BIGELOW: EXPLORATIONS IN THE GULF OF MAINE. 



65 



that each was Salter than its predecessor at all depths. The bottom 

 salinity at Station 24 is an apparent exception to this generalization; 

 but this Station, like Station 2, lies in a circumscribed trough of the 

 sea bottom, and it is probable that the salinity at the level of the en- 

 closing sill, eighty fathoms, was almost as high as it was at the bottom, 

 just as it was at Station 2. At Stations 8, 9 and 16 (fig. 23, 26) i. e. T 



FaAM .7 

 



5 



10 



15 



20 

 25 

 30 

 35 

 40 

 45 

 50 

 55 

 60 

 65 

 70 

 75 



85 

 90 

 95 

 100 

 105 

 110 

 115 

 .120 

 125 



.9 31 .1 .2 .3 4 5 .6 .7 .8 .9 33 .1 .2 .3 4- 5 .6 .7 .8 .9 

















































































































































































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X 



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A, 



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2 



1 





























































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43 















































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 \ 





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23->2 



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7 



























































Fig. 21. — Salinity sections at Stations 2, 7, 23, 24, 43. 



in the coastal band of low surface salinity, the rate of increase with 

 depth was much more rapid than at the off-shore stations, which shows 

 of course that the effect of the fresh drainage from the land is greatest 

 at the surface; and the same is true of Stations 25 and 38 off the mouth 

 of Penobscot Bay. The curves on the off-shore banks, Piatt's, Jeffrey's 

 and German, and in the Grand Manan Channel (fig. 24) are especially 



