A glacial deposit near Christiania. 13 



Drøbak-Aas, ice movement and the removal of morainique 

 matter has taken place in the direction due south, with only 

 a very little deviation, somewhat variable, and shifting as 

 climatic conditions changed. This line of motion is also 

 completely corresponding with the direction of the moraine 

 range in question. We see, that in the Christiania Region, at 

 this time, the movement of the ice-sheet has been normal to 

 the margin of the continental cover of glaciation. 



The University of Christiania, March, 1900. 



