STATHER : A GLACIATED SURFACE AT FILEY. 
349 
now blocks the mouth of this valley shows clearly by its character 
that a tongue of ice passed inland at this point for some distance. 
The stripe are close to the place where the great inland curve would 
occur, and where, therefore, considerable augmentation of the 
pressure in the basal layers of the ice might be expected. 
For the map illustrating these notes I am indebted to my 
friend, Mr. W. H. Crofts. 
