178 INFERIOR OOLITE AT BRANCH HUISH, RADSTOCK. 



former notice, and are the same beds as are seen in the well- 

 known Mungar quarry, W. of Radstock, 



They are surmounted by a few feet of brownish clays in both 

 the Huish quarries ; this clay we formerly classed with the Upper 

 Lias ; no fossils have been found ; they have been previously 

 alluded to {loc. cit. p. 178 and 188.) 



Perhaps I should apologise for bringing so small a matter before 

 the Society, but it is a case where fossil evidence is so abundant 

 and so palpable, that any member however unpractised, may easily 

 draw his lines after a little careful collecting from beds in situ. 



