Geology of fJie Lower Moorahool. 53 



The evidence, then, as to whether we have here an anticline in 

 Eocene strata merely, or an unconformable junction between 

 easterly clipping Eocene and westerly dipping Miocene is fairly 

 evenly balanced, and we leave the question open. At the locality 

 marked as fossiliferous on the Quarter-sheet (Section 104) we 

 found fossils in the railway cutting and also close to the creek 

 bed wliich showed the Eocene age of the deposit. The upper 

 beds yield very few forms, but those at the lower level are fairly 

 rich, though the fossils are very much decomposed. 



Railway-cutting. 



Forannnipra. 



Cidaroid spines. 



Crustacea (crab carapace). 



Folyzoa. 



Brachiopoda. 



Waldheimia insolita ?, Tate. 



Terebratulina scoulari, Tate. 

 Lamellihranchiata. 



Ostrea sp. 



Pecten sp. 



Limatula jeffreysiana ?, Tate. 



Spondylus pseudoradula, McCoy. 



Dimya dissimilis, Tate. 



Cowie's' Crekk. 

 Brachiopoda. 



Terebratulina scoulari, Tate. 

 Lamellibranchiata. 



Pecten zitteli, Hutton. 

 Leda vagans, Tate. 

 ,, apiculata, Tate. 

 ,, huttoni, T. Woods. 

 Limopsis belcheri, Adams and Reeve. 

 Plagiarca cainozoica, Tate. 

 Cardita polyneraa, Tate. 

 ,, delicatula, Tate. 

 Diplodonta subquadrata, Tate. 

 Cytherea eburnea, Tate. 



