"5 

 may U- it <i a fault or an ordinary conformable 



some districts, particularly in those where older for 

 mations are covered by more recent superficial accuimi 



IB, a iloti: nonliability n -\ be seen. 



.iccompar example (1-ig. 34), re- 



presents what is exposed in a cliff se< n<>n at ( ullcn, on 

 the coast of Banffshirc. The lowest n consists 



of quart /it c ( < d at a high angle to 



the south-east The upturned ends of these strata are 

 unconformahly ly red sandstones and con- 



