 On October 7 , a large elongated extratropical cyclone extended across the Atlantic Ocean with a pressure of at most 1015 mbar ( hPa ; 29 @.@ 98 inHg ) . The following day , the low @-@ pressure area became more narrow and well @-@ defined , with its central pressure deepening to 1000 mph ( hPa ; 29 @.@ 53 inHg ) . On October 9 , the extratropical system was analyzed to have become a tropical depression . The low moved slowly to the northeast and gradually weakened before dissipating on October 10 . On October 14 , offshore observations indicated that a tropical depression had developed north of The Bahamas . The following day , however , the depression became less defined and degenerated into a trough of low pressure . On October 16 , two ships listed in the International <unk> Ocean @-@ <unk> Data Set reported winds of 40 mph ( 65 km / h ) off the coast of North Carolina . However , since these reports occurred in a higher pressure gradient , the system was not included in HURDAT . 
