful, I am 
inclined to think it is the former. 
Notes of some Somerset Wells. By W. Wuitaxer, B.A., F.R.S., 
F.G.S., Assoc. Inst. C.E., and Horace B. Woopwarp, F.G.S, 
Where not otherwise stated the figures stand for feet. 
[Remarks in square brackets have been added by the authors. ] 
BEDMINSTER. Ashton Gate Brewery. 
Made and communicated by Messrs. G. ISLER & Co. 
No supply. 
THICKNESS.; DEPTH. 
Shaft (the rest bored) tg sive — 434 
[ ? Valley Drift | Sand a, ae 24 46 
(Red bind... ae 5 51 
| Red and blue bind 4 55 
[Trias] { Marl, very binding + 59 
| Red stony marl 7 66 
| Hard red stone 54 714 
{ Iron band : — 34 743 
Spar and hard sandstone 13 76 
Red mixed marl 2 784 
Shaly marl 5 834 
[Coal Dry gault [clay] 24 853 
Measures ? | jreae soe ’ At ag 
Mixed stone ... 24 924 
Red shaly marl 2 944 
Hard stone 1} 953 
Stony marl 14 97 
\_ Pit down 34 1004 
