71 



RISTIANIA. 



t a t i £ i> 



Undulations of I.ower and Upper Silurian, 



moir on the Geology of Scandinavia, very imper- 

 The original section, as given in the great work 



justify the conclusions insisted on in the memoir 

 succession tliere traceable from Lower through 

 small scale, towards the right-hand side of the 



the effects they have produced, though it is not 



