the <Icr 



ivery would 



be 51,028,905,312,000 



'To the 



northward 



of the Bahama Banks, 



)f the sti 





k'as a sliglit current set- 



InUII.I t! 







> of' Jill) 



cam, oil 



OnXTon' 



inetiines inclining' it to 



3ve to, some fifty miles 



when we experienced 



,".i|i J, J, 



■ hour sett ii 



i- southeast, the wind 

 len rise of the plateau 







of the Arctic current. 



■ disturb 



ance. In J 





Chariest 









southwest. 



"When our trawl was 





esse! headed 



. northeast, and .Iriflcl 



r^uthw 



est. I found 



this southwest current 



'h.'.t I <To-M , ,V't),e snvainJ-u'i j -liTn-.t ih.dVt'at an) 



- A very striking example of the influence of the wind on the 

 current was experienced by us off Cape Lookout. We were in 



a liwh o-al'o nmir <„, f.v.m the XAV. The current was 'turned 



er. The fact ot 

 ninution, and at 

 end to show the 



