38 -GASTEROPODA OF THE INFERIOR OOLITE. 
Profile No, 2.—Virney Cross Quarry. 
(Section complete.) 
Capping of Fuller’s Earth. 
1 9" P, 
Upper shell-bed. Belemnites, 
Trigonia, Se. 
Brachytrema. Onustus. 
It should be noted that not very far from here, in a southerly direction, traces of the 
Humphriesianus-zone have been found by Mr. H. B. Woodward ; i.e. he obtained a fine specimen of 
Am. Humphriesianus in a certain quarry. See remarks on this point with reference to the Burton 
Bradstock section. Either a thin layer of an older rock is adherent to the shell-bed, or there is an 
admixture of forms. 
a Es | 3) 3" Caleareous rock with fewer fossils, chiefly Brachiopoda. 
= qd 
a| | Crowded with Brachiopoda of ; 
is) lene rowded wit rachiopoda of many species. Some 
At % | Eo) Be Gasteropoda. 
et 
= | = || 2! 9 Calcareous rock 
Ay Ay z 
a 
p 
| Terebratula spheroidalis above. 
1’ 9" P, In two divisions. GastERopopa. 
I Astarte obliqua below. 
-(R = ea =F = 
A 5 & [ I Block containing in lower part a line of irony nodules. 
S ‘a Oo 
(2) ||| sy tS 
= a i | 0! 8" Blue block containing Am. Murchisone atop. 
Lal 
Qa A 
me) | GH Grey calciferous grits and hard brownish sand-rock. 
ea 
= 
Sg 13/ 3! Yeovil Sands. 
a Total. 
