GREAT OOLITE : WTCHWOOD. 
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marly bed seems to be part of 
the Great Oolite, in a some- 
what remanie condition. 
The accompanying section 
(Fig. 88) will serve to show 
the general relations? of the 
strata in the Wychwood area. 
The White Limestone has 
also been quarried near Min- 
ster Lovel, but the beds are 
not very well shown. They 
are much fissured and shat- 
tered near the surface. Some 
Fish-remains have been found 
in the top beds.* 
* See W. S. Horton, Geologist, vol. 
iii. p. 252. 
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