 In late September , a tropical wave persisted in the northeastern Atlantic Ocean . The low @-@ pressure area later became sufficiently organized to be classified as a tropical storm at 0000 UTC on September 22 . The disturbance quickly organized after tropical cyclogenesis , and reached a strength equivalent to a modern @-@ day Category 1 hurricane strength at 1800 UTC later that day . The American steamship <unk> encountered the system that day , and reported gale force winds in conjunction with a peripheral barometric pressure of 996 mbar ( hPa ; 29 @.@ 42 inHg ) . The tropical cyclone continued to the east @-@ northeast , where it gradually intensified . At 1200 UTC on September 23 , the hurricane attained modern @-@ day Category 2 hurricane intensity with winds of 100 mbar ( 155 km / h ) ; a peak which would be maintained for at least the following 12 hours . A second steamship , the <unk> , reported hurricane @-@ force winds along with a minimum pressure of 977 mbar ( hPa ; 28 @.@ 85 inHg ) ; this would be the lowest pressure measured associated with the tropical cyclone . After reaching peak intensity , the hurricane began a weakening trend , and degenerated to a Category 1 hurricane at 0600 UTC as it passed over the Azores . The following day , the hurricane recurved westward , where it weakened before transitioning into an extratropical cyclone on September 28 . This remnant system subsequently dissipated . 
