Banco Chinchorro, Mexico, at 00:00 UTC on October 28. Moving north-northeast, the storm reached Category 1 hurricane intensity about 24 hours after its classification. Around that time, it peaked with maximum sustained winds of . Around 06:00 UTC on October 29, the system made landfall near Cape San Antonio, Cuba, at the same intensity. After about six hours over Cuba, the hurricane weakened to a tropical storm. It transitioned into an extratropical cyclone in present-day Mayabeque Province before being absorbed by a frontal boundary shortly thereafter. Other systems In addition to the six systems that reached tropical storm status, four other tropical depressions developed. The first formed northeast of Bermuda on May 5, marking the third consecutive year in which a tropical cyclone originated before June. The depression was absorbed by a frontal boundary on May 7. Another tropical depression developed in the Bay of Campeche on June 13. Drifting slowly northward and westward, the system made landfall in southern Texas on June 16 and dissipated the following day. The next tropical depression formed in the vicinity of the Azores on July 20. After four days, it was absorbed into a frontal system. The final cyclone that failed to tropical storm status developed in the northeastern Gulf of Mexico to the south of Tallahassee, Florida, on August 4. Drifting southwestward over the next few days, the depression dissipated by August 7. See also List of tropical cyclones Atlantic hurricane season 1900–1940 South Pacific cyclone seasons 1900–1950 South-West Indian Ocean cyclone seasons 1910s Australian region cyclone seasons References External links Monthly Weather Review Articles which contain graphical timelines 1913 meteorology 1913 natural disasters