784 



BULLETIN OF THE BUEEAU OF FISHERIES 



from the channel (34.4 per mille), to about 33.6 per mille in the northeastern corner 

 of the gulf. 



At still deeper levels the distribution of salinity becomes increasingly governed 

 by the contour of the bottom as this more and more confines the inflowing slope 



Fig. 147.— Salinity at a depth of 100 meters, July 19 to August 26, 1914. Bay of Fundy from Craigie 



water. Thus the latter (34 per mille) was not only directed more into the eastern 

 arm of the Y-shaped trough at 175 meters than into the western in 1914 (fig. 149) 

 but hugged the eastern slope of the former, making it the site of an anticlockwise 



