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At upper end of section [[strikethrough]][[?]][[/strikethrough]] at water tower occurs Curdsville Under this is a 3 foot Bentonite, then calcareous mudstone (30 - 35') bounded below by another thick (2') bentonite. This interval is said to be Eggleston. Below this is thin platy fossiliferous ls. abounding in Pionodema and said to be Tyrone. The green shale is also placed in this interval. The Eggleston produced few fossils. Subulites, Strophomena.

[[image in margin]]

-------------| 
Curdsville   |  
-------------| -|  
Bentonite    |  |    
-------------|  |
Platy ls.    |  |--- Eggleston
-------------|  |
Bentonite    |  |
-------------| -|  
Within like  |      Tyrone? T-42
Thin bedded  |            |     
Pionodema ls |            |  [[down arrow through green shale layer]]   
-------------|            |
Green Shale  |            |
-------------|            v
Platy -      |        
silty -      |
shaly        | Moccasin
ls.          |
             |