'»'\ 



'^ cp 3a 



\ 



7ai{h of Holdoi'ns 

 ■(apid recession iji-e 



I' fl 



(%Jatyeihprp* ] 



Outmarilm ^ Caasr profecred fcy sea.ivalfs 

 ol v^ ^'S, erosion fairly stsffc floW ' 





W^.fm tif iKf-iiW f 



6u//f up by the long breakers sweeping in 

 from the Atlantic, this beach at Cap Breton 

 In the Bay of Biscay Is composed of long 

 stretches of sand. Its ridged profile, 

 gradually built up by the long waves, is 

 worn smooth each year by winter storms 



ings Lyn* 



Part of the east coast of England Is shown 

 on this map at a large scale and in detail. 

 This particularly interesting area has been 

 chosen because it has both cliffs and 

 artificially reenforced coast lines, low 

 coast lines and also areas of erosion and 

 deposition. In some areas where the 

 Pleistocene glaciation has left marl^ed 

 features, these have been indicated. 



231 



