92 



considerably lower than now, but we cannot at present draw 

 any conclusions as to the order in which these different 

 changes of level succeeded each other in either country. In 

 southern Scandinavia, sinking of the country has taken place 

 twice since it was covered by ice , and in the interval it has 

 been raised above the present level of the sea; possibly the 

 same changes have taken place in Greenland. 



