Geol. Mag. 1903. 



Dec. IV, Vol. X, PI. XIII. 



Fig. I.— Side of Granite Sill, Strathy Point. 



Note.— The junctions here shown are much sharper than those of the true permeation phenomena 

 the softness of which it is very difficult to represent. 



Fig. 2.— End of Granite Sill, Kinbrace. 



. f 



\ I 



Fig. 3.— ClitTabout 200 feet high, G1as Eilean, Strathy Point. 



