FAULT IN THE CLIFF WEST OF BRIDrORT HARBOUR. 121 



For instance, Professor Secley, T. Robeits, and others have shown 

 that the corallian series are represented by a bed of clay in the 

 Fen district. 



If this opinion is correct, an important line of division has 

 hitherto escaped all notice on our Bridport coast owing to the 

 faintncss of its lithological character, and we have one more 

 instance of the necessity of determining these lines upon a careful 

 study of palaeontology. 



