;594 . Dr. Wheelton Hind— Lower Culm of North Devon. 



the synclinal trough is important. Tracing the rocks from north to 

 south, Coddon Hill beds form an east to west line of elevation, 

 succeeded by a hollow trough. In this hollow the Venn limestones. 



W 



w 



I .2 



^ ;i z> 



M *-, 2 



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with Posidonomija Becheri, have been worked. In the centre of 

 the synclinal is an east to west line of elevation, sections of which 



