268 THE FOREST LANDS OF FINLAND. 



Southern Scandinavia is that two kinds of ice-marks 

 remain on this part of the Northern Hemisphere. There 

 are marks of local ice-systems which radiated from the 

 watershed. There are also marks on watersheds and high 

 passes ; and on lower lands at 3000, 2000, and 500 feet, 

 which do not radiate from any watershed, but point N.E. 

 and S.W., or thereby. Take the northern block of the 

 peninsula, and the same thing appears.' 



