l\ans. Roy. Soc. Edin. 



Vol. XLVI. 



Professor P. F. Kendall and Mr E. B. Bailey on " The Glaciation of East Lothian 

 South of the Garleton Hills."— Plate II. 



Fig. 1. — Junction of the dry valley shown in PI. I. fig. 2, with that which carries the Spott Burn. 

 carrying the stream has not been appreciably deepened since glacial times (p. 11). 



In this case the valley 



Fig. 2. — Braidwood Burn. The present stream has cut a minor winding gorge into the bottom of the glacial channel, 

 can still be readily recognised. The material cut through by the burn is Old Red conglomerate (p. 12). 



The latter 



