Show GULF tt among tie many tl cones wl icci agnen to us as flotd fiche aid stored a ivay is such in our memories during our schoolboy days but which arc being swept away aire by one by later invests In vesti we sl all probably that which professed to describe so accurately tl e u and influence of the gi tio nored teaching of 0 old 1 ies that the fi force of the current after entering ind nutting complete circuit ol 01 mexico made its way northward gli alie cooler tiers of tl e V estern atlantic and even affected of 1 drope ins been materially 1 by tl e more car ful lions of modern ahe view that is now favored it not fully cd by t observers veis is 01 if stream as a current re illy begins it 1 lond i str ailt ind ei ds where near tl grand J inka e fact that the deitt aiom the stream le found largely in 11 e western p artof 11 atlantic is eipl lin d by tl e li 11 lelice of tl e prevailing winds but I 1 aleut leut 1 ils bury is thought to have shown tint winds do not eilt er tho velocity position or direction of the itself 1 ltd cs of tho stream drift have been found during the last few years closely picked il nie the eist ern alious of tt middle and north atlantic bt itis 11 is giai lid some to fear that alie gulf atit irn avis its position to 11 coast and that a gradual of alie result hut mr J lied way out m a docent articie that has botn i i briod ic change in certain of the fitments fit ments of the stream ivar bini o it 1 iid ain ence and lie argues th it the sunia Su nip alou that in d very long i of time tho of tho may ct the 1 position and of the ano of 1 flow is a question of theory and not of fid mr U at Is remarkable cor ecsi between tl e track of tl is current and the cyclones of alie north atlantic but asserts tl at proof of any connection between tho two 1 he nomen Is lacking the records of it e er korean of the ui ilca baates show th it during alie months when tl e canent of tho ault stream is i utting forth its glei lest alie cyclones come fre aind it is thought possible th it alie excess of moisture which hovers along the tragic of the efreim a be the fuel to which their energy tor ta |