Mr. Cumberland on the Strata near Bristol. 
113 
No. 
Ft. 
In 
281. 
Shaley bed 
“ 
1 
282. 
Ditto 
2 
6 
283. 
Ditto 
8 
284. 
Ditto, rotten bottom . 
, , 
2 
G 
285. 
Ditto, solid 
# 
6 
28 6. 
A broken bed . * ' 
O » 
1 
287. 
Ditto, solid 
J-* 
a 
2 
6 
288. 
Ditto, broken 
QJ u 
1 
2 
289. 
Ditto, solid 
aS . 
6 
290. 
Ditto . . , 
QJ U 
<8 m 
r! 
4 
291 . 
Ditto 
s 
5 
After this the beds of limestone disappear, being- 
covered by soil and low woods, sloping down at forty- 
five degrees S.W. to the towing-path of the river Avon. 
The foot of the hill terminating at about three hundred 
yards from the lowest bed that appears above ground, 
from whence the woody hill rises again at the point of 
this second woody hill, the three last beds of this long- 
range appear : viz. 
292. The corner of a thin bed containing encrinites of a singular 
construction in the stem. The trochus having five per- 
forations like a flower, also it has anomia of three species. 
293. A thin pallet bed, described by Mr, Bright in his paper before 
the Society. 
294. Another No. 16, of the same paper, being a highly ferruginous 
limestone. 
Here terminates all that is visible of this noble section 
of limestone beds, perhaps not to be equalled in number, 
or for convenience of access. 
vol. v. 
p 
