5o km 



Fig. 1. Jutland peninsula with lines indicating different stages of ice-margins. 



remained stationary in any position the more typical the landscapes 

 have become. 



The heath-plains are composed of material washed out from the 

 ice by the streams issuing from it and deposited in advance of the 

 ice-margin. 



The hill-land was accumulated at the edge of the ice and beneath its 

 margin. Here the ice on melting, gradually left the greater part of the 

 material brought along with it, and here the deposition has been most 

 irregular. 



