354- 
LOWER OOLITIC ROCKS OP ENGLAND : 
in J.TUT -L.I 
Forest Marble 
Bradford Clay - 
Great Oolite 
FT. IN. 
5. Clay and thin stone - - - " "I fi 
4. False-bedded oolitic limestone - J 
3. Grey marly clay much like the 
Fuller's Earth clay of Eype : 
few if any fossils ... 
^Marly clay.here^ 
and there ce- 
mented into 
a tolerably 
hard bed by 
calcareous ^ about 10 
2. Fossil J matter, and I 1 ft. 3 in. 
Bed. 1 with an im- f to 2 ft. 
persistent 
layer of 
shelly lime- 
stone (6 to 
8 in.) at the 
base - 
1. Shelly oolite and hard brown marly oolitic 
limestone. 
The Fossil-bed yields Apiocrinus Parkinsoni, Pentacrinus 
(fragments), Waldheimia digona, Terebratula maxillata, T. 
coarctata, Rhynchonella concinna, R. obsoleta, R. varians, Avicula 
costata, Corbicella subangulata, Lima, Ostrea gregaria, O. 
Sowerbyi, Pecten vagans, Vermilia (Serpula) sulcata ?, &c. 
FIG. 100. 
Section near Upper Westwood, Bradford-on-Avon. 
Slabs of the shelly Forest Marble yield Serpula, Rhynchonella, 
Osirea Sowerbyi, Pecten vagans, and Ccrithium. 
A section very similar to that above noted, was exposed by the 
Lime-kilns to the south-east. Here the beds, as noticed by 
Townsend, are at a much lower level than the same strata at 
Berfield. Evidently the fault traced on the Geological Survey 
