Quart. Journ. Geoi. Soc.Vol.LXV, PL XXX. 



Crosby Garrett 



(Scale: i inch = i^ miles.) 



>ved. This has been inferred from a study of (i) the distribution of the erratic 

 glacial sculpture ; and (3) the alignment of the drumlins and other glacial deposits, 

 mit to which boulders of oriyin external to the Howgill Fells have been observed, 

 which no evidences of glacial sculpture or erosion have been impressed, 

 -courses, which are the same as in the map of the rivers of the Howgill Fells (PI. XXIX).] 



