 On October 19 , a low @-@ pressure area moved into the southwestern Caribbean Sea . The area of disturbed weather quickly became well @-@ organized , and was analyzed to have become a tropical depression at 0000 UTC on October 20 . Initially , the tropical cyclone moved very slowly towards the west and then the northwest . Shortly after formation , the disturbance intensified into a tropical storm at 1800 UTC later that day . The S.S. <unk> provided the first indications of a tropical cyclone in the region , after reporting strong gusts and low pressures north of the Panama Canal Zone during that evening . Continuing to intensify , the storm reached hurricane intensity at 0600 UTC on October 22 . Several vessels in the storm 's vicinity reported strong gusts and rough seas generated by the storm . Later that day at 1200 UTC , the ship S.S. <unk> reported a minimum pressure of 983 mbar ( hPa ; 29 @.@ 03 inHg ) near the periphery of the storm . Based on this observation , the hurricane was estimated to have reached intensity at the same time with winds of 80 mph ( 130 km / h ) . The hurricane subsequently curved west and then southwest , before making its only landfall in northern Nicaragua at 1900 UTC on October 23 at peak intensity . Once inland , the tropical cyclone rapidly weakened over mountainous terrain , and dissipated at 1200 UTC the following day . Reports of damage were limited , though a report stated that considerable damage had occurred where the hurricane made landfall . 
